1.
Tropical rainforest climate
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A tropical rainforest climate, also known as an equatorial climate, is a tropical climate usually found along the equator. Regions with this climate typically feature tropical rainforests, and it is designated Af by the Köppen climate classification. One day in an equatorial climate can be similar to the next. A tropical rainforest is found at latitudes within 10 degrees North and South of the equator. The climate is most commonly found in South America, Central Africa, however, tropical rainforest microclimates are found in many other regions, while not everywhere along the equatorial region features a tropical rainforest climate. Additionally, while tropical rainforest climates are located near the equator. For instance, Santos, Brazil and Fort Lauderdale, United States are not only far removed from the equator, yet both of these cities feature a tropical rainforest climate, albeit with noticeably cooler and warmer periods of the year
Tropical rainforest climate
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Worldwide zones of Tropical rainforest climate (Af).
2.
Tropical monsoon climate
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Tropical monsoon climates have monthly mean temperatures above 18 °C in every month of the year and feature wet and dry seasons, as Tropical savanna climates do. Tropical monsoon climates however features its driest month seeing on average less than 60 mm and this latter fact is in direct contrast to a tropical savanna climate, whose driest month sees less than 60 mm of precipitation and also less than 100 – of precipitation. In essence, a monsoon climate tends to either see more rainfall than a tropical savanna climate or have less pronounced dry seasons. Additionally, a monsoon climate tends to see less variance in temperatures during the course of the year than a tropical savanna climate. This climate has a driest month which nearly always occurs at or soon after the winter solstice for that side of the equator, there are generally two versions of a tropical monsoon climate, Less pronounced dry seasons. Regions with this variation of the monsoon climate typically see copious amounts of rain during the wet season. However, unlike most tropical climates, a sizeable amount of precipitation also falls during the dry season. In essence, this version of the monsoon climate generally has less pronounced dry seasons than tropical savanna climates. Extraordinarily rainy wet seasons and pronounced dry seasons and this variation features pronounced dry seasons similar in length and character to dry seasons observed in tropical savanna climates. However, this is followed by a period of extraordinary rainfall. In some instances, up to 1,000 mm of precipitation is observed per month for two or more consecutive months, Tropical savanna climates generally do not see this level of sustained rainfall. Tropical monsoon climates are most commonly found in South and Central America, however, there are sections of South Asia, Southeast Asia, Africa, the Caribbean and North America that also feature this climate. The major controlling factor over a tropical climate is its relationship to the monsoon circulation. The monsoon is a change in wind direction. In Asia, during the summer there is a flow of air. In the “winter” an offshore air flow is prevalent, the change in direction is due to the difference in the way water and land heat. October is the hottest month no matter whether is it in the southern or northern hemisphere and this is because October is the shoulder season of the year as if it is the end of the wet season and no winter winds blowing. Changing pressure patterns that affect the seasonality of precipitation occur in Africa though it generally differs from the way it operates in Asia
Tropical monsoon climate
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Worldwide zones of tropical monsoon climate (Am).
3.
Tropical savanna climate
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Tropical savanna climate or tropical wet and dry climate is a type of climate that corresponds to the Köppen climate classification categories Aw and As. This latter fact is in direct contrast to a monsoon climate. In essence, a savanna climate tends to either see less rainfall than a tropical monsoon climate or have more pronounced dry seasons. There are generally four types of tropical climate,1. Distinct wet and dry seasons of relatively equal duration, most of the regions annual rainfall is experienced during the wet season and very little precipitation falls during the dry season. A lengthy dry season and a short wet season. This version features seven or more dry season months and five or less wet season months, there are variations within this version, On one extreme, the region receives just enough precipitation during the short wet season to preclude it from a semi-arid climate classification. This drier variation of the savanna climate is typically found adjacent to regions with semi-arid climates. On the other extreme, the features a lengthy dry season followed by a short. However, regions with this variation of the climate do not experience enough rainfall during the wet season to qualify as a monsoon climate. A lengthy wet season and a short dry season. This version features seven or more wet season months and five or less dry season months, a dry season with a noticeable amount of rainfall followed by a rainy wet season. Tropical savanna climates are most commonly found in Africa, Asia, the climate is also prevalent in sections of Central America, northern Australia and southern North America, specifically in sections of Mexico and the state of Florida in the United States. Most places that have this climate are found at the margins of the tropical zone. Similarly, the Caribbean coast, eastward from the Gulf of Urabá on the Colombia – Panamá border to the Orinoco river delta and this condition extends to the Lesser Antilles and Greater Antilles forming the Circumcaribbean dry belt. The length and severity of the dry season diminishes inland, at the latitude of the Amazon river—which flows eastward, East from the Andes, between the arid Caribbean and the ever-wet Amazon are the Orinoco river llanos or savannas, from where this climate takes its name. Sometimes As is used in place of Aw if the dry season occurs during the time of higher sun and this is the case in parts of Hawaii, East Africa, Sri Lanka and coastal regions of Northeastern Brazil, for instance. The difference between summer and winter in such locations is usually so slight that a distinction between an As and Aw climate is a quibble
Tropical savanna climate
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Worldwide zones of Tropical savanna climate (Aw).
4.
Hot desert climate
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An area that features this climate usually experiences from 25 to 200 mm per year of precipitation and in some years may experience no precipitation at all. Averages may be even less such as in Arica, Chile, there are usually two or three variations of a desert climate, a hot desert climate, a cold desert climate and, sometimes, a mild desert climate. To determine whether a location has a climate, the precipitation threshold is determined. If the areas precipitation is less than half the threshold. Hot desert climates are found under the subtropical ridge where there is largely unbroken sunshine for the whole year due to the stable descending air. These areas are located between 30 degrees south and 30 degrees north latitude, under the subtropical latitudes called the horse latitudes, hot desert climates are generally hot, sunny and dry year-round. Hot desert climates also reach similar latitudes in the Middle East, North Africa, hot desert climates usually feature hot, sometimes exceptionally hot, periods of the year. In many locations featuring a hot climate, maximum temperatures of over 40 °C are not uncommon in summer. The world absolute heat records, over 50 °C, are generally in the hot deserts, some desert locations consistently experience very high temperatures all year long, even during wintertime. These locations feature some of the highest annual average temperatures recorded on Earth and this last feature is seen in some parts of deserts of Africa and Arabia. During colder periods of the year, night-time temperatures can drop to freezing or below due to the radiation loss under the clear skies. However, very rarely do temperatures drop far below freezing, only one region in Europe has a hot desert climate, Province of Almeria, Province of Alicante and Province of Murcia in South Eastern Spain. Cold desert climates usually feature warm and dry summers, though summers typically are not quite as hot as summers in hot desert climates, unlike hot desert climates, cold desert climates tend to feature cold winters with rare snow. Cold desert climates are found at higher altitudes than hot desert climates. A cold desert climate is found in temperate zones, usually in the rain shadow of high mountains. A classic example of this is the Patagonian Desert in Argentina bounded by the Andes to its west, in the case of Central Asia, mountains restrict precipitation from the monsoon. The Gobi desert in Mongolia is an example of this. Though hot in summer, it shares the cold winters of the rest of Central Asia
Hot desert climate
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Namib Desert, Namibia
Hot desert climate
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A dusting of snow in the Atacama Desert.
Hot desert climate
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Cold deserts do get the occasional blanket of snow, such as
Snake Valley, Utah and Nevada
5.
Cold desert climate
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An area that features this climate usually experiences from 25 to 200 mm per year of precipitation and in some years may experience no precipitation at all. Averages may be even less such as in Arica, Chile, there are usually two or three variations of a desert climate, a hot desert climate, a cold desert climate and, sometimes, a mild desert climate. To determine whether a location has a climate, the precipitation threshold is determined. If the areas precipitation is less than half the threshold. Hot desert climates are found under the subtropical ridge where there is largely unbroken sunshine for the whole year due to the stable descending air. These areas are located between 30 degrees south and 30 degrees north latitude, under the subtropical latitudes called the horse latitudes, hot desert climates are generally hot, sunny and dry year-round. Hot desert climates also reach similar latitudes in the Middle East, North Africa, hot desert climates usually feature hot, sometimes exceptionally hot, periods of the year. In many locations featuring a hot climate, maximum temperatures of over 40 °C are not uncommon in summer. The world absolute heat records, over 50 °C, are generally in the hot deserts, some desert locations consistently experience very high temperatures all year long, even during wintertime. These locations feature some of the highest annual average temperatures recorded on Earth and this last feature is seen in some parts of deserts of Africa and Arabia. During colder periods of the year, night-time temperatures can drop to freezing or below due to the radiation loss under the clear skies. However, very rarely do temperatures drop far below freezing, only one region in Europe has a hot desert climate, Province of Almeria, Province of Alicante and Province of Murcia in South Eastern Spain. Cold desert climates usually feature warm and dry summers, though summers typically are not quite as hot as summers in hot desert climates, unlike hot desert climates, cold desert climates tend to feature cold winters with rare snow. Cold desert climates are found at higher altitudes than hot desert climates. A cold desert climate is found in temperate zones, usually in the rain shadow of high mountains. A classic example of this is the Patagonian Desert in Argentina bounded by the Andes to its west, in the case of Central Asia, mountains restrict precipitation from the monsoon. The Gobi desert in Mongolia is an example of this. Though hot in summer, it shares the cold winters of the rest of Central Asia
Cold desert climate
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Namib Desert, Namibia
Cold desert climate
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A dusting of snow in the Atacama Desert.
Cold desert climate
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Cold deserts do get the occasional blanket of snow, such as
Snake Valley, Utah and Nevada
6.
Hot semi-arid climate
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A semi-arid climate or steppe climate is the climate of a region that receives precipitation below potential evapotranspiration, but not extremely. There are different kinds of climates, depending on such variables as temperature. Semi-arid climates tend to short or scrubby vegetation, with semi-arid areas usually dominated by either grasses or shrubs. To determine if a location has a climate, the precipitation threshold must first be determined. If the areas precipitation is less than the threshold but more than half the threshold. Hot semi-arid climates tend to be located in the tropics and subtropics and these climates tend to have hot, sometimes extremely hot, summers and warm to cool winters, with some to minimal precipitation. Hot semi-arid climates are most commonly found around the fringes of subtropical deserts, hot semi-arid climates are most commonly found in Africa, Australia and South Asia. In Australia, a portion of the Outback surrounding the central desert regions lies within the hot semi-arid climate regime. Hot semi-arid climates can also be found in North America, primarily in Mexico, areas of Texas near Mexico, cold semi-arid climates tend to be located in temperate zones or elevated portions in subtropical zones. They are typically found in continental interiors some distance from bodies of water. Cold semi-arid climates usually feature warm and dry summers, though their summers are not quite as hot as those of hot semi-arid climates. Unlike hot semi-arid climates, areas with cold semi-arid climates tend to have cold winters and these areas usually see some snowfall during the winter, though snowfall is much lower than at locations at similar latitudes with more humid climates. These large diurnal temperature variations are seen in hot semi-arid climates. Cold semi-arid climates are most commonly found in Asia and North America, however, they can also be found in Northern Africa, South Africa, Europe, sections of South America and sections of interior southern Australia and New Zealand. As a result of this, some areas can have climates that are classified as hot or cold depending on the isotherm used. One such location is San Diego, California, which has cool summers for the due to prevailing winds off the ocean. Arid Forest Research Institute Continental climate Dust Bowl Goyders Line Pallisers Triangle Köppen climate classification Wave height Ustic
Hot semi-arid climate
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The semi-arid terrain of
Machakos
Hot semi-arid climate
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BSh
Hot semi-arid climate
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Northeast Caatinga - semiárido brasileño
Hot semi-arid climate
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Extreme weather at
Atacama Large Millimeter Array.
7.
Cold semi-arid climate
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A semi-arid climate or steppe climate is the climate of a region that receives precipitation below potential evapotranspiration, but not extremely. There are different kinds of climates, depending on such variables as temperature. Semi-arid climates tend to short or scrubby vegetation, with semi-arid areas usually dominated by either grasses or shrubs. To determine if a location has a climate, the precipitation threshold must first be determined. If the areas precipitation is less than the threshold but more than half the threshold. Hot semi-arid climates tend to be located in the tropics and subtropics and these climates tend to have hot, sometimes extremely hot, summers and warm to cool winters, with some to minimal precipitation. Hot semi-arid climates are most commonly found around the fringes of subtropical deserts, hot semi-arid climates are most commonly found in Africa, Australia and South Asia. In Australia, a portion of the Outback surrounding the central desert regions lies within the hot semi-arid climate regime. Hot semi-arid climates can also be found in North America, primarily in Mexico, areas of Texas near Mexico, cold semi-arid climates tend to be located in temperate zones or elevated portions in subtropical zones. They are typically found in continental interiors some distance from bodies of water. Cold semi-arid climates usually feature warm and dry summers, though their summers are not quite as hot as those of hot semi-arid climates. Unlike hot semi-arid climates, areas with cold semi-arid climates tend to have cold winters and these areas usually see some snowfall during the winter, though snowfall is much lower than at locations at similar latitudes with more humid climates. These large diurnal temperature variations are seen in hot semi-arid climates. Cold semi-arid climates are most commonly found in Asia and North America, however, they can also be found in Northern Africa, South Africa, Europe, sections of South America and sections of interior southern Australia and New Zealand. As a result of this, some areas can have climates that are classified as hot or cold depending on the isotherm used. One such location is San Diego, California, which has cool summers for the due to prevailing winds off the ocean. Arid Forest Research Institute Continental climate Dust Bowl Goyders Line Pallisers Triangle Köppen climate classification Wave height Ustic
Cold semi-arid climate
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The semi-arid terrain of
Machakos
Cold semi-arid climate
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BSh
Cold semi-arid climate
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Northeast Caatinga - semiárido brasileño
Cold semi-arid climate
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Extreme weather at
Atacama Large Millimeter Array.
8.
