1.
Brunei
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Brunei, officially the Nation of Brunei, the Abode of Peace, is a sovereign state located on the north coast of the island of Borneo in Southeast Asia. Apart from its coastline with the South China Sea, the country is surrounded by the state of Sarawak. It is separated into two parts by the Sarawak district of Limbang, Brunei is the only sovereign state completely on the island of Borneo, the remainder of the islands territory is divided between the nations of Malaysia and Indonesia. Bruneis population was 408,786 in July 2012, the maritime state was visited by Spains Magellan Expedition in 1521 and fought against Spain in the 1578 Castille War. During the 19th century, the Bruneian Empire began to decline, the Sultanate ceded Sarawak to James Brooke and installed him as the White Rajah, and it ceded Sabah to the British North Borneo Chartered Company. In 1888, Brunei became a British protectorate and was assigned a British resident as colonial manager in 1906, after the Japanese occupation during World War II, in 1959 a new constitution was written. In 1962, an armed rebellion against the monarchy was ended with the help of the British. Brunei gained its independence from the United Kingdom on 1 January 1984, Economic growth during the 1990s and 2000s, with the GDP increasing 56% from 1999 to 2008, transformed Brunei into an industrialised country. It has developed wealth from petroleum and natural gas fields. Brunei has the second-highest Human Development Index among the Southeast Asian nations, after Singapore, according to the International Monetary Fund, Brunei is ranked fifth in the world by gross domestic product per capita at purchasing power parity. The IMF estimated in 2011 that Brunei was one of two countries with a debt at 0% of the national GDP. Forbes also ranks Brunei as the fifth-richest nation out of 182, based on its petroleum, according to legend, Brunei was founded by Awang Alak Betatar, later to be Sultan Muhammad Shah. He moved from Garang, a place in the Temburong District to the Brunei River estuary, according to legend, upon landing he exclaimed, Baru nah, from which the name Brunei was derived. He was the first Muslim ruler of Brunei, before the rise of the Bruneian Empire under the Muslim Bolkiah Dynasty, Brunei is believed to have been under Buddhist rulers. It was renamed Barunai in the 14th century, possibly influenced by the Sanskrit word varuṇ, the word Borneo is of the same origin. In the countrys name, Negara Brunei Darussalam, darussalam means abode of peace. The people are pagans and are men of goodwill and their colour is whiter than that of the other sort. in this island justice is well administered. One of the earliest Chinese records is the 977 AD letter to Chinese emperor from the ruler of Po-ni, which some scholars believe to refer to Borneo
2.
South China Sea
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The South China Sea is a marginal sea that is part of the Pacific Ocean, encompassing an area from the Karimata and Malacca Straits to the Strait of Taiwan of around 3,500,000 square kilometres. The areas importance largely results from one-third of the worlds shipping sailing through its waters, the sea and its mostly uninhabited islands are subject to competing claims of sovereignty by several countries. These claims are reflected in the variety of names used for the islands. South China Sea is the dominant term used in English for the sea, and this name is a result of early European interest in the sea as a route from Europe and South Asia to the trading opportunities of China. In the sixteenth century Portuguese sailors called it the China Sea, the International Hydrographic Organization refers to the sea as South China Sea. The Classic of Poetry, Zuo Zhuan, and Guoyu classics of the Spring and Autumn period also referred to the sea, Nan Hai, the South Sea, was one of the Four Seas of Chinese literature. There are three other seas, one for each of the four cardinal directions, during the Eastern Han dynasty, Chinas rulers called the Sea Zhang Hai. Fei Hai became popular during the Southern and Northern Dynasties period, usage of the current Chinese name, Nan Hai, became gradually widespread during the Qing Dynasty. In Southeast Asia it was called the Champa Sea or Sea of Cham. The majority of the sea came under Japanese naval control during World War II following the acquisition of many surrounding South East Asian territories in 1941. Japan calls the sea Minami Shina Kai South China Sea and this was written 南支那海 until 2004, when the Japanese Foreign Ministry and other departments switched the spelling 南シナ海, which has become the standard usage in Japan. In China, it is called the South Sea, 南海 Nánhǎi, in Malaysia, Indonesia and the Philippines, it was long called the South China Sea, with the part within Philippine territorial waters often called the Luzon Sea, Dagat Luzon, by the Philippines. However, following an escalation of the Spratly Islands dispute in 2011, a PAGASA spokesperson said that the sea to the east of the Philippines will continue to be called the Philippine Sea. In September 2012, Philippine President Benigno Aquino III signed Administrative Order No, states and territories with borders on the sea include, the Peoples Republic of China, the Republic of China, the Philippines, Malaysia, Brunei, Indonesia, Singapore, and Vietnam. Major rivers that flow into the South China Sea include the Pearl, Min, Jiulong, Red, Mekong, Rajang, Pahang, Pampanga, the International Hydrographic Organization defines the limits of the South China Sea as follows, On the South. From Fuki Kaku the North point of Formosa to Kiushan Tao on to the South point of Haitan Tao, the Mainland, the Southern limit of the Gulf of Thailand and the East coast of the Malay Peninsula. The sea lies above a drowned continental shelf, during recent ice ages global sea level was hundreds of metres lower, the South China Sea opened around 45 million years ago when the Dangerous Ground rifted away from southern China. Extension culminated in seafloor spreading around 30 million years ago, a process that propagated to the SW resulting in the V-shaped basin we see today, extension ceased around 17 million years ago
3.
