1.
Nepal
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Nepal, officially the Federal Democratic Republic of Nepal, is a landlocked central Himalayan country in South Asia. Nepal is divided into 7 provinces and 75 districts and 744 local units including 4 metropolises,13 sub-metropolises,246 municipal councils and 481 village and it has a population of 26.4 million and is the 93rd largest country by area. Bordering China in the north and India in the south, east, Nepal does not border Bangladesh, which is located within only 27 km of its southeastern tip. It neither borders Bhutan due to the Indian state of Sikkim being located in between, Nepal has a diverse geography, including fertile plains, subalpine forested hills, and eight of the worlds ten tallest mountains, including Mount Everest, the highest point on Earth. Kathmandu is the capital and largest city. It is a nation with Nepali as the official language. The territory of Nepal has a history since the Neolithic age. The name Nepal is first recorded in texts from the Vedic Age, the era which founded Hinduism, in the middle of the first millennium BCE, Gautama Buddha, the founder of Buddhism, was born in southern Nepal. Parts of northern Nepal were intertwined with the culture of Tibet, the Kathmandu Valley in central Nepal became known as Nepal proper because of its complex urban civilization. It was the seat of the prosperous Newar confederacy known as Nepal Mandala, the Himalayan branch of the ancient Silk Road was dominated by the valleys traders. The cosmopolitan region developed distinct traditional art and architecture, by the 18th century, the Gorkha Kingdom achieved the unification of Nepal. The Shah dynasty established the Kingdom of Nepal and later formed an alliance with the British Empire, the country was never colonized but served as a buffer state between Imperial China and Colonial India. In the 20th century, Nepal ended its isolation and forged ties with regional powers. Parliamentary democracy was introduced in 1951, but was suspended by Nepalese monarchs in 1960 and 2005. The Nepalese Civil War resulted in the proclamation of a republic in 2008, modern Nepal is a federal secular parliamentary republic. Nepal is a nation, ranking 144th on the Human Development Index in 2016. The country struggles with the transition from a monarchy to a republic and it also suffers from high levels of hunger and poverty. Despite these challenges, Nepal is making progress, with the government declaring its commitment to elevate the nation from least developed country status by 2022
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Geography of Nepal
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Nepal measures about 800 kilometers along its Himalayan axis by 150 to 250 kilometers across. Nepal has an area of 147,181 square kilometers, Nepal is landlocked by India on three sides and Chinas Tibet Autonomous Region to the north. West Bengals narrow Siliguri Corridor or Chickens Neck separate Nepal and Bangladesh, to the east are India and Bhutan. Nepal depends on India for goods facilities and access to the sea. For a small country, Nepal has tremendous geographic diversity, along a south-to-north transect, Nepal can be divided into three belts, Terai, Hill and Mountain Regions. In the other direction, it is divided into three major systems, from east to west, Koshi, Gandaki/Narayani and Karnali, all tributaries of the Ganges. The Ganges-Yarlung Zangbo/Brahmaputra watershed largely coincides with the Nepal-Tibet border, however several Ganges tributaries rise inside Tibet, the Terai or Madhesh region begins at the Indian border and includes the southernmost part of the flat, intensively farmed Gangetic Plain called the Outer Terai. By the 19th century, timber and other resources were being exported to India, the Outer Terai is culturally more similar to adjacent parts of Indias Bihar and Uttar Pradesh than to the hill region of Nepal. Nepali is taught in schools and often spoken in government offices, however the population mostly uses Maithali, Bhojpuri. The Outer Terai ends at the base of the first range of foothills called the Siwaliks or Churia and this range has a densely forested skirt of coarse alluvium called the bhabhar. Below the bhabhar, finer, less permeable sediments force groundwater to the surface in a zone of springs, in Persian, terai refers to wet or marshy ground. Before the use of DDT this was dangerously malarial, Nepals rulers used this for a defensive frontier called the char kose jhadi. Above the bhabhar belt, the Siwaliks rise to about 700 metres with peaks as high as 1,000 metres and this range is composed of poorly consolidated, coarse sediments that do not retain water or support soil development so there is virtually no agricultural potential and sparse population. In several places beyond the Siwaliks there are dūn valleys called Inner Terai and these valleys have productive soil but were dangerously malarial except to indigenous Tharu people who had genetic resistance. In the mid-1950s DDT came into use to suppress mosquitos and the way was open to settlement from the land-poor hills, the terai ends and the Hills begin at a higher range of foothills called the Mahabharat Range. Situated south of the Mountain Region, the Hill Region is mostly betw altitude. This region begins at the Mahabharat Range where a system called the Main Boundary Thrust creates an escarpment 1,000 to 1,500 metres high. These steep southern slopes are nearly uninhabited, thus an effective buffer between languages and culture in the Terai and Hill regions, Hindu Paharis mainly populate river and stream bottoms that enable rice cultivation and are warm enough for winter/spring crops of wheat and potato
3.