Hot-summer Mediterranean climate
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A Mediterranean climate /ˌmɛdɪtəˈreɪniən/ or dry summer climate, is the climate typical of the lands in the Mediterranean Basin. The Mediterranean climate is characterised by dry summers and mild, moist winters, the Azores High is associated with the Mediterranean climate found in southern Europe and north Africa and the Sahara Desert with France and England both bordering this climate, France especially. The South Atlantic High is similarly associated with the Namib Desert, under the Köppen climate classification, hot dry-summer climates and cool dry-summer climates are often referred to as mediterranean. Under the Köppen climate system, the first letter indicates the climate group, temperate climates or C zones have an average temperature above 0 °C, but below 18 °C, in their coolest months. The second letter indicates the precipitation pattern, Köppen has defined a dry summer month as a month with less than 30 mm of precipitation and with less than one-third that of the wettest winter month. Some, however, use a 40 mm level, the third letter indicates the degree of summer heat, a represents an average temperature in the warmest month above 22 °C, while b indicates the average temperature in the warmest month below 22 °C. Under the Köppen classification, dry-summer climates usually occur on the sides of continents. Under Trewarthas system, at least eight months must have average temperatures of 10 °C or higher, during summer, regions of mediterranean climate are dominated by subtropical high pressure cells, with dry sinking air capping a surface marine layer of varying humidity and making rainfall unlikely. In many Mediterranean climates there is a strong character to daily temperatures in the warm months. The majority of the regions with mediterranean climates have relatively mild winters, however winter and summer temperatures can vary greatly between different regions with a mediterranean climate. Or to consider summer, Athens experiences rather high temperatures in that season, in contrast, San Francisco has cool summers with daily highs around. In North America, areas with Csc climate can be found in the Olympic, Cascade, Klamath and these locations are found at high altitude nearby lower altitude regions characterized by a warm-summer mediterranean climate or hot-summer mediterranean climate. A rare instance of this occurs in the tropics, on Haleakalā Summit in Hawaii. In South America, Csc regions can be found along the Andes in Chile, the town of Balmaceda is one of the few towns confirmed to have this climate. Small areas with a Csc climate can also be found at elevations in Corsica. Mediterranean climate Explanation of Mediterranean Climate
Hot-summer Mediterranean climate
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Mediterranean climate distribution in the Americas
Hot-summer Mediterranean climate
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Hot-summer Mediterranean climate (Csa)
9.
Warm-summer Mediterranean climate
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A Mediterranean climate /ˌmɛdɪtəˈreɪniən/ or dry summer climate, is the climate typical of the lands in the Mediterranean Basin. The Mediterranean climate is characterised by dry summers and mild, moist winters, the Azores High is associated with the Mediterranean climate found in southern Europe and north Africa and the Sahara Desert with France and England both bordering this climate, France especially. The South Atlantic High is similarly associated with the Namib Desert, under the Köppen climate classification, hot dry-summer climates and cool dry-summer climates are often referred to as mediterranean. Under the Köppen climate system, the first letter indicates the climate group, temperate climates or C zones have an average temperature above 0 °C, but below 18 °C, in their coolest months. The second letter indicates the precipitation pattern, Köppen has defined a dry summer month as a month with less than 30 mm of precipitation and with less than one-third that of the wettest winter month. Some, however, use a 40 mm level, the third letter indicates the degree of summer heat, a represents an average temperature in the warmest month above 22 °C, while b indicates the average temperature in the warmest month below 22 °C. Under the Köppen classification, dry-summer climates usually occur on the sides of continents. Under Trewarthas system, at least eight months must have average temperatures of 10 °C or higher, during summer, regions of mediterranean climate are dominated by subtropical high pressure cells, with dry sinking air capping a surface marine layer of varying humidity and making rainfall unlikely. In many Mediterranean climates there is a strong character to daily temperatures in the warm months. The majority of the regions with mediterranean climates have relatively mild winters, however winter and summer temperatures can vary greatly between different regions with a mediterranean climate. Or to consider summer, Athens experiences rather high temperatures in that season, in contrast, San Francisco has cool summers with daily highs around. In North America, areas with Csc climate can be found in the Olympic, Cascade, Klamath and these locations are found at high altitude nearby lower altitude regions characterized by a warm-summer mediterranean climate or hot-summer mediterranean climate. A rare instance of this occurs in the tropics, on Haleakalā Summit in Hawaii. In South America, Csc regions can be found along the Andes in Chile, the town of Balmaceda is one of the few towns confirmed to have this climate. Small areas with a Csc climate can also be found at elevations in Corsica. Mediterranean climate Explanation of Mediterranean Climate
Warm-summer Mediterranean climate
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Mediterranean climate distribution in the Americas
Warm-summer Mediterranean climate
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Hot-summer Mediterranean climate (Csa)
10.
Humid subtropical climate
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A humid subtropical climate is a zone of climate characterised by hot, usually humid summers and mild to cool winters. It normally lies on the southeast side of all continents, generally between latitudes 25° and 40° and it tends to be located at coastal or near coastal locations. However, in cases it extends inland, most notably in China. Under the Köppen climate classification, subtropical climates are found in the warmest parts of his Warm Temperate climates or Cfa and this climate features mean temperatures in the coldest month between 0 °C and 18 °C and mean temperatures in the warmest month 22 °C or higher. However, while some climatologists have opted to describe this type as a humid subtropical climate Köppen himself never used this term. The humid subtropical climate classification was created under the Trewartha Climate classification. The Trewartha system was a 1966 update of the Köppen climate classification and this was seen to effectively separate temperate climates like London or New York City from true subtropical locations like Brisbane or Savannah for example. Rainfall often shows a peak, especially where monsoons are well developed, as in Southeast Asia. Most summer rainfall occurs during thunderstorms that build up due to the surface heating and strong subtropical sun angle. Weak tropical lows that move in from adjacent warm tropical oceans, winter rainfall is often associated with large storms in the westerlies that have fronts that reach down into subtropical latitudes. However, many subtropical climates such as southeast Asia or Florida have very dry winters, with frequent brush fires, in Africa, the humid subtropical climates are found in two separate areas on the southern hemisphere of the continent. The Cwa climate is found over a portion of the interior of the Middle. Some lower portions of the Ethiopian Highlands also have this climate, the climate is also found in the narrow coastal sections of southern and eastern South Africa, primarily in KwaZulu-Natal and the Eastern Cape provinces. South Africas version of this climate features heavy oceanic influences resulting in milder temperatures. This is particularly evident in its winters when temperatures do not drop as low as in other regions within the humid subtropical category. Locations in Asia with a subtropical climate differ from those in other continents in that they often have marked seasonal differences in precipitation. Cities near the boundary of this zone include Hong Kong, Hanoi. At Hainan Island and in Taiwan, the transitions from subtropical into fully tropical
Humid subtropical climate
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Cfa
11.
Subtropical highland climate
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Oceanic climates are defined as having a monthly mean temperature below 22 °C in the warmest month, and above 0 °C in the coldest month. It typically lacks a dry season, as precipitation is evenly dispersed throughout the year. Oceanic climates generally have cool summers and mild to cool winters, Oceanic climates are most dominant in Europe, where they spread much farther inland than in other continents. Oceanic climates can have much storm activity as they are located in the belt of the stormy westerlies, many oceanic climates have frequent cloudy or overcast conditions due to the near constant storms and lows tracking over or near them. Precipitation is both adequate and reliable throughout the year in oceanic climates, extended months of rain and cloudy conditions are common in oceanic climates. Seattle is an example of this, between October and May, Seattle experiences high rainfall and is mostly or partly cloudy six out of every seven days. In most areas with a climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter, outside of Australia and parts of New Zealand, most areas with an oceanic climate experience at least one snowstorm per year. In the poleward locations of the climate zone, snowfall is more frequent. Overall temperature characteristics of the oceanic climates feature cool temperatures and infrequent extremes of temperature, summers are cool, with the warmest month having a mean temperature below 22 °C. Poleward of the latter is a zone of the subpolar oceanic climate, with long and cold winters and cool. Examples of this climate include parts of coastal Iceland in the Northern Hemisphere and extreme southern Chile, Oceanic climates are not necessarily always found in coastal locations on the aforementioned parallels, however, in most cases oceanic climates parallel higher middle latitude oceans. The polar jet stream, which moves in a west to east direction across the middle latitudes, advancing low pressure systems, storms, in coastal areas of the higher middle latitudes, the prevailing onshore flow creates the basic structure of most oceanic climates. Oceanic climates are a product and reflection of the adjacent to them. In summer, high pressure pushes the prevailing westerlies north of many oceanic climates. As a result of the Gulf Stream, west-coast areas located in high latitudes like Ireland, the UK, Oceanic climates in Europe occur mostly in Northwest Europe, from Ireland and Great Britain eastward to central Europe. Most of France, Germany, Norway, the north coast of Spain, examples of oceanic climates are found in London, Bergen, Dublin, Berlin, Bilbao, Donostia-San Sebastian, Biarritz, Bayonne, Zürich, Copenhagen and Paris. With decreasing distance to the Mediterranean Sea, the climate of Northwest Europe gradually changes to the subtropical dry-summer or Mediterranean climate of southern Europe
Subtropical highland climate
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Seattle, a city with an oceanic climate
Subtropical highland climate
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World map showing oceanic climate zones, as defined by the
Köppen climate types "Cfb", "Cfc", "Cwb" and "Cwc"
Subtropical highland climate
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Curitiba, capital city of Brazilian
Paraná state features a subtropical highland climate
12.
Oceanic climate
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Oceanic climates are defined as having a monthly mean temperature below 22 °C in the warmest month, and above 0 °C in the coldest month. It typically lacks a dry season, as precipitation is evenly dispersed throughout the year. Oceanic climates generally have cool summers and mild to cool winters, Oceanic climates are most dominant in Europe, where they spread much farther inland than in other continents. Oceanic climates can have much storm activity as they are located in the belt of the stormy westerlies, many oceanic climates have frequent cloudy or overcast conditions due to the near constant storms and lows tracking over or near them. Precipitation is both adequate and reliable throughout the year in oceanic climates, extended months of rain and cloudy conditions are common in oceanic climates. Seattle is an example of this, between October and May, Seattle experiences high rainfall and is mostly or partly cloudy six out of every seven days. In most areas with a climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter, outside of Australia and parts of New Zealand, most areas with an oceanic climate experience at least one snowstorm per year. In the poleward locations of the climate zone, snowfall is more frequent. Overall temperature characteristics of the oceanic climates feature cool temperatures and infrequent extremes of temperature, summers are cool, with the warmest month having a mean temperature below 22 °C. Poleward of the latter is a zone of the subpolar oceanic climate, with long and cold winters and cool. Examples of this climate include parts of coastal Iceland in the Northern Hemisphere and extreme southern Chile, Oceanic climates are not necessarily always found in coastal locations on the aforementioned parallels, however, in most cases oceanic climates parallel higher middle latitude oceans. The polar jet stream, which moves in a west to east direction across the middle latitudes, advancing low pressure systems, storms, in coastal areas of the higher middle latitudes, the prevailing onshore flow creates the basic structure of most oceanic climates. Oceanic climates are a product and reflection of the adjacent to them. In summer, high pressure pushes the prevailing westerlies north of many oceanic climates. As a result of the Gulf Stream, west-coast areas located in high latitudes like Ireland, the UK, Oceanic climates in Europe occur mostly in Northwest Europe, from Ireland and Great Britain eastward to central Europe. Most of France, Germany, Norway, the north coast of Spain, examples of oceanic climates are found in London, Bergen, Dublin, Berlin, Bilbao, Donostia-San Sebastian, Biarritz, Bayonne, Zürich, Copenhagen and Paris. With decreasing distance to the Mediterranean Sea, the climate of Northwest Europe gradually changes to the subtropical dry-summer or Mediterranean climate of southern Europe
Oceanic climate
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Seattle, a city with an oceanic climate
Oceanic climate
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World map showing oceanic climate zones, as defined by the
Köppen climate types "Cfb", "Cfc", "Cwb" and "Cwc"
Oceanic climate
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Curitiba, capital city of Brazilian
Paraná state features a subtropical highland climate
13.
Subpolar oceanic climate
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Oceanic climates are defined as having a monthly mean temperature below 22 °C in the warmest month, and above 0 °C in the coldest month. It typically lacks a dry season, as precipitation is evenly dispersed throughout the year. Oceanic climates generally have cool summers and mild to cool winters, Oceanic climates are most dominant in Europe, where they spread much farther inland than in other continents. Oceanic climates can have much storm activity as they are located in the belt of the stormy westerlies, many oceanic climates have frequent cloudy or overcast conditions due to the near constant storms and lows tracking over or near them. Precipitation is both adequate and reliable throughout the year in oceanic climates, extended months of rain and cloudy conditions are common in oceanic climates. Seattle is an example of this, between October and May, Seattle experiences high rainfall and is mostly or partly cloudy six out of every seven days. In most areas with a climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter, outside of Australia and parts of New Zealand, most areas with an oceanic climate experience at least one snowstorm per year. In the poleward locations of the climate zone, snowfall is more frequent. Overall temperature characteristics of the oceanic climates feature cool temperatures and infrequent extremes of temperature, summers are cool, with the warmest month having a mean temperature below 22 °C. Poleward of the latter is a zone of the subpolar oceanic climate, with long and cold winters and cool. Examples of this climate include parts of coastal Iceland in the Northern Hemisphere and extreme southern Chile, Oceanic climates are not necessarily always found in coastal locations on the aforementioned parallels, however, in most cases oceanic climates parallel higher middle latitude oceans. The polar jet stream, which moves in a west to east direction across the middle latitudes, advancing low pressure systems, storms, in coastal areas of the higher middle latitudes, the prevailing onshore flow creates the basic structure of most oceanic climates. Oceanic climates are a product and reflection of the adjacent to them. In summer, high pressure pushes the prevailing westerlies north of many oceanic climates. As a result of the Gulf Stream, west-coast areas located in high latitudes like Ireland, the UK, Oceanic climates in Europe occur mostly in Northwest Europe, from Ireland and Great Britain eastward to central Europe. Most of France, Germany, Norway, the north coast of Spain, examples of oceanic climates are found in London, Bergen, Dublin, Berlin, Bilbao, Donostia-San Sebastian, Biarritz, Bayonne, Zürich, Copenhagen and Paris. With decreasing distance to the Mediterranean Sea, the climate of Northwest Europe gradually changes to the subtropical dry-summer or Mediterranean climate of southern Europe
Subpolar oceanic climate
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Seattle, a city with an oceanic climate
Subpolar oceanic climate
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World map showing oceanic climate zones, as defined by the
Köppen climate types "Cfb", "Cfc", "Cwb" and "Cwc"
Subpolar oceanic climate
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Curitiba, capital city of Brazilian
Paraná state features a subtropical highland climate
14.