East Malaysia
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East Malaysia, also known as Sabah, Sarawak and Labuan or Malaysian Borneo, is the part of Malaysia located on the island of Borneo. It consists of the Malaysian states of Sabah, Sarawak, and it lies to the east of Peninsular Malaysia, which is located on the Malay Peninsula. The two are separated by the South China Sea, while East Malaysia is less populated and less developed than West Malaysia, its land mass is larger and it has notably more natural resources, chiefly oil and gas reserves. Some parts of present-day East Malaysia, especially the regions, were once part of the thalassocracy of the Sultanate of Brunei. However, most parts of the region consisted of independent tribal societies. In 1658, the northern and eastern coasts of Sabah were ceded to the Sultanate of Sulu while the west coast of Sabah, beginning in the mid 19th century, Sabah and Sarawak became British protectorates, and, in 1946, they became separate British colonies. Sabah and Sarawak were separate British colonies from Malaya, and did not become part of the Federation of Malaya in 1957, however, each voted to become part of the new Federation of Malaysia along with the Federation of Malaya and Singapore in 1963. Previously, there were efforts to unite Brunei, Sabah, and Sarawak under the North Borneo Federation, Sabah and Sarawak retained a higher degree of local government and legislative autonomy than other states in West Malaysia. For example, both states have their own immigration controls, requiring Malaysian citizens from West Malaysia to carry passports or identity cards when visiting East Malaysia, the islands of Labuan were once part of North Borneo in 1946 before becoming a Federal Territory in Malaysia on 1984. It was used to establish a centre for finance in 1990. The consensus seems to be that Sabah and Sarawak are merely states of the federation with a higher degree of autonomy compared to states in Peninsular Malaysia. There are also separate laws governing Sabah and Sarawak, as opposed to the National Land Code. With regard to the administration of justice, the courts in East Malaysia are part of the court system in Malaysia. The Constitution of Malaysia provides that there shall be two High Courts of co-ordinate jurisdiction – The High Court in Malaya and the High Court in Sabah, the current Chief Judge of Sabah and Sarawak is Richard Malanjum from Sabah. His office is the fourth highest in the Malaysian judicial system, in 1976, all the Sabah and Sarawak MPs supported the Malaysian parliament bill which downgraded both the states from equal partners to one of the 13 states in the federation. Political parties in Sarawak and Sabah evolved independently of each other, party switching and party leadership tussle are common in both the states. The landscape of East Malaysia is mostly rain forests with areas of mountain rain forest towards the interior regions. The total area of East Malaysia is 200,565 km2, representing approximately 61% of the land area of Malaysia
4.
Climate
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Climate is the statistics of weather, usually over a 30-year interval. Climate differs from weather, in that weather only describes the conditions of these variables in a given region. A regions climate is generated by the system, which has five components, atmosphere, hydrosphere, cryosphere, lithosphere. The climate of a location is affected by its latitude, terrain, climates can be classified according to the average and the typical ranges of different variables, most commonly temperature and precipitation. The most commonly used classification scheme was the Köppen climate classification, the Bergeron and Spatial Synoptic Classification systems focus on the origin of air masses that define the climate of a region. Paleoclimatology is the study of ancient climates, Climate models are mathematical models of past, present and future climates. Climate change may occur long and short timescales from a variety of factors. For example, a 3°C change in mean annual temperature corresponds to a shift in isotherms of approximately 300–400 km in latitude or 500 m in elevation, therefore, species are expected to move upwards in elevation or towards the poles in latitude in response to shifting climate zones. Climate is commonly defined as the weather averaged over a long period, the standard averaging period is 30 years, but other periods may be used depending on the purpose. Climate also includes statistics other than the average, such as the magnitudes of day-to-day or year-to-year variations, the classical period is 30 years, as defined by the World Meteorological Organization. These quantities are most often surface variables such as temperature, precipitation, Climate in a wider sense is the state, including a statistical description, of the climate system. The World Meteorological Organization describes climate normals as reference points used by climatologists to compare current climatological trends to that of the past or what is considered normal, a Normal is defined as the arithmetic average of a climate element over a 30-year period. A30 year period is used, as it is enough to filter out any interannual variation or anomalies. The WMO originated from the International Meteorological Organization which set up a commission for climatology in 1929. At its 1934 Wiesbaden meeting the commission designated the thirty-year period from 1901 to 1930 as the reference time frame for climatological standard normals. In 1982 the WMO agreed to update climate normals, and in these were completed on the basis of climate data from 1 January 1961 to 31 December 1990. The difference between climate and weather is usefully summarized by the popular phrase Climate is what you expect, weather is what you get. Over historical time spans there are a number of nearly constant variables that determine climate, including latitude, altitude, proportion of land to water and these change only over periods of millions of years due to processes such as plate tectonics
5.
Tropical climate
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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
6.
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