Montane ecosystems
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Montane ecosystems refers to any ecosystem found in mountains. These ecosystems are affected by climate, which gets colder as elevation increases. They are stratified according to elevation, dense forests are common at moderate elevations. However, as the elevation increases, the climate becomes harsher, as elevation increases, the climate becomes cooler, due to a decrease in the greenhouse effect. The characteristic flora and fauna in the mountains tend to depend on elevation. This dependency causes life zones to form, bands of similar ecosystems at similar altitude, one of the typical life zones on mountains is the montane forest, at moderate elevations, the rainfall and temperate climate encourages dense forests to grow. Holdridge defines the climate of montane forest as having a biotemperature of between 6 and 12 °C, where biotemperature is the mean temperature considering temperatures below 0 °C to be 0 °C. Above the elevation of the montane forest, the trees thin out in the zone, become twisted krummholz. Therefore, Montane forests often contain trees with twisted trunks and this phenomenon is observed due to the increase in the wind strength with the elevation. The elevation where trees fail to grow is called the tree line. The biotemperature of the zone is between 3 and 6 °C. Above the tree line the ecosystem is called the zone or alpine tundra, dominated by grasses. The biotemperature of the zone is between 1.5 and 3 °C. Many different plant species live in the environment, including perennial grasses, sedges, forbs, cushion plants, mosses. Alpine plants must adapt to the conditions of the alpine environment, which include low temperatures, dryness, ultraviolet radiation. Alpine plants display adaptations such as structures, waxy surfaces. Because of the characteristics of these zones, the World Wildlife Fund groups a set of related ecoregions into the montane grassland and shrubland biome. Climates with biotemperatures below 1.5 °C tend to consist purely of rock, Montane forests occur between the submontane zone and the subalpine zone. The elevation at which one habitat changes to another varies across the globe, the upper limit of montane forests, the forest line or timberline, is often marked by a change to hardier species that occur in less dense stands
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Subtropics
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The subtropics are geographic and climate zones located roughly between the tropic circle of latitude at 23.5 latitude and temperate latitudes. Subtropical climates are characterized by warm to hot summers and cool to mild winters with infrequent frost. Subtropical climates can occur at elevations within the tropics, such as in the southern end of the Mexican Plateau and in Vietnam. Six climate classifications use the term to define the various temperature. A great portion of the deserts are located within the subtropics. Within savanna regimes in the subtropics, a wet season is seen annually during the summer, within Mediterranean climate regimes, the wet season occurs during the winter. Areas bordering warm oceans are prone to heavy rainfall from tropical cyclones. Plants such as palms, citrus, mango, lychee, the tropics have been historically defined as lying between the Tropic of Cancer and Tropic of Capricorn, located at 23. 45° north and south latitude respectively. The poleward fringe of the subtropics is located at approximately 40° north and south latitude respectively, northern fringes of the type can go further north due to moderating effects of ocean streams, like in parts of Southern Europe due to heat transported by the Gulf Stream. Several methods have used to define the subtropical climate. In the Trewartha climate classification, a subtropical region should have at least eight months with a temperature greater than 10 °C. According to the Troll-Paffen climate classification