Humid continental climate
–
Precipitation is usually well distributed through the year. Some climatologists prefer to use the 0 °C isotherm as it is commonly used. In addition, the location in question must not be semi-arid or arid, humid continental climates tend to be found between latitudes 40° N and 60° N, within the central and northeastern portions of North America, Europe, and Asia. They are much less commonly found in the Southern Hemisphere due to the ocean area at that latitude. More extreme humid continental climates found in southern Siberia and the American Midwest combine hotter summer maxima, climatological averages are used to determine which locations are within a certain climate regime. The World Meteorological Organization has defined this average as through a 30 year period, the version from 1936 utilized a mean temperature of the coldest month of below −3 °C and there must be at least four months whose mean temperatures are at or above 10 °C. In Europe, the −3 °C average temperature isotherm was near the extent of winter snowpack. Many climatologists in the U. S. prefer to use 0 °C as the standard because they feel it better reflects consistency in regional landscapes, the 10 °C average temperature was found to be the minimum temperature necessary for the tree growth. Large temperature ranges are common within this climate zone, in addition, the location in question must not be semi-arid or arid. This is from an update to the climate regime definition introduced by Trewartha & Horn in 1980, despite the 1980 update, climate regimes are essentially the same within the Southern Hemisphere. The largest changes are seen in North America, Europe, under Köppen, the following variants of this climate are possible. The climate regime uses a three letter code, beginning with the letter D. Otherwise, The second letter f , s , A dry summer — the driest summer month has at most 30 millimetres of rainfall and has at most 1⁄3 the precipitation of the wettest winter month. W , A dry winter — the driest winter month has at most one‑tenth of the found in the wettest summer month. The third letter a , Warmest month averages above 22 °C b , Does not meet the requirements for a, within North America, moisture within this climate regime is supplied by the Gulf of Mexico and adjacent western subtropical Atlantic. Snowfall occurs in all areas with a continental climate and in many such places is more common than rain during the height of winter. In places with sufficient wintertime precipitation, the cover is often deep. Most summer rainfall occurs during thunderstorms, and in North America, though humidity levels are often high in locations with humid continental climates, the humid designation means that the climate is not dry enough to be classified as semi-arid or arid. By definition, forests thrive within this climate, biomes within this climate regime include temperate woodlands, temperate grasslands, temperate deciduous, temperature evergreen forests, and coniferous forests
Humid continental climate
–
The snowy city of
Sapporo, Japan.
Humid continental climate
–
Dsa
Humid continental climate
–
Deciduous forest in autumn
15.
Subarctic climate
–
The subarctic climate is a climate characterised by long, usually very cold winters, and short, cool to mild summers. It is found on large landmasses, away from the effects of an ocean. These climates represent Köppen climate classification Dfc, Dwc, Dsc, Dfd, Dwd and Dsd. This type of climate offers some of the most extreme seasonal temperature variations found on the planet, in winter, temperatures can drop to −40 °C and in summer, record low temperatures can be as cold as −60 °C. With 5–7 consecutive months where the temperature is below freezing. Summer warmth is insufficient to thaw more than a few surface feet, seasonal thaw penetrates from 2 to 14 ft, depending on latitude, aspect, and type of ground. Some northern areas with subarctic climates located near oceans, have milder winters and no permafrost, the frost-free season is very short, varying from about 45 to 100 days at most, and a freeze can occur during any month in many areas. Most subarctic climates have very little precipitation, typically no more than 380 mm over an entire year, a notable exception to this pattern is that subarctic climates occurring at high altitudes in otherwise temperate regions have extremely high precipitation due to orographic lift. Mount Washington, with temperatures typical of a climate, receives an average rain-equivalent of 101.91 inches of precipitation per year.5 metres that does not melt until June. Vegetation in regions with subarctic climates is generally of low diversity, as only hardy species can survive the long winters, trees are mostly limited to conifers, as few broadleaved trees are able to survive the very low temperatures in winter. This type of forest is known as taiga, a term which is sometimes applied to the climate found therein as well. Even though the diversity may be low, numbers are high, the process by which plants become acclimated to cold temperatures is called hardening. In some areas, ice has scoured rock surfaces bare, entirely stripping off the overburden, elsewhere rock basins have been formed and stream courses dammed, creating countless lakes. The Tatra Mountains in Poland, above 800m, the Eastern Anatolia, between 1,600 and 2,100 meters – Turkey. The Pyrenees, between 1,600 and 2,100 meters – Andorra, France and Spain, further north in Siberia, continentality increases so much that winters can be exceptionally severe, averaging below −38 °C, even though the hottest month still averages more than 10 °C. This creates Dfd, Dwd and Dsd climates, one example is parts of the Snowy Mountains in Australia, although theyre more alpine than true subarctic. In China and Mongolia, as one moves southwestwards or towards lower altitudes, temperatures increase, Boreal ecology Boreal forest Plants of continental subarctic climate Köppen climate classification Subantarctic
Subarctic climate
–
Dsc
16.
Tundra climate
–
In physical geography, tundra is a type of biome where the tree growth is hindered by low temperatures and short growing seasons. The term tundra comes through Russian тундра from the Kildin Sami word tūndâr uplands, there are three types of tundra, Arctic tundra, alpine tundra, and Antarctic tundra. In tundra, the vegetation is composed of shrubs, sedges and grasses, mosses. Scattered trees grow in tundra regions. The ecotone between the tundra and the forest is known as the line or timberline. Arctic tundra occurs in the far Northern Hemisphere, north of the taiga belt, the word tundra usually refers only to the areas where the subsoil is permafrost, or permanently frozen soil. Permafrost tundra includes vast areas of northern Russia and Canada, the polar tundra is home to several peoples who are mostly nomadic reindeer herders, such as the Nganasan and Nenets in the permafrost area. Arctic tundra contains areas of landscape and is frozen for much of the year. The soil there is frozen from 25–90 cm down, and it is impossible for trees to grow, instead, bare and sometimes rocky land can only support low growing plants such as moss, heath, and lichen. There are two seasons, winter and summer, in the polar tundra areas. During the winter it is cold and dark, with the average temperature around −28 °C. However, extreme temperatures on the tundra do not drop as low as those experienced in taiga areas further south. During the summer, temperatures rise somewhat, and the top layer of seasonally-frozen soil melts, the tundra is covered in marshes, lakes, bogs and streams during the warm months. Generally daytime temperatures during the rise to about 12 °C. Arctic tundras are sometimes the subject of conservation programs. In Canada and Russia, many of areas are protected through a national Biodiversity Action Plan. Tundra tends to be windy, with winds often blowing upwards of 50–100 km/h, however, in terms of precipitation, it is desert-like, with only about 15–25 cm falling per year. Although precipitation is light, evaporation is also relatively minimal, there is a natural pattern of accumulation of fuel and wildfire which varies depending on the nature of vegetation and terrain
Tundra climate
–
Tundra in Greenland
Tundra climate
–
Tundra in
Siberia
Tundra climate
–
Vuntut National Park in Canada
Tundra climate
–
A group of
muskoxen in Alaska
17.
Ice cap climate
–
An ice cap climate is a polar climate where the temperature never exceeds 0 °C. The climate covers areas in or near the regions, such as Antarctica and Greenland. Such areas are covered by a permanent layer of ice and have no vegetation, but they may have animal life, ice cap climates are inhospitable to human life. Antarctica, the coldest continent on Earth, sustains no permanent human residents, some places like Antarctica had a different climate before having an ice cap climate Under the Köppen climate classification, the ice cap climate is denoted as EF. Ice caps are defined as a climate with no months above 0 °C, such areas are found around the north and south pole, and on the top of the highest mountains. Since the temperature never exceeds the point of ice, any snow or ice that accumulates remains there permanently. The ice cap climate is distinct from the climate, or ET. A tundra climate has a season with temperatures consistently above freezing for several months. This summer is enough to melt the ice cover, which prevents the formation of ice sheets. Because of this, tundras have vegetation, while ice caps do not, ice cap climate is the worlds coldest climate, and includes the coldest places on Earth. Vostok, Antarctica is the coldest place in the world, having recorded a temperature of −89.2 °C and these ice sheets, however, are not static, but slowly move off the continents into the surrounding waters. New snow and ice accumulation then replaces the ice that is lost, precipitation is nearly non-existent in ice cap climates. It is never enough for rain, and usually too cold to generate snow. However, wind can blow snow onto the ice sheets from nearby tundras, the ice sheets are often miles thick. Much of the land located under the ice sheets is actually below sea level, however, it is the weight of the ice itself that forces this land below sea level. If the ice was removed, the land would rise back up in an effect called post-glacial rebound and this effect is creating new land in formerly ice cap areas such as Sweden. The causes the formation of lakes, the largest being Lake Vostok in Antarctica. Ice cap climates have only existed in ice ages, there have been at least five such ice ages in the Earths past
Ice cap climate
–
A polar bear with cub
Ice cap climate
–
Solar radiation has a lower intensity in polar regions because it travels a longer distance through the atmosphere, and is also spread across a larger surface area due to its oblique angle of approach.
18.
Germany
–
Germany, officially the Federal Republic of Germany, is a federal parliamentary republic in central-western Europe. It includes 16 constituent states, covers an area of 357,021 square kilometres, with about 82 million inhabitants, Germany is the most populous member state of the European Union. After the United States, it is the second most popular destination in the world. Germanys capital and largest metropolis is Berlin, while its largest conurbation is the Ruhr, other major cities include Hamburg, Munich, Cologne, Frankfurt, Stuttgart, Düsseldorf and Leipzig. Various Germanic tribes have inhabited the northern parts of modern Germany since classical antiquity, a region named Germania was documented before 100 AD. During the Migration Period the Germanic tribes expanded southward, beginning in the 10th century, German territories formed a central part of the Holy Roman Empire. During the 16th century, northern German regions became the centre of the Protestant Reformation, in 1871, Germany became a nation state when most of the German states unified into the Prussian-dominated German Empire. After World War I and the German Revolution of 1918–1919, the Empire was replaced by the parliamentary Weimar Republic, the establishment of the national socialist dictatorship in 1933 led to World War II and the Holocaust. After a period of Allied occupation, two German states were founded, the Federal Republic of Germany and the German Democratic Republic, in 1990, the country was reunified. In the 21st century, Germany is a power and has the worlds fourth-largest economy by nominal GDP. As a global leader in industrial and technological sectors, it is both the worlds third-largest exporter and importer of goods. Germany is a country with a very high standard of living sustained by a skilled. It upholds a social security and universal health system, environmental protection. Germany was a member of the European Economic Community in 1957. It is part of the Schengen Area, and became a co-founder of the Eurozone in 1999, Germany is a member of the United Nations, NATO, the G8, the G20, and the OECD. The national military expenditure is the 9th highest in the world, the English word Germany derives from the Latin Germania, which came into use after Julius Caesar adopted it for the peoples east of the Rhine. This in turn descends from Proto-Germanic *þiudiskaz popular, derived from *þeudō, descended from Proto-Indo-European *tewtéh₂- people, the discovery of the Mauer 1 mandible shows that ancient humans were present in Germany at least 600,000 years ago. The oldest complete hunting weapons found anywhere in the world were discovered in a mine in Schöningen where three 380, 000-year-old wooden javelins were unearthed
Germany
–
The
Nebra sky disk is dated to c. 1600 BC.
Germany
–
Flag
Germany
–
Martin Luther (1483–1546) initiated the
Protestant Reformation.
Germany
–
Foundation of the
German Empire in
Versailles, 1871.
Bismarck is at the center in a white uniform.
19.
Latitude
–
In geography, latitude is a geographic coordinate that specifies the north–south position of a point on the Earths surface. Latitude is an angle which ranges from 0° at the Equator to 90° at the poles, lines of constant latitude, or parallels, run east–west as circles parallel to the equator. Latitude is used together with longitude to specify the location of features on the surface of the Earth. Without qualification the term latitude should be taken to be the latitude as defined in the following sections. Also defined are six auxiliary latitudes which are used in special applications, there is a separate article on the History of latitude measurements. Two levels of abstraction are employed in the definition of latitude and longitude, in the first step the physical surface is modelled by the geoid, a surface which approximates the mean sea level over the oceans and its continuation under the land masses. The second step is to approximate the geoid by a mathematically simpler reference surface, the simplest choice for the reference surface is a sphere, but the geoid is more accurately modelled by an ellipsoid. The definitions of latitude and longitude on such surfaces are detailed in the following sections. Lines of constant latitude and longitude together constitute a graticule on the reference surface, latitude and longitude together with some specification of height constitute a geographic coordinate system as defined in the specification of the ISO19111 standard. This is of importance in accurate applications, such as a Global Positioning System, but in common usage, where high accuracy is not required. In English texts the latitude angle, defined below, is denoted by the Greek lower-case letter phi. It is measured in degrees, minutes and seconds or decimal degrees, the precise measurement of latitude requires an understanding of the gravitational field of the Earth, either to set up theodolites or to determine GPS satellite orbits. The study of the figure of the Earth together with its field is the science of geodesy. These topics are not discussed in this article and this article relates to coordinate systems for the Earth, it may be extended to cover the Moon, planets and other celestial objects by a simple change of nomenclature. The primary reference points are the poles where the axis of rotation of the Earth intersects the reference surface, the plane through the centre of the Earth and perpendicular to the rotation axis intersects the surface at a great circle called the Equator. Planes parallel to the plane intersect the surface in circles of constant latitude. The Equator has a latitude of 0°, the North Pole has a latitude of 90° North, the latitude of an arbitrary point is the angle between the equatorial plane and the radius to that point. The latitude, as defined in this way for the sphere, is termed the spherical latitude
Latitude
–
A graticule on the Earth as a
sphere or an
ellipsoid. The lines from pole to pole are lines of constant
longitude, or meridians. The circles parallel to the
equator are lines of constant latitude, or parallels. The graticule determines the latitude and longitude of points on the surface. In this example meridians are spaced at 6° intervals and parallels at 4° intervals.
20.
Celsius
–
Celsius, also known as centigrade, is a metric scale and unit of measurement for temperature. As an SI derived unit, it is used by most countries in the world and it is named after the Swedish astronomer Anders Celsius, who developed a similar temperature scale. The degree Celsius can refer to a temperature on the Celsius scale as well as a unit to indicate a temperature interval. Before being renamed to honour Anders Celsius in 1948, the unit was called centigrade, from the Latin centum, which means 100, and gradus, which means steps. The scale is based on 0° for the point of water. This scale is widely taught in schools today, by international agreement the unit degree Celsius and the Celsius scale are currently defined by two different temperatures, absolute zero, and the triple point of VSMOW. This definition also precisely relates the Celsius scale to the Kelvin scale, absolute zero, the lowest temperature possible, is defined as being precisely 0 K and −273.15 °C. The temperature of the point of water is defined as precisely 273.16 K at 611.657 pascals pressure. This definition fixes the magnitude of both the degree Celsius and the kelvin as precisely 1 part in 273.16 of the difference between absolute zero and the point of water. Thus, it sets the magnitude of one degree Celsius and that of one kelvin as exactly the same, additionally, it establishes the difference between the two scales null points as being precisely 273.15 degrees. In his paper Observations of two persistent degrees on a thermometer, he recounted his experiments showing that the point of ice is essentially unaffected by pressure. He also determined with precision how the boiling point of water varied as a function of atmospheric pressure. He proposed that the point of his temperature scale, being the boiling point. This pressure is known as one standard atmosphere, the BIPMs 10th General Conference on Weights and Measures later defined one standard atmosphere to equal precisely 1013250dynes per square centimetre. On 19 May 1743 he published the design of a mercury thermometer, in 1744, coincident with the death of Anders Celsius, the Swedish botanist Carolus Linnaeus reversed Celsiuss scale. In it, Linnaeus recounted the temperatures inside the orangery at the University of Uppsala Botanical Garden, since the 19th century, the scientific and thermometry communities worldwide referred to this scale as the centigrade scale. Temperatures on the scale were often reported simply as degrees or. More properly, what was defined as centigrade then would now be hectograde.2 gradians, for scientific use, Celsius is the term usually used, with centigrade otherwise continuing to be in common but decreasing use, especially in informal contexts in English-speaking countries
Celsius
–
A
thermometer calibrated in degrees Celsius
21.
Desert climate
–
An area that features this climate usually experiences from 25 to 200 mm per year of precipitation and in some years may experience no precipitation at all. Averages may be even less such as in Arica, Chile, there are usually two or three variations of a desert climate, a hot desert climate, a cold desert climate and, sometimes, a mild desert climate. To determine whether a location has a climate, the precipitation threshold is determined. If the areas precipitation is less than half the threshold. Hot desert climates are found under the subtropical ridge where there is largely unbroken sunshine for the whole year due to the stable descending air. These areas are located between 30 degrees south and 30 degrees north latitude, under the subtropical latitudes called the horse latitudes, hot desert climates are generally hot, sunny and dry year-round. Hot desert climates also reach similar latitudes in the Middle East, North Africa, hot desert climates usually feature hot, sometimes exceptionally hot, periods of the year. In many locations featuring a hot climate, maximum temperatures of over 40 °C are not uncommon in summer. The world absolute heat records, over 50 °C, are generally in the hot deserts, some desert locations consistently experience very high temperatures all year long, even during wintertime. These locations feature some of the highest annual average temperatures recorded on Earth and this last feature is seen in some parts of deserts of Africa and Arabia. During colder periods of the year, night-time temperatures can drop to freezing or below due to the radiation loss under the clear skies. However, very rarely do temperatures drop far below freezing, only one region in Europe has a hot desert climate, Province of Almeria, Province of Alicante and Province of Murcia in South Eastern Spain. Cold desert climates usually feature warm and dry summers, though summers typically are not quite as hot as summers in hot desert climates, unlike hot desert climates, cold desert climates tend to feature cold winters with rare snow. Cold desert climates are found at higher altitudes than hot desert climates. A cold desert climate is found in temperate zones, usually in the rain shadow of high mountains. A classic example of this is the Patagonian Desert in Argentina bounded by the Andes to its west, in the case of Central Asia, mountains restrict precipitation from the monsoon. The Gobi desert in Mongolia is an example of this. Though hot in summer, it shares the cold winters of the rest of Central Asia
Desert climate
–
Namib Desert, Namibia
Desert climate
–
A dusting of snow in the Atacama Desert.
Desert climate
–
Cold deserts do get the occasional blanket of snow, such as
Snake Valley, Utah and Nevada
22.
Semi-arid
–
A semi-arid climate or steppe climate is the climate of a region that receives precipitation below potential evapotranspiration, but not extremely. There are different kinds of climates, depending on such variables as temperature. Semi-arid climates tend to short or scrubby vegetation, with semi-arid areas usually dominated by either grasses or shrubs. To determine if a location has a climate, the precipitation threshold must first be determined. If the areas precipitation is less than the threshold but more than half the threshold. Hot semi-arid climates tend to be located in the tropics and subtropics and these climates tend to have hot, sometimes extremely hot, summers and warm to cool winters, with some to minimal precipitation. Hot semi-arid climates are most commonly found around the fringes of subtropical deserts, hot semi-arid climates are most commonly found in Africa, Australia and South Asia. In Australia, a portion of the Outback surrounding the central desert regions lies within the hot semi-arid climate regime. Hot semi-arid climates can also be found in North America, primarily in Mexico, areas of Texas near Mexico, cold semi-arid climates tend to be located in temperate zones or elevated portions in subtropical zones. They are typically found in continental interiors some distance from bodies of water. Cold semi-arid climates usually feature warm and dry summers, though their summers are not quite as hot as those of hot semi-arid climates. Unlike hot semi-arid climates, areas with cold semi-arid climates tend to have cold winters and these areas usually see some snowfall during the winter, though snowfall is much lower than at locations at similar latitudes with more humid climates. These large diurnal temperature variations are seen in hot semi-arid climates. Cold semi-arid climates are most commonly found in Asia and North America, however, they can also be found in Northern Africa, South Africa, Europe, sections of South America and sections of interior southern Australia and New Zealand. As a result of this, some areas can have climates that are classified as hot or cold depending on the isotherm used. One such location is San Diego, California, which has cool summers for the due to prevailing winds off the ocean. Arid Forest Research Institute Continental climate Dust Bowl Goyders Line Pallisers Triangle Köppen climate classification Wave height Ustic
Semi-arid
–
The semi-arid terrain of
Machakos
Semi-arid
–
BSh
Semi-arid
–
Northeast Caatinga - semiárido brasileño
Semi-arid
–
Extreme weather at
Atacama Large Millimeter Array.
23.
Monsoon
–
Usually, the term monsoon is used to refer to the rainy phase of a seasonally changing pattern, although technically there is also a dry phase. The term is sometimes used for locally heavy but short-term rains. The major monsoon systems of the world consist of the West African and Asia-Australian monsoons, the inclusion of the North and South American monsoons with incomplete wind reversal has been debated. The south-west monsoon winds are called Nairutya Maarut in India, the English monsoon came from Portuguese monção, ultimately from Arabic mawsim and/or Hindi mausam, perhaps partly via early modern Dutch monsun. Strengthening of the Asian monsoon has been linked to the uplift of the Tibetan Plateau after the collision of the Indian sub-continent and Asia around 50 million years ago. Because of studies of records from the Arabian Sea and that of the wind-blown dust in the Loess Plateau of China, testing of this hypothesis awaits deep ocean sampling by the Integrated Ocean Drilling Program. The monsoon has varied significantly in strength since this time, largely linked to climate change. A study of marine plankton suggested that the Indian Monsoon strengthened around 5 million years ago, then, during ice periods, the sea level fell and the Indonesian Seaway closed. When this happened, cold waters in the Pacific were impeded from flowing into the Indian Ocean and it is believed that the resulting increase in sea surface temperatures in the Indian Ocean increased the intensity of monsoons. Five episodes during the Quaternary at 2.22 Ma,1.83 Ma,0.68 Ma,0.45 Ma and 0.04 Ma were identified which showed a weakening of Leeuwin Current. The weakening of the LC would have an effect on the sea surface temperature field in the Indian Ocean, thus these five intervals could probably be those of considerable lowering of SST in the Indian Ocean and would have influenced Indian monsoon intensity. The impact of monsoon on the weather is different from place to place. In some places there is just a likelihood of having a more or less rain. In other places, quasi semi-deserts are turned into green grasslands where all sorts of plants. The Indian Monsoon turns large parts of India from a kind of semi-desert into green lands, see photos only taken 3 months apart in the Western Ghats. In places like this it is crucial for farmers to have the right timing for putting the seeds on the fields, Monsoons are large-scale sea breezes which occur when the temperature on land is significantly warmer or cooler than the temperature of the ocean. These temperature imbalances happen because oceans and land absorb heat in different ways, in contrast, dirt, sand, and rocks have lower heat capacities, and they can only transmit heat into the earth by conduction and not by convection. Therefore, bodies of water stay at an even temperature
Monsoon
–
Advancing monsoon clouds and showers in Aralvaimozhy, near
Nagercoil,
India
Monsoon
–
Monsoon clouds over
Lucknow,
Uttar Pradesh.
Monsoon
–
Western Ghats on May 28 in dry season, 2010
Monsoon
–
Western Ghats on August 28 in rainy season, 2010
24.
Mediterranean climate
–
A Mediterranean climate /ˌmɛdɪtəˈreɪniən/ or dry summer climate, is the climate typical of the lands in the Mediterranean Basin. The Mediterranean climate is characterised by dry summers and mild, moist winters, the Azores High is associated with the Mediterranean climate found in southern Europe and north Africa and the Sahara Desert with France and England both bordering this climate, France especially. The South Atlantic High is similarly associated with the Namib Desert, under the Köppen climate classification, hot dry-summer climates and cool dry-summer climates are often referred to as mediterranean. Under the Köppen climate system, the first letter indicates the climate group, temperate climates or C zones have an average temperature above 0 °C, but below 18 °C, in their coolest months. The second letter indicates the precipitation pattern, Köppen has defined a dry summer month as a month with less than 30 mm of precipitation and with less than one-third that of the wettest winter month. Some, however, use a 40 mm level, the third letter indicates the degree of summer heat, a represents an average temperature in the warmest month above 22 °C, while b indicates the average temperature in the warmest month below 22 °C. Under the Köppen classification, dry-summer climates usually occur on the sides of continents. Under Trewarthas system, at least eight months must have average temperatures of 10 °C or higher, during summer, regions of mediterranean climate are dominated by subtropical high pressure cells, with dry sinking air capping a surface marine layer of varying humidity and making rainfall unlikely. In many Mediterranean climates there is a strong character to daily temperatures in the warm months. The majority of the regions with mediterranean climates have relatively mild winters, however winter and summer temperatures can vary greatly between different regions with a mediterranean climate. Or to consider summer, Athens experiences rather high temperatures in that season, in contrast, San Francisco has cool summers with daily highs around. In North America, areas with Csc climate can be found in the Olympic, Cascade, Klamath and these locations are found at high altitude nearby lower altitude regions characterized by a warm-summer mediterranean climate or hot-summer mediterranean climate. A rare instance of this occurs in the tropics, on Haleakalā Summit in Hawaii. In South America, Csc regions can be found along the Andes in Chile, the town of Balmaceda is one of the few towns confirmed to have this climate. Small areas with a Csc climate can also be found at elevations in Corsica. Mediterranean climate Explanation of Mediterranean Climate
Mediterranean climate
–
Mediterranean climate distribution in the Americas
Mediterranean climate
–
Hot-summer Mediterranean climate (Csa)
25.
Continental climate
–
In the Köppen climate system, Continental climates were bordered to the south by Temperate climates or C climates and to the north by Boreal climate or E climates. Köppen also defined continental climates as having more than 30 days with continuous snowcover on the ground, Continental climates often have a significant annual variation in temperature. They tend to occur in the latitudes, where prevailing winds come from over land. Continental climates occur mostly in the Northern Hemisphere which has the large landmasses required for this type of climate to develop, most of northern and northeastern China, eastern and southeastern Europe, and the central and upper eastern United States have this type of climate. In Continental climates, Precipitation tends to be moderate in amount, a portion of the annual precipitation falls as snowfall, and snow often remains on the ground for more than a month. Summers in continental climates can feature thunderstorms and frequent cool temperatures, the timing of intermediate spring-like or autumn-like temperatures in this zone vary depending on latitude and/or elevation. For example, spring may arrive as soon as early March in the parts of this zone. Annual precipitation in this zone is usually between 600 millimetres and 1,200 millimetres, most of it in the form of snow during winter and it also has cold winters and warm summers. Most such areas fit Köppen classifications of Dfa, Dwa or Dfb or Dwb, dry summer continental climates exist in high altitude areas near Mediterranean climates. In some cases, the climate classification of BSk can also be considered to be continental as long it has cold winter. Some climatologists use the 0 °C isotherm instead for the coldest month, Continental climates exist where cold air masses infiltrate during the winter and warm air masses form in summer under conditions of high sun and long days. Places with continental climates are as a rule either far from any moderating effects of oceans or are so situated that prevailing winds tend to head offshore. Such regions get quite warm in the summer, achieving temperatures characteristic of tropical climates but are colder than any other climates of similar latitude in the winter. These climates grade off toward subtropical climates equator-ward where winters are less severe, in Europe these climates may grade off into oceanic climates in which the influence of moderating air masses is more marked toward the west. The subarctic climate, with cold, long and dry winters. Canada, Throughout much of southern Canada from the Rocky Mountains to Atlantic Canada, major cities, Whistler, Prince George, Kamloops, Calgary, Edmonton, Fort McMurray, Saskatoon, Regina, Winnipeg, Kenora, Thunder Bay, Sault Ste
Continental climate
–
The snowy city of
Sapporo
Continental climate
–
Af
26.
Tundra
–
In physical geography, tundra is a type of biome where the tree growth is hindered by low temperatures and short growing seasons. The term tundra comes through Russian тундра from the Kildin Sami word tūndâr uplands, there are three types of tundra, Arctic tundra, alpine tundra, and Antarctic tundra. In tundra, the vegetation is composed of shrubs, sedges and grasses, mosses. Scattered trees grow in tundra regions. The ecotone between the tundra and the forest is known as the line or timberline. Arctic tundra occurs in the far Northern Hemisphere, north of the taiga belt, the word tundra usually refers only to the areas where the subsoil is permafrost, or permanently frozen soil. Permafrost tundra includes vast areas of northern Russia and Canada, the polar tundra is home to several peoples who are mostly nomadic reindeer herders, such as the Nganasan and Nenets in the permafrost area. Arctic tundra contains areas of landscape and is frozen for much of the year. The soil there is frozen from 25–90 cm down, and it is impossible for trees to grow, instead, bare and sometimes rocky land can only support low growing plants such as moss, heath, and lichen. There are two seasons, winter and summer, in the polar tundra areas. During the winter it is cold and dark, with the average temperature around −28 °C. However, extreme temperatures on the tundra do not drop as low as those experienced in taiga areas further south. During the summer, temperatures rise somewhat, and the top layer of seasonally-frozen soil melts, the tundra is covered in marshes, lakes, bogs and streams during the warm months. Generally daytime temperatures during the rise to about 12 °C. Arctic tundras are sometimes the subject of conservation programs. In Canada and Russia, many of areas are protected through a national Biodiversity Action Plan. Tundra tends to be windy, with winds often blowing upwards of 50–100 km/h, however, in terms of precipitation, it is desert-like, with only about 15–25 cm falling per year. Although precipitation is light, evaporation is also relatively minimal, there is a natural pattern of accumulation of fuel and wildfire which varies depending on the nature of vegetation and terrain
Tundra
–
Tundra in Greenland
Tundra
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Tundra in
Siberia
Tundra
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Vuntut National Park in Canada
Tundra
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A group of
muskoxen in Alaska
27.
Tropical climate
–
A tropical climate in the Köppen climate classification it is a non-arid climate in which all twelve months have mean temperatures of at least 18 °C. In tropical climates there is only two seasons, a wet season and a dry season. Tropical climates are frost-free and changes in the angle are small. In tropical climates temperature remains constant throughout the year. Within the tropical climate there are distinct varieties based on precipitation, In the Tropical rainforest climate. These climates usually occur within 5–10° latitude of the equator, in some eastern coast areas, they may extend to as much as over 26° away from the equator. This climate is dominated by the doldrums Low Pressure System all year round and it is dominated by the monsoon winds which change direction according to the seasons. This climate has a driest month with less than 60 millimetres. Examples, Southern part of Arabian Peninsula, mountaintops within the tropics, e. g. Mount Kenya, can be cold. However, like lowlands in the tropics, there is seasonal variation of temperature. Because of the effect of sun angle on climate most areas within the tropics are hot year-round, the ITCZ is shown, for July average, in the graphic. Areas of ascending air have heavy rainfall, areas of descending air are dry, the ITCZ somewhat follows the solar equator throughout the year, but with geographical variations, and in some areas is heavily influenced by local large-scale monsoons
Tropical climate
–
Beach in
Naples, Florida lined with
coconut trees is an example of a tropical climate. Although it lies in the
subtropics over a hundred miles north of the
tropic of cancer, the warm waters of the
Gulf of Mexico give it a monthly mean temperature never under 18 °C (64 °F), classifying its climate as tropical.
Tropical climate
–
Af—Tropical rainforest climate.
28.
Equator
–
The Equator usually refers to an imaginary line on the Earths surface equidistant from the North Pole and South Pole, dividing the Earth into the Northern Hemisphere and Southern Hemisphere. The Equator is about 40,075 kilometres long, some 78. 7% lies across water and 21. 3% over land, other planets and astronomical bodies have equators similarly defined. Generally, an equator is the intersection of the surface of a sphere with the plane that is perpendicular to the spheres axis of rotation. The latitude of the Earths equator is by definition 0° of arc, the equator is the only line of latitude which is also a great circle — that is, one whose plane passes through the center of the globe. The plane of Earths equator when projected outwards to the celestial sphere defines the celestial equator, in the cycle of Earths seasons, the plane of the equator passes through the Sun twice per year, at the March and September equinoxes. To an observer on the Earth, the Sun appears to travel North or South over the equator at these times, light rays from the center of the Sun are perpendicular to the surface of the Earth at the point of solar noon on the Equator. Locations on the Equator experience the quickest sunrises and sunsets because the sun moves nearly perpendicular to the horizon for most of the year. The Earth bulges slightly at the Equator, the diameter of the Earth is 12,750 kilometres. Because the Earth spins to the east, spacecraft must also launch to the east to take advantage of this Earth-boost of speed, seasons result from the yearly revolution of the Earth around the Sun and the tilt of the Earths axis relative to the plane of revolution. During the year the northern and southern hemispheres are inclined toward or away from the sun according to Earths position in its orbit, the hemisphere inclined toward the sun receives more sunlight and is in summer, while the other hemisphere receives less sun and is in winter. At the equinoxes, the Earths axis is not tilted toward the sun, instead it is perpendicular to the sun meaning that the day is about 12 hours long, as is the night, across the whole of the Earth. Near the Equator there is distinction between summer, winter, autumn, or spring. The temperatures are usually high year-round—with the exception of high mountains in South America, the temperature at the Equator can plummet during rainstorms. In many tropical regions people identify two seasons, the wet season and the dry season, but many places close to the Equator are on the oceans or rainy throughout the year, the seasons can vary depending on elevation and proximity to an ocean. The Equator lies mostly on the three largest oceans, the Pacific Ocean, the Atlantic Ocean, and the Indian Ocean. The highest point on the Equator is at the elevation of 4,690 metres, at 0°0′0″N 77°59′31″W and this is slightly above the snow line, and is the only place on the Equator where snow lies on the ground. At the Equator the snow line is around 1,000 metres lower than on Mount Everest, the Equator traverses the land of 11 countries, it also passes through two island nations, though without making a landfall in either. Starting at the Prime Meridian and heading eastwards, the Equator passes through, Despite its name, however, its island of Annobón is 155 km south of the Equator, and the rest of the country lies to the north
Equator
–
Left: A monument marking the Equator near the town of
Pontianak, Indonesia Right: Road sign marking the Equator near
Nanyuki, Kenya
Equator
Equator
–
The Equator marked as it crosses
Ilhéu das Rolas, in São Tomé and Príncipe
29.
Samoa
–
The Independent State of Samoa, commonly known as Samoa and, until 1997, known as Western Samoa, is a unitary parliamentary democracy with eleven administrative divisions. The two main islands are Savaii and Upolu with four smaller islands surrounding the landmasses, the Lapita people discovered and settled the Samoan islands around 3,500 years ago. They developed a language and cultural identity. Samoa is a member of the Commonwealth of Nations, Western Samoa was admitted to the United Nations on 15 December 1976. The entire island group, which includes American Samoa, was called Navigator Islands by European explorers before the 20th century because of the Samoans seafaring skills. The oldest date so far for remains in Samoa has been calculated by New Zealand scientists to a true age of circa 3,000 years ago from a Lapita site at Mulifanua during the 1970s. The origins of the Samoans are closely studied in research about Polynesia in various scientific disciplines such as genetics, linguistics. Contact with Europeans began in the early 18th century, jacob Roggeveen, a Dutchman, was the first known European to sight the Samoan islands in 1722. This visit was followed by French explorer Louis-Antoine de Bougainville, who named them the Navigator Islands in 1768, contact was limited before the 1830s, which is when English missionaries and traders began arriving. Christian missionary work in Samoa began in 1830 by John Williams, of the London Missionary Society arriving in Sapapalii from The Cook Islands and Tahiti. However, Robert Louis Stevenson, who lived in Samoa from 1889 until his death in 1894, wrote in A Footnote to History, Eight Years of Trouble in Samoa, … the Samoans are gentle people. The Germans in particular began to show great commercial interest in the Samoan Islands, especially on the island of Upolu, Britain also sent troops to protect British business enterprise, harbour rights, and consulate office. This was followed by a civil war, during which each of the three powers supplied arms, training and in some cases combat troops to the warring Samoan parties. The Samoan crisis came to a critical juncture in March 1889 when all three colonial contenders sent warships into Apia harbour, and a larger-scale war seemed imminent, a massive storm on 15 March 1889 damaged or destroyed the warships, ending the military conflict. The Second Samoan Civil War reached a head in 1898 when Germany, the United Kingdom, the Siege of Apia occurred in March 1899. Samoan forces loyal to Prince Tanu were besieged by a force of Samoan rebels loyal to Mataafa Iosefo. Supporting Prince Tanu were landing parties from four British and American warships, after several days of fighting, the Samoan rebels were finally defeated. American and British warships shelled Apia on 15 March 1899, including the USS Philadelphia, the eastern island-group became a territory of the United States and was known as American Samoa
Samoa
–
Studio photo depicting preparation of the
Samoa 'ava ceremony c. 1911.
Samoa
–
Flag
Samoa
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Interior of Samoan house, Apia, Urville 1842.
Samoa
–
Exiled orator Lauaki Namulauulu Mamoe
30.
Philippines
–
The Philippines, officially the Republic of the Philippines, is a sovereign island country in Southeast Asia situated in the western Pacific Ocean. It consists of about 7,641 islands that are categorized broadly under three main geographical divisions from north to south, Luzon, Visayas, and Mindanao, the capital city of the Philippines is Manila and the most populous city is Quezon City, both part of Metro Manila. The Philippines has an area of 300,000 square kilometers, and it is the eighth-most populated country in Asia and the 12th most populated country in the world. As of 2013, approximately 10 million additional Filipinos lived overseas, multiple ethnicities and cultures are found throughout the islands. In prehistoric times, Negritos were some of the archipelagos earliest inhabitants and they were followed by successive waves of Austronesian peoples. Exchanges with Chinese, Malay, Indian, and Islamic nations occurred, then, various competing maritime states were established under the rule of Datus, Rajahs, Sultans or Lakans. The arrival of Ferdinand Magellan in Homonhon, Eastern Samar in 1521 marked the beginning of Hispanic colonization, in 1543, Spanish explorer Ruy López de Villalobos named the archipelago Las Islas Filipinas in honor of Philip II of Spain. With the arrival of Miguel López de Legazpi from Mexico City, in 1565, the Philippines became part of the Spanish Empire for more than 300 years. This resulted in Roman Catholicism becoming the dominant religion, during this time, Manila became the western hub of the trans-Pacific trade connecting Asia with Acapulco in the Americas using Manila galleons. Aside from the period of Japanese occupation, the United States retained sovereignty over the islands until after World War II, since then, the Philippines has often had a tumultuous experience with democracy, which included the overthrow of a dictatorship by a non-violent revolution. It is a member of the United Nations, World Trade Organization, Association of Southeast Asian Nations, the Asia-Pacific Economic Cooperation forum. It also hosts the headquarters of the Asian Development Bank, the Philippines was named in honor of King Philip II of Spain. Spanish explorer Ruy López de Villalobos, during his expedition in 1542, named the islands of Leyte, eventually the name Las Islas Filipinas would be used to cover all the islands of the archipelago. Before that became commonplace, other such as Islas del Poniente. The official name of the Philippines has changed several times in the course of its history, during the Philippine Revolution, the Malolos Congress proclaimed the establishment of the República Filipina or the Philippine Republic. From the 1898 Treaty of Paris, the name Philippines began to appear, since the end of World War II, the official name of the country has been the Republic of the Philippines. The metatarsal of the Callao Man, reliably dated by uranium-series dating to 67,000 years ago is the oldest human remnant found in the archipelago to date and this distinction previously belonged to the Tabon Man of Palawan, carbon-dated to around 26,500 years ago. Negritos were also among the archipelagos earliest inhabitants, but their first settlement in the Philippines has not been reliably dated, there are several opposing theories regarding the origins of ancient Filipinos
Philippines
–
King Philip II of Spain.
Philippines
Philippines
–
Tabon Cave and its carvings.
Philippines
–
The
Banaue Rice Terraces where
Ifugao/Igorot utilized terrace farming in the steep mountainous regions of northern Philippines over 2000 years ago.
31.
Davao City
–
Davao City is the largest city in the Philippines in terms of land area and the most populous city in the country outside of Metro Manila and Luzon. A 1st class city on Mindanao Island with a land area of 2,444 square kilometers. This figure also makes it the city in the Philippines. It is the center of Metro Davao, the third most populous area in the Philippines. The city serves as the trade, commerce, and industry hub of Mindanao. Davao is home to Mount Apo, the highest mountain in the Philippines, the city is also nicknamed as the Durian Capital of the Philippines. For geographical and statistical purposes, Davao City is grouped with the province of Davao del Sur but is governed independently from it, the city is divided into three congressional districts, which are subdivided into 11 administrative districts with a total of 182 barangays. Davao City is constantly described by its residents and the media as arguably among one of the safest cities in the Philippines. The regions name is derived from its Bagobo origins, the Bagobo were indigenous to the Philippines. The word davao came from the blending of three Bagobo subgroups names for the Davao River, a major waterway emptying into the Davao Gulf near the city. The aboriginal Obos, who inhabit the hinterlands of the region, called the river Davah, the Clatta called it Dawaw, to the Obos, davah also means a place beyond the high grounds. When asked where they were going, the reply was davah. Davao was then ruled by a chieftain, Bago, who had a settlement on the banks of the Davao River. After Cruz de Oyanguren defeated Bago, he renamed the region Nueva Guipúzcoa, founding the town of Nueva Vergara on 29 June 1848 to honor of his home in Spain and these groups generally refer to themselves today as Kalagans. The development of large-scale plantations faced a shortage, and workers were contracted from Luzon. Many Japanese became landowners, acquiring lands by government lease or buying American plantations, the bill called for the appointment of local officials by the president. Davao was inaugurated as a city on October 16,1936 by President Manuel L. Quezon. The City of Davao became provincial capital of a united Davao Province and it was one of the first two towns in Mindanao to be converted into a city
Davao City
Davao City
Davao City
Davao City
32.
United States
–
Forty-eight of the fifty states and the federal district are contiguous and located in North America between Canada and Mexico. The state of Alaska is in the northwest corner of North America, bordered by Canada to the east, the state of Hawaii is an archipelago in the mid-Pacific Ocean. The U. S. territories are scattered about the Pacific Ocean, the geography, climate and wildlife of the country are extremely diverse. At 3.8 million square miles and with over 324 million people, the United States is the worlds third- or fourth-largest country by area, third-largest by land area. It is one of the worlds most ethnically diverse and multicultural nations, paleo-Indians migrated from Asia to the North American mainland at least 15,000 years ago. European colonization began in the 16th century, the United States emerged from 13 British colonies along the East Coast. Numerous disputes between Great Britain and the following the Seven Years War led to the American Revolution. On July 4,1776, during the course of the American Revolutionary War, the war ended in 1783 with recognition of the independence of the United States by Great Britain, representing the first successful war of independence against a European power. The current constitution was adopted in 1788, after the Articles of Confederation, the first ten amendments, collectively named the Bill of Rights, were ratified in 1791 and designed to guarantee many fundamental civil liberties. During the second half of the 19th century, the American Civil War led to the end of slavery in the country. By the end of century, the United States extended into the Pacific Ocean. The Spanish–American War and World War I confirmed the status as a global military power. The end of the Cold War and the dissolution of the Soviet Union in 1991 left the United States as the sole superpower. The U. S. is a member of the United Nations, World Bank, International Monetary Fund, Organization of American States. The United States is a developed country, with the worlds largest economy by nominal GDP. It ranks highly in several measures of performance, including average wage, human development, per capita GDP. While the U. S. economy is considered post-industrial, characterized by the dominance of services and knowledge economy, the United States is a prominent political and cultural force internationally, and a leader in scientific research and technological innovations. In 1507, the German cartographer Martin Waldseemüller produced a map on which he named the lands of the Western Hemisphere America after the Italian explorer and cartographer Amerigo Vespucci
United States
–
Native Americans meeting with Europeans, 1764
United States
–
Flag
United States
–
The signing of the
Mayflower Compact, 1620.
United States
–
The
Declaration of Independence: the
Committee of Five presenting their draft to the
Second Continental Congress in 1776
33.
Hilo, Hawaii
–
Hilo is the largest settlement and census-designated place in Hawaii County, Hawaii, which encompasses the Island of Hawaiʻi. The population was 40,759 at the 2000 census, the population increased by 6. 1% to 43,263 at the 2010 census. Hilo is the county seat of the County of Hawaiʻi and is located in the District of South Hilo, the majority of human settlement in Hilo stretches from Hilo Bay to Waiākea-Uka, on the flanks of Mauna Loa. Hilo is also home to the Mauna Loa Macadamia Nut Corporation and it is served by Hilo International Airport, located inside the CDP. Around 1100 AD, the first Hilo inhabitants arrived, bringing with them Polynesian knowledge, although archaeological evidence is scant, oral history has many references to people living in Hilo, along the Wailuku and Wailoa Rivers during the time of ancient Hawaii. Oral history also gives the meaning of Hilo as to twist, originally, the name Hilo applied to a district encompassing much of the east coast of the Island of Hawaiʻi, now divided into the District of South Hilo and the District of North Hilo. When William Ellis visited in 1823, the settlement in the Hilo district was Waiākea on the south shore of Hilo Bay. Missionaries came to the district in the early-to-middle 19th century, founding Haili Church, Hilo expanded as sugarcane plantations in the surrounding area created new jobs and drew in many workers from Asia, making the town a trading center. A breakwater across Hilo Bay was begun in the first decade of the 20th century, on April 1,1946, a 7.8 magnitude earthquake near the Aleutian Islands created a fourteen-meter high tsunami that hit Hilo 4.9 hours later, killing 160 people. In response an early warning system, the Pacific Tsunami Warning Center, was established in 1949 to track these killer waves and provide warning. This tsunami also caused the end of the Hawaii Consolidated Railway, and instead the Hawaii Belt Road was built north of Hilo using some of the old railbed. On May 23,1960, another tsunami, caused by a 9.5 magnitude earthquake off the coast of Chile the previous day, claimed 61 lives, allegedly due to the failure of people to heed warning sirens. Low-lying bayfront areas of the city on Waiākea peninsula and along Hilo Bay, previously populated, were rededicated as parks, Hilo expanded inland beginning in the 1960s. The downtown found a new role in the 1980s as the cultural center with several galleries and museums being opened. Closure of the plantations during the 1990s led to a downturn in the local economy. Hilo in recent years has seen commercial and population growth, as the neighboring District of Puna became the region in the state. Hilo is located at 19°42′20″N 155°5′9″W, Hilo features a tropical rainforest climate, with substantial rainfall throughout the course of the year. An average of around 126.72 inches of rain fell at Hilo International Airport annually between 1981 and 2010, with 272 days of the year receiving some rain
Hilo, Hawaii
–
Top:
S. Hata Building. Upper Left: Hilo Masonic Lodge Hall. Upper Right:
Hilo Bay with
Mauna Kea. Lower Left:
Rainbow Falls (Hawaii). Lower Right:
Federal Building, United States Post Office and Courthouse (Hilo, Hawaii). Bottom:
Liliuokalani Park and Gardens.
Hilo, Hawaii
–
Location in
Hawaii County and the state of
Hawaii
34.
Australia
–
Australia, officially the Commonwealth of Australia, is a country comprising the mainland of the Australian continent, the island of Tasmania and numerous smaller islands. It is the worlds sixth-largest country by total area, the neighbouring countries are Papua New Guinea, Indonesia and East Timor to the north, the Solomon Islands and Vanuatu to the north-east, and New Zealand to the south-east. Australias capital is Canberra, and its largest urban area is Sydney, for about 50,000 years before the first British settlement in the late 18th century, Australia was inhabited by indigenous Australians, who spoke languages classifiable into roughly 250 groups. The population grew steadily in subsequent decades, and by the 1850s most of the continent had been explored, on 1 January 1901, the six colonies federated, forming the Commonwealth of Australia. Australia has since maintained a liberal democratic political system that functions as a federal parliamentary constitutional monarchy comprising six states. The population of 24 million is highly urbanised and heavily concentrated on the eastern seaboard, Australia has the worlds 13th-largest economy and ninth-highest per capita income. With the second-highest human development index globally, the country highly in quality of life, health, education, economic freedom. The name Australia is derived from the Latin Terra Australis a name used for putative lands in the southern hemisphere since ancient times, the Dutch adjectival form Australische was used in a Dutch book in Batavia in 1638, to refer to the newly discovered lands to the south. On 12 December 1817, Macquarie recommended to the Colonial Office that it be formally adopted, in 1824, the Admiralty agreed that the continent should be known officially as Australia. The first official published use of the term Australia came with the 1830 publication of The Australia Directory and these first inhabitants may have been ancestors of modern Indigenous Australians. The Torres Strait Islanders, ethnically Melanesian, were originally horticulturists, the northern coasts and waters of Australia were visited sporadically by fishermen from Maritime Southeast Asia. The first recorded European sighting of the Australian mainland, and the first recorded European landfall on the Australian continent, are attributed to the Dutch. The first ship and crew to chart the Australian coast and meet with Aboriginal people was the Duyfken captained by Dutch navigator, Willem Janszoon. He sighted the coast of Cape York Peninsula in early 1606, the Dutch charted the whole of the western and northern coastlines and named the island continent New Holland during the 17th century, but made no attempt at settlement. William Dampier, an English explorer and privateer, landed on the north-west coast of New Holland in 1688, in 1770, James Cook sailed along and mapped the east coast, which he named New South Wales and claimed for Great Britain. The first settlement led to the foundation of Sydney, and the exploration, a British settlement was established in Van Diemens Land, now known as Tasmania, in 1803, and it became a separate colony in 1825. The United Kingdom formally claimed the part of Western Australia in 1828. Separate colonies were carved from parts of New South Wales, South Australia in 1836, Victoria in 1851, the Northern Territory was founded in 1911 when it was excised from South Australia
Australia
–
Aboriginal rock art in the
Kimberley region of Western Australia
Australia
Australia
–
Portrait of Captain
James Cook, the first European to map the eastern coastline of Australia in 1770
Australia
–
Tasmania's
Port Arthur penal settlement is one of eleven UNESCO World Heritage-listed
Australian Convict Sites.
35.
Innisfail, Queensland
–
Innisfail a town and locality in the Cassowary Coast Region in Far North Queensland, Australia. The town was originally called Geraldton until 1910 and it is the major township of the Cassowary Coast Region and is well renowned for its sugar and banana industries, as well as for being one of Australias wettest towns. In March 2006 Innisfail gained worldwide attention when severe Tropical Cyclone Larry passed over causing extensive damage, in the 2011 census, the town of Innisfail had a population of 7,176 people. Prior to European settlement the Innisfail area was occupied by five separate societies of the Mamu people and these Aboriginal people followed migratory lifestyles in the rainforest and traversed rivers in string-bark canoes. The first arrival of European people came in 1872 when survivors of the shipwreck, sub-Inspector Robert Arthur Johnstones search party came with the intention of rescuing remaining survivors. The crew would later venture up river between what is today Flying Fish Point and Coquette Point, Johnstone named the area after himself and upon his recommendation the explorer George Elphinstone Dalrymple arrived in the area in September 1873 to chart the area further. Later in 1879, Irishman Thomas Henry FitzGerald arrived in the area to establish a sugar industry and he was accompanied by large numbers of Kanaka South Sea Islanders workers accompanied by smaller numbers of Irish labourers. The house built by FitzGerald and thus the first establishment in the area was called Innisfallen, after the largest island in the Lakes of Killarney, inis Fáil is an ancient Irish name for Ireland itself. The name is used in the third verse of The Soldiers Song. The stone mentioned may be the stone at Tara, Co Meath, from 1879, the settlement was named Geraldton after FitzGerald, but in 1910 was renamed Innisfail to avoid confusion with the town of the same name in Western Australia. Johnstone River Post Office opened on 1 November 1882, was renamed Geraldton two months later and Innisfail in 1910, in 1906 Patrick Leahy established the Johnstone River Advocate newspaper. Later it was renamed the Johnstone River Advocate and Innisfail News, the Evening Advocate, the newspaper continues to be published as the Innisfail Advocate. The 1920s and 1930s saw the beginning of a period of settlement by Italian immigrants and noteworthy populations from Greece. Later in this period populations from Yugoslavia, India and the Philippines would also settle in the area, local rugby league footballer Kerry Boustead was the only player from outside the Sydney and Brisbane Leagues selected to represent Australia on the 1978 Kangaroo tour. The Innisfail War Memorial in Jack Fossey Park on Fitzgerald Esplanade was dedicated on 16 April 2005, in the 2006 census, Innisfail had a population of 8,262 people. Today the town still boasts many examples of the Art Deco. In 2001 Los Angeles band Sugar Ray filmed part of their music DVD Music in High Places at the Johnstone Crocodile Farm in Innisfail, being a small community, and one that was recently subjected to a severe natural disaster Innisfail harbours a definite sense of community. The township has only 2 secondary schools, Good Counsel College and Innisfail State College, in the past Chinese Australians built the Innisfail Temple/Lit Sing Gung
Innisfail, Queensland
–
The township of Innisfail, as seen from Coquette Point
Innisfail, Queensland
–
Innisfail War Memorial, 2006
Innisfail, Queensland
–
Court house
Innisfail, Queensland
–
A large turnout of the Annual
Harvest Festival Parade in 2005
36.
Uganda
–
Uganda, officially the Republic of Uganda, is a landlocked country in East Africa. It is bordered to the east by Kenya, to the north by South Sudan, to the west by the Democratic Republic of the Congo, to the south-west by Rwanda, Uganda is the worlds second most populous landlocked country after Ethiopia. The southern part of the country includes a portion of Lake Victoria, shared with Kenya. Uganda is in the African Great Lakes region, Uganda also lies within the Nile basin, and has a varied but generally a modified equatorial climate. Uganda takes its name from the Buganda kingdom, which encompasses a portion of the south of the country. The people of Uganda were hunter-gatherers until 1,700 to 2,300 years ago, beginning in 1894, the area was ruled as a protectorate by the British, who established administrative law across the territory. Uganda gained independence from Britain on 9 October 1962, luganda, a central language, is widely spoken across the country, and several other languages are also spoken including Runyoro, Runyankole, Rukiga, and Luo. The president of Uganda is Yoweri Museveni, who came to power in January 1986 after a protracted guerrilla war. The ancestors of the Ugandans were hunter-gatherers until 1, 700-2,300 years ago, Bantu-speaking populations, who were probably from central Africa, migrated to the southern parts of the country. According to oral tradition, the Empire of Kitara covered an important part of the lakes area, from the northern lakes Albert and Kyoga to the southern lakes Victoria. Bunyoro-Kitara is claimed as the antecedent of the Buganda, Toro, Ankole, some Luo invaded the area of Bunyoro and assimilated with the Bantu there, establishing the Babiito dynasty of the current Omukama of Bunyoro-Kitara. Arab traders moved inland from the Indian Ocean coast of East Africa in the 1830s and they were followed in the 1860s by British explorers searching for the source of the Nile. British Anglican missionaries arrived in the kingdom of Buganda in 1877 and were followed by French Catholic missionaries in 1879, the British government chartered the Imperial British East Africa Company to negotiate trade agreements in the region beginning in 1888. From 1886, there were a series of wars in Buganda. Because of civil unrest and financial burdens, IBEAC claimed that it was unable to maintain their occupation in the region, in the 1890s,32,000 labourers from British India were recruited to East Africa under indentured labour contracts to construct the Uganda Railway. Most of the surviving Indians returned home, but 6,724 decided to remain in East Africa after the lines completion, subsequently, some became traders and took control of cotton ginning and sartorial retail. British naval ships unknowingly carried rats that contained the bubonic plague and these rats spread the disease throughout Uganda. From 1900 to 1920, a sleeping sickness epidemic in the part of Uganda, along the north shores of Lake Victoria
Uganda
–
Left: Construction of the
Owen Falls Dam in
Jinja. Right: A street in Uganda in the 1950s.
Uganda
–
Flag
Uganda
Uganda
–
Mount Kadam, Uganda.
37.
Kampala
–
Kampala is the capital and largest city of Uganda. The city is divided into five boroughs that oversee local planning, Kampala Central Division, Kawempe Division, Makindye Division, Nakawa Division, the city is coterminous with Kampala District. Surrounding Kampala is the rapidly growing Wakiso District, whose more than doubled between 2002 and 2014 and now stands at over 2 million. Kampala was named the 13th fastest growing city on the planet, with a population growth rate of 4.03 percent. Kampala has been ranked the best city to live in East Africa ahead of Nairobi and Kigali by Mercer, in December 2015, Google launched its first wi-fi network in Kampala. Before the arrival of the British colonists, the Kabaka of Buganda had chosen the zone that would become Kampala as a hunting reserve, the area, composed of rolling hills with grassy wetlands in the valleys, was home to several species of antelope, particularly impala. When the British arrived, they called it Hills of the Impala, the language of the Buganda, Luganda, adopted many English words because of their interactions with the British. The Buganda translated Hill of the Impala as Akasozi keEmpala - Kasozi meaning hill, ke meaning of, and empala the plural of impala. In Luganda, the words mean that is of the impala, in reference to a hill. The city grew as the capital of the Buganda kingdom, from several buildings survive, including the Kasubi Tombs, the Lubiri Palace, the Buganda Parliament. In 1894, the British government officially established a protectorate within this territory, and in 1896, the protectorate expanded to cover the Ankole, Toro Kingdom, in 1905, the British government formally declared the entire territory to be a British colony. From that time until the independence of the country in 1962, following the 1962 independence, Milton Obote became president of Uganda, and held the position until 1971, when former sergeant Idi Amin defeated his government in a military coup. He proceeded to expel all Asian residents living within Kampala, in 1978, he invaded the neighboring country of Tanzania, and in turn, the government there started the Uganda–Tanzania War, which created severe damage to the buildings of Kampala. Traditionally, Kampala was a city of seven hills, but over time it has come to have a lot more, the main campus of Makerere University is in the Makerere Hill area of the city. Kampala also hosts the headquarters of the East African Development Bank on Nakasero Hill, Kampala was originally built on seven hills, but as its size has increased, it has expanded to more hills than seven. The original seven hills are, The first hill in historical importance is Kasubi Hill, the third is Kibuli Hill, which is home to the Kibuli Mosque. The fourth is Namirembe Hill, home to the Namirembe Anglican Cathedral, the fifth is Lubaga Hill, the site of the Rubaga Catholic Cathedral. A mosque was built with assistance from Libya on the hill in 2003
Kampala
–
From left to right: Kampala skyline,
Bahá'í House of Worship on
Kikaaya Hill,
Uganda National Mosque,
Makerere University main building, skyscraper in central business district, and view over
Victoria Lake
Kampala
–
View of Kampala from space
Kampala
–
Gaddafi National Mosque.
Kampala
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Uganda House, Kampala Road, Kampala
38.
Democratic Republic of the Congo
–
The Democratic Republic of the Congo, also known as DR Congo, DRC, DROC, East Congo, Congo-Kinshasa, or simply the Congo is a country located in Central Africa. From 1971 to 1997 it was named, and is still called, Zaire. It is the second-largest country in Africa by area and eleventh largest in the world, the Congolese Civil Wars, which began in 1996, brought about the end of Mobutu Sese Sekos 32-year reign and devastated the country. These wars ultimately involved nine African nations, multiple groups of UN peacekeepers and twenty armed groups, besides the capital, Kinshasa, the other major cities, Lubumbashi and Mbuji-Mayi, are both mining communities. DR Congos largest export is raw minerals, with China accepting over 50% of DRCs exports in 2012, as of 2015, according to the Human Development Index, DR Congo has a low level of human development, ranking 176 out of 187 countries. The country was known officially as the Democratic Republic of the Congo from 1965 to 27 October 1971, in 1992, the Sovereign National Conference voted to change the name of the country to the Democratic Republic of the Congo, but the change was not put into practice. The countrys name was restored by former president Laurent-Désiré Kabila following the fall of longtime dictator Mobutu Sese Seko in 1997, some historians think that Bantu peoples began settling in the extreme northwest of Central Africa at the beginning of the 5th century and then gradually started to expand southward. Their propagation was accelerated by the transition from Stone Age to Iron Age techniques, the people living in the south and southwest were mostly San Bushmen and hunter-gatherer groups, whose technology involved only minimal use of metal technologies. The development of tools during this time period revolutionized agriculture. This led to the displacement of the groups in the east and southeast. The 10th century marked the expansion of the Bantu in West-Central Africa. Rising populations soon made intricate local, regional and foreign commercial networks that traded mostly in salt, iron. Belgian exploration and administration took place from the 1870s until the 1920s and it was first led by Sir Henry Morton Stanley, who undertook his explorations under the sponsorship of King Leopold II of Belgium. The eastern regions of the precolonial Congo were heavily disrupted by constant slave raiding, mainly from Arab–Swahili slave traders such as the infamous Tippu Tip, Leopold had designs on what was to become the Congo as a colony. Leopold formally acquired rights to the Congo territory at the Conference of Berlin in 1885 and he named it the Congo Free State. Leopolds rėgime began various infrastructure projects, such as construction of the railway ran from the coast to the capital of Leopoldville. Nearly all such projects were aimed at making it easier to increase the assets which Leopold. In the Free State, colonists brutalized the local population into producing rubber, for which the spread of automobiles, rubber sales made a fortune for Leopold, who built several buildings in Brussels and Ostend to honor himself and his country
Democratic Republic of the Congo
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Village attacked by Arab-Swahili slavers near
Nyangwe, end of 19th century
Democratic Republic of the Congo
–
Flag
Democratic Republic of the Congo
–
View of
Leopoldville Station and Port in 1884.
Democratic Republic of the Congo
–
Force Publique soldiers in the Belgian Congo in 1918. At its peak, the Force Publique had around 19,000 African soldiers, led by 420 white officers.
39.
Kisangani
–
Kisangani /kiːsəŋˈɡɑːni/ is the capital of Orientale Province in the Democratic Republic of the Congo. It is the third largest urbanized city in the country and the largest of the cities lie in the tropical woodlands of the Congo. Singitini as rendered in Lingala, each of which share the same meaning the City on the Island and it is also known as Kisangani Boyoma, and the demonym for Kisangani is Boyoman. The languages most spoken at home by the population in the city are Swahili and Lingala, the official language of Kisangani is French, as defined by the Constitution of the Democratic Republic of the Congo. Some 1300 mi from the mouth of the Congo River, Kisangani is the farthest navigable point upstream and it has been the commercial capital of the northern Congo since the late 19th century. Kisangani has been home to politicians, including the national hero, Patrice Emery Lumumba. The city is also the birthplace of the University of Kisangani graduate, entrepreneur and current governor of Orientale Province, henry Morton Stanley founded Stanley Falls Station in 1883, on the Island of Wana Rusari in the Congo River near the present town of Kisangani. During the mid-19th century the area was inhabited by a native Congolese tribe known as the Clans of Enya, the island is located a few meters from the shore site of the present town on the Lualaba River its 7 falls spread over 100 km between Kisangani and Ubundu. Some 1,300 miles from the mouth of the Congo River, the city was known first as Falls Station and then with Belgian colonization of the area, it grew into a settlement called Stanleyville. A city terminus of steamer navigation on the Congo River, the town began as a Belgian trading post and it has been the major centre of the northern Congo since the late 19th century. Stanley left Mr. Binnie, an engineer and a Scotsman, in charge to trade with the local people, the name Kisangani was apparently used consistently by the local people, in conjunction with the name Stanleyville. In Swahili the manual published by the Marist Brothers in the 1920s, the name Kisangani is a Swahili rendering of the indigenous Congolese language word Boyoma, meaning City on the Island, also rendered in Lingala as Singitini with the same meaning. Relations between Free State Officials and the slavers were strained and after a fight the Station was abandoned in 1887, ultimately the Europeans gained complete control of the vast area in central Africa. On 15 July 1898, Stanleyville began serving as the capital of the relatively prosperous District of the Eastern Province Stanley Falls, City status was achieved by incorporation Order No. 12/357 on 6 September 1958, which divided Stanleyville into 4 municipalities, Belgian I, Belgian II, Brussels, towards the end of 1958, the city became the stronghold of Patrice Emery Lumumba, the leader of the political party Mouvement National Congolais. His strong ties with the city had been forged during his days as one of 350 clerks at the central post office, ethiopian ONUC troops arrived in the city after July 1960. After the assassination of Lumumba in 1961, Antoine Gizenga installed a government that competed with the government in Leopoldville. Before the country gained independence from Belgium in 1960, Kisangani was reputed to have more Rolls-Royces per capita than any city in the world
Kisangani
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Kisangani
Kisangani
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Belgo-Arab War at the Arab stronghold,
Nyangwe Circa 1892–1894
Kisangani
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Stanley Falls Station, map plan in 1893, laying the foundations of Kisangani
Kisangani
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Wagenya fishermen
40.
Malaysia
–
Malaysia is a federal constitutional monarchy located in Southeast Asia. Peninsular Malaysia shares a land and maritime border with Thailand and maritime borders with Singapore, Vietnam, East Malaysia shares land and maritime borders with Brunei and Indonesia and a maritime border with the Philippines and Vietnam. The capital city is Kuala Lumpur, while Putrajaya is the seat of the federal government, with a population of over 30 million, Malaysia is the 44th most populous country. The southernmost point of continental Eurasia, Tanjung Piai, is in Malaysia, located in the tropics, Malaysia is one of 17 megadiverse countries on earth, with large numbers of endemic species. Malaysia has its origins in the Malay kingdoms present in the area which, from the 18th century, the first British territories were known as the Straits Settlements, whose establishment was followed by the Malay kingdoms becoming British protectorates. The territories on Peninsular Malaysia were first unified as the Malayan Union in 1946, Malaya was restructured as the Federation of Malaya in 1948, and achieved independence on 31 August 1957. Malaya united with North Borneo, Sarawak, and Singapore on 16 September 1963 to become Malaysia, less than two years later in 1965, Singapore was expelled from the federation. The country is multi-ethnic and multi-cultural, which plays a role in politics. About half the population is ethnically Malay, with minorities of Malaysian Chinese, Malaysian Indians. The constitution declares Islam the state religion while allowing freedom of religion for non-Muslims, the government system is closely modelled on the Westminster parliamentary system and the legal system is based on common law. The head of state is the king, known as the Yang di-Pertuan Agong and he is an elected monarch chosen from the hereditary rulers of the nine Malay states every five years. The head of government is the prime minister, since its independence, Malaysia has had one of the best economic records in Asia, with its GDP growing at an average of 6. 5% per annum for almost 50 years. The economy has traditionally been fuelled by its resources, but is expanding in the sectors of science, tourism, commerce. Today, Malaysia has a newly industrialised market economy, ranked third largest in Southeast Asia, the name Malaysia is a combination of the word Malay and the Latin-Greek suffix -sia/-σία. The word melayu in Malay may derive from the Tamil words malai and ur meaning mountain and city, land, malayadvipa was the word used by ancient Indian traders when referring to the Malay Peninsula. Whether or not it originated from these roots, the word melayu or mlayu may have used in early Malay/Javanese to mean to steadily accelerate or run. This term was applied to describe the current of the river Melayu in Sumatra. The name was adopted by the Melayu Kingdom that existed in the seventh century on Sumatra
Malaysia
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"Malaysia" used as a label for the
Malay Archipelago on a 1914 map from a United States atlas
Malaysia
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Flag
Malaysia
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The Dutch fleet battling with the Portuguese armada as part of the
Dutch–Portuguese War in 1606 to gain control of
Malacca.
Malaysia
–
Statue of
Francis Light in the
Fort Cornwallis of Penang, marking the first step of
British expansion in the 18th century over the Malay Archipelago.
41.
Kuala Lumpur
–
Kuala Lumpur, officially the Federal Territory of Kuala Lumpur, or more commonly called KL is the national capital of Malaysia as well as its largest city. Being rated as an Alpha world city, Kuala Lumpur is the global city in Malaysia which covers an area of 243 km2 and has an estimated population of 1.73 million as of 2016. Greater Kuala Lumpur, also known as the Klang Valley, is an agglomeration of 7.25 million people as of 2017. It is among the fastest growing regions in South-East Asia, in terms of population. Kuala Lumpur is the seat of the Parliament of Malaysia, the city was once home to the executive and judicial branches of the federal government, but they were moved to Putrajaya in early 1999. Some sections of the judiciary still remain in the city of Kuala Lumpur. The official residence of the Malaysian King, the Istana Negara, is situated in Kuala Lumpur. Kuala Lumpur is the cultural, financial and economic centre of Malaysia due to its position as the capital as well as being a key city. Kuala Lumpur is one of three Federal Territories of Malaysia, enclaved within the state of Selangor, on the central west coast of Peninsular Malaysia. Since the 1990s, the city has played host to international sporting, political and cultural events including the 1998 Commonwealth Games. Kuala Lumpur has undergone rapid development in recent decades and it is home to the tallest twin buildings in the world, the Petronas Twin Towers, which have become an iconic symbol of Malaysias futuristic development. Kuala Lumpur means muddy confluence, kuala is the point where two rivers join together or an estuary, and lumpur means mud. One suggestion is that it was named after Sungai Lumpur, it was recorded in 1824 that Sungei Lumpoor was the most important tin-producing settlement up the Klang River. It has also proposed that Kuala Lumpur was originally named Pengkalan Lumpur in the same way that Klang was once called Pengkalan Batu. Another suggestion is that it was initially a Cantonese word lam-pa meaning flooded jungle or decayed jungle, there is however no firm contemporary evidence for these suggestions other than anecdotes. It is also possible that the name is a form of an earlier. It is unknown who founded or named the settlement called Kuala Lumpur, Kuala Lumpur was originally a small hamlet of just a few houses and shops at the confluence of Sungai Gombak and Sungai Klang before it grew into a town. The miners landed at Kuala Lumpur and continued their journey on foot to Ampang where the first mine was opened
Kuala Lumpur
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Clockwise from top left:
Petronas Twin Towers,
Petaling Street, Masjid Jamek and
Gombak /
Klang river confluence,
National Monument,
National Mosque, skyline of KL. Centre:
KL Tower
Kuala Lumpur
–
Jamek Mosque at the confluence of
Gombak (left) and
Klang (right) rivers. The earliest settlement of Kuala Lumpur developed on the eastern side of the river bank (to the right in this picture).
Kuala Lumpur
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Japanese troops advancing up High Street (now
Jalan Tun H S Lee) in Kuala Lumpur in December 1941 during
World War II.
Kuala Lumpur
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The Majestic Theatre on Pudu Road was an early pioneer in Kuala Lumpur's cinema scene. It was converted into an amusement park in the 1990s and demolished in 2009.
42.
Kuching
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Kuching /ˈkuːtʃɪŋ/, officially the City of Kuching, is the capital and the most populous city in the state of Sarawak in Malaysia. It is also the capital of Kuching Division, Kuching was the third capital of Sarawak in 1827 during the administration of the Bruneian Empire. The town continued to receive attention and development during the rule of Charles Brooke such as the construction of a system, hospital, prison, fort. In 1941, the Brooke administration had a Centenary Celebration in Kuching, during World War II, Kuching was occupied by Japanese forces from 1942 to 1945. The Japanese government set up a Batu Lintang camp near Kuching to hold prisoners of war, after the war, the town survived intact. However, the last Rajah of Sarawak, Sir Charles Vyner Brooke decided to cede Sarawak as part of British Crown Colony in 1946, Kuching remained as capital during the Crown Colony period. After the formation of Malaysia in 1963, Kuching retained its status as capital and was granted city status in 1988. Since then, the Kuching city is divided into two administrative regions managed by two local authorities. The administrative centre of Sarawak state government is located at Wisma Bapa Malaysia, Kuching is a major food destination for tourists and the main gateway for travellers visiting Sarawak and Borneo. The city has one of the major industrial and commercial centres in East Malaysia. The name of Kuching was already in use for the city by the time Brooke arrived in 1841, there are many theories as to the derivation of the word Kuching. It was perhaps derived from the Malay word for cat, kucing or from Cochin, an Indian trading port on the Malabar Coast, some Hindu artefacts can be seen today at the Sarawak State Museum. However, another source reported that the Kuching city was known as Sarawak before the Brooke arrived. The settlement was renamed to Sarawak proper during the kingdom expansion and it was only in 1872 that Charles Brooke renamed the settlement to Kuching. There was one unlikely theory based on a story on miscommunication, according to the story, James Brooke arrived in Kuching on his yacht Royalist. He then asked his local guide about the name of the town, the local guide thinking that James Brooke was pointing towards a cat, and said the word Kuching. However, ethnic Malays in Sarawak usually refer the name of a cat as pusak instead of the Malay word kucing, some source also stated that it was derived from a fruit called mata kucing, a fruit that grows widely in Malaysia and Indonesia. There was also a hill in the city that was named after the fruit, which is called Bukit Mata Kuching
Kuching
–
These statues of
cats became a symbol of Kuching City.
Kuching
Kuching
–
Kuching was later established as the seat of Brooke government under the management of Sir
James Brooke.
Kuching
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The Kuching state prison was situated beside the Square Tower building in 1896.
43.
Indonesia
–
Indonesia, officially the Republic of Indonesia, is a unitary sovereign state and transcontinental country located mainly in Southeast Asia with some territories in Oceania. Situated between the Indian and Pacific oceans, it is the worlds largest island country, with more than seventeen thousand islands. At 1,904,569 square kilometres, Indonesia is the worlds 14th-largest country in terms of area and worlds 7th-largest country in terms of combined sea. It has an population of over 260 million people and is the worlds fourth most populous country. The worlds most populous island, Java, contains more than half of the countrys population, Indonesias republican form of government includes an elected legislature and president. Indonesia has 34 provinces, of which five have Special Administrative status and its capital and countrys most populous city is Jakarta, which is also the most populous city in Southeast Asia and the second in Asia. The country shares land borders with Papua New Guinea, East Timor, other neighbouring countries include Singapore, Vietnam, the Philippines, Australia, Palau, and the Indian territory of the Andaman and Nicobar Islands. Despite its large population and densely populated regions, Indonesia has vast areas of wilderness that support the second highest level of biodiversity. The country has abundant natural resources like oil and natural gas, tin, copper, agriculture mainly produces rice, palm oil, tea, coffee, cacao, medicinal plants, spices and rubber. Indonesias major trading partners are Japan, United States, China, the Indonesian archipelago has been an important region for trade since at least the 7th century, when Srivijaya and then later Majapahit traded with China and India. Local rulers gradually absorbed foreign cultural, religious and political models from the early centuries CE, Indonesian history has been influenced by foreign powers drawn to its natural resources. Indonesia consists of hundreds of native ethnic and linguistic groups. The largest – and politically dominant – ethnic group are the Javanese, a shared identity has developed, defined by a national language, ethnic diversity, religious pluralism within a Muslim-majority population, and a history of colonialism and rebellion against it. Indonesias national motto, Bhinneka Tunggal Ika, articulates the diversity that shapes the country, Indonesias economy is the worlds 16th largest by nominal GDP and the 8th largest by GDP at PPP, the largest in Southeast Asia, and is considered an emerging market and newly industrialised country. Indonesia has been a member of the United Nations since 1950, Indonesia is a member of the G20 major economies and World Trade Organization. The name Indonesia derives from the Greek name of the Indós, the name dates to the 18th century, far predating the formation of independent Indonesia. In 1850, George Windsor Earl, an English ethnologist, proposed the terms Indunesians—and, his preference, in the same publication, one of his students, James Richardson Logan, used Indonesia as a synonym for Indian Archipelago. However, Dutch academics writing in East Indies publications were reluctant to use Indonesia, they preferred Malay Archipelago, the Netherlands East Indies, popularly Indië, the East, and Insulinde
Indonesia
–
A
Borobudur ship carved on
Borobudur, c. 800 CE. Indonesian outrigger boats may have made trade voyages to the east coast of Africa as early as the 1st century CE.
Indonesia
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Flag
Indonesia
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The
nutmeg plant is native to Indonesia's
Banda Islands.
Indonesia
–
Tan Malaka, Indonesian philosopher, guerilla, and national hero.
44.
Medan
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Medan is the capital of North Sumatra province in Indonesia. Located along the northeastern coast of Sumatra Island, Medan is the third biggest city in Indonesia, behind Jakarta, with 2,097,610 inhabitants at the 2010 census, Medan remains the largest settlement outside of Java Island. Bordered by the Strait of Malacca, Medan is a trading city as the strait is one of the most important shipping lanes in the world. Medan is the gateway to the part of Indonesia, accessible via the Port of Belawan. Both the seaport and the airport are connected to the city center via toll road, Medan became the first city in Indonesia to have an airport supported with train service. The city was founded by Guru Patimpus, a Karonese man who named a swampy land in confluence of Deli River, in 1632, the Deli Sultanate was established by Tuanku Gocah Pahlawan, who became its first king. In the 18th century, the king, Sultan Mahmud Al Rasyid Perkasa Alam. Jacob Nienhuys, a Dutch tobacco merchant, pioneered the opening of plantations in Deli Land. The areas name changed to Medan-Deli when it was established by Dutch tobacco commerce after the formation of the Deli Company. The Deli Railway was established for shipping rubber, tea, timber, palm oil, and sugar industries from the city to Belawan, following the establishment of the Republic of Indonesia, Medan became the capital of North Sumatra in mid-1950. Medan was dubbed by the Dutch Parijs van Sumatra due to the resemblance to Paris. Residential property prices in Medan have also trended upward over the period from 2013 to the first quarter of 2015, according to Bank Indonesia. According to BI, Medan’s residential property price index rose from 205.24 in the quarter of 2013 to 212.17 in the fourth quarter of 2014. One of the Karo-Indonesia dictionaries written by Darwin Prinst SH published in 2002 stated that Medan could also be defined as recover or be better, in ancient times the city of Medan was known as Kampung Medan. It was a piece of land with an area of approximately 4000 ha. Some of the crossing the city of Medan drain into the Straits of Malacca. These rivers are Sei Deli, Sei Babura, Sei Sikambing, Sei Denai, Sei Putih, Sei Percut, Medan started as a village called Kampung Medan. Kampung Medan was founded by Guru Patimpus Sembiring Pelawi, a Karonese man who came from the Karo Land, before he became a Muslim, he was a Pemena follower
Medan
–
Skyline of Medan, 2013
Medan
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Portrait of
Sultan Ma'mun Al Rasyid Perkasa Alam, 1900s.
Medan
–
Aerial view of Medan in 1931.
Medan
–
Tjong A Fie, a
kapitan of Medan and one of contributor to the early development in the city.
45.
Suriname
–
Suriname, officially known as the Republic of Suriname, is a sovereign state on the northeastern Atlantic coast of South America. It is bordered by French Guiana to the east, Guyana to the west, at just under 165,000 square kilometers, it is the smallest country in South America. Suriname has a population of approximately 566,000, most of live on the countrys north coast, in and around the capital and largest city. Long inhabited by cultures of indigenous tribes, Suriname was explored and contested by European powers before coming under Dutch rule in the late 17th century. In 1954, the country one of the constituent countries of the Kingdom of the Netherlands. Its indigenous peoples have been active in claiming land rights and working to preserve their traditional lands. Suriname is considered to be a culturally Caribbean country, and is a member of the Caribbean Community, while Dutch is the official language of government, business, media, and education, Sranan, an English-based creole language, is a widely used lingua franca. Suriname is the territory outside Europe where Dutch is spoken by a majority of the population. The people of Suriname are among the most diverse in the world, spanning a multitude of ethnic, religious, and linguistic groups. This area was occupied by cultures of indigenous peoples long before European contact, remnants of which can be found in petroglyph sites at Werehpai. The name Suriname may derive from a Taino indigenous people called Surinen, British settlers, who founded the first European colony at Marshalls Creek along the Suriname River, spelled the name as Surinam. When the territory was taken over by the Dutch, it part of a group of colonies known as Dutch Guiana. The official spelling of the countrys English name was changed from Surinam to Suriname in January 1978, a notable example is Surinames national airline, Surinam Airways. The older English name is reflected in the English pronunciation, /ˈsʊrᵻnæm/ or /ˈsʊrᵻnɑːm/, in Dutch, the official language of Suriname, the pronunciation is, with the main stress on the third syllable and a schwa terminal vowel. Indigenous settlement of Suriname dates back to 3,000 BC, the largest tribes were the Arawak, a nomadic coastal tribe that lived from hunting and fishing. They were the first inhabitants in the area, the Carib also settled in the area and conquered the Arawak by using their superior sailing ships. They settled in Galibi at the mouth of the Marowijne River, while the larger Arawak and Carib tribes lived along the coast and savanna, smaller groups of indigenous peoples lived in the inland rainforest, such as the Akurio, Trió, Warrau, and Wayana. Beginning in the 16th century, French, Spanish, and English explorers visited the area, a century later, Dutch and English settlers established plantation colonies along the many rivers in the fertile Guiana plains
Suriname
–
Maroon village,
Suriname River, 1955
Suriname
–
Flag
Suriname
–
Presidential Palace of Suriname
Suriname
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Waterfront houses in
Paramaribo, 1955
46.
Paramaribo
–
Paramaribo is the capital and largest city of Suriname, located on the banks of the Suriname River in the Paramaribo District. Paramaribo has a population of roughly 240,000 people, almost half of Surinames population, the historic inner city of Paramaribo has been a UNESCO World Heritage Site since 2002. The city is named for the Paramaribo tribe living at the mouth of the Suriname River, the name Paramaribo is probably a corruption of the name of an Indian village, Parmirbo. This was the location of the first Dutch settlement, a trading post established by Nicolaes Baliestel, English and French traders also tried to establish settlements in Suriname, including a French post established in 1644 near present-day Paramaribo. The Dutch settlement was abandoned some time before the arrival of English settlers in 1650, the settlers were sent by the English governor of Barbados, Lord Francis Willoughby, 5th Baron Willoughby of Parham, and established a town on the site of Paramaribo. The town was protected by a fort, called Fort Willoughby, in 1662, Governor Willoughby was granted the settlement and surrounding lands by King Charles II. In 1667, during the Second Anglo-Dutch War, Paramaribo was conquered by a squadron of ships under Abraham Crijnssen, the Treaty of Breda in 1667, confirmed Paramaribo as the leading town of the now Dutch colony of Suriname. The fort protecting Paramaribo was renamed Fort Zeelandia in honor of the Dutch province that had financed Crijnssen’s fleet, the population of Paramaribo has always been very diverse. Among the first British settlers were many Jews and one of the oldest synagogues in the Americas is found in Paramaribo, the population of the town was greatly increased after 1873, when former slaves were allowed to stop working for their former masters and leave the sugar plantations. Paramaribo has remained the capital of Suriname, from its colonial days through the independence of Suriname in 1975 to the present day, the old town has suffered many devastating fires over the years, notably in January 1821 and September 1832. In 1987 an administrative reorganization took place in Suriname and the city was divided into 12 administrative jurisdictions, the city is located on the Suriname River, approximately 15 kilometres inland from the Atlantic Ocean, in the Paramaribo district. Evolution of Paramaribo Paramaribo features a tropical rainforest climate, under the Köppen climate classification, the city has no true dry season, all 12 months of the year average more than 60 mm of rainfall, but the city does experience noticeably wetter and drier periods during the year. During autumn is the driest period of the year in Paramaribo, Paramaribo on average receives roughly 2200 mm of rainfall each year. Paramaribo has a population of 240,924 people, in the past decades a significant number of Brazilians, Guyanese and new Chinese immigrants have settled in Paramaribo. Paramaribo is the business and financial centre of Suriname, all banks, insurance corporations and other financial and commercial companies are headquartered in Paramaribo. Around 75 percent of Surinames GDP is consumed in Paramaribo, tourism is an increasingly important sector, with most visitors coming from the Netherlands. Administratively, Paramaribo forms its own district in Suriname, the resorts of Paramaribo district therefore correspond to boroughs of the city. There are twelve resorts in the Paramaribo district, Paramaribo is served by the Johan Adolf Pengel International Airport, the Jules Wijdenbosch Bridge, which is part of the East-West Link, connects Paramaribo with Meerzorg on the other side of the Suriname River
Paramaribo
–
The street Waterkant in Paramaribo
Paramaribo
–
1830s
lithograph of the market
Paramaribo
–
View of Paramaribo from space
Paramaribo
–
UNESCO World Heritage Site
47.
Pontianak, Indonesia
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Kota Pontianak is the capital of the Indonesian province of West Kalimantan, founded by Syarif Abdurrahman Alkadrie as a capital of Sultanate of Kadriyah in 23 Oktober 1771 /24 Rajab 1181 Hijriah. Syarif Abdurrahman Alkadrie developed Pontianak as a port on the island of Borneo. It is located precisely on the equator, hence it is known as Kota Khatulistiwa. The city center is actually less than 3 kilometres south of the equator, at the year of 2013, Vania Larissa is winner to support area Pontianak, West Kalimantan at Miss Indonesia 2013. The city was formerly the capital of the independent Sultanate of Pontianak and was founded on 23 October 1771 around an old trading station on the Borneo coast. It is built on ground that is subjected to regular flooding by the river. Then, He build a Mosque and a palace, exactly on the location of the ghosts nest, the Mosque and The palace is become the first building in Pontianak City The history of the city of Pontianak written by a Dutch historian, V. J. Verth in his book Borneos Afdeling Wester, whose content is different from the version of the stories circulating in the community today. According to him, the Dutch started to go to Pontianak in 1773 from Batavia, verth wrote that Syarif Abdurrahman, son of Sharif Hussein bin Ahmed cleric Alqadrie, leaving the kingdom Mempawah and began to wander. In the region of Banjarmasin, he married the sister of the Sultan of Banjar Sunan Nata Nature and he was successful in commerce and accumulate enough capital to arm ships and boats Pencalang lancangnya, then he started to take the fight against Dutch colonialism. With the help of Sultan Sand, Syarif Abdurrahman then successfully hijack Dutch ship near Bangka, also British, Abdurrahman became a rich man and then tried to establish a settlement on an island in the Kapuas River. He found branching Porcupine River and then to develop the area into a trading center. This is the region that is now called Pontianak, in 1778, Dutch colonialists from Batavia entered Pontianak, led by Willem Ardinpola. Netherlands when it occupies an area opposite the palace now known as the Land of a Thousand or Verkendepaal area. This area then became Controleur Onderafdeeling van het Hoofd Hoofd Pontianak or Plaatselijk Bestuur van Pontianak, assistant Resident het Hoofd van der Afdeeling Pontianak set Plaatselijk Fonds. The agency manages eigendom or government wealth and take care of tax funds, Plaatselijk Fonds later renamed Shintjo during the Japanese population in New York City. Pontianak City lies on the Equator track with a height ranging from 0.1 to 1.5 meters above sea level, cities are separated by the Kapuas Besar River, Kapuas Kecil River and Landak River. Thus Pontianak city is divided into three parts, in 1963 by Presidential Decree No.243 In 1963, the City entered into the zone Central Indonesian Time But, on January 1,1988 by Presidential Decree No.41 Year 1987
Pontianak, Indonesia
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Pontianak
Pontianak, Indonesia
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Pontianak street view
Pontianak, Indonesia
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Kapuas Bridge
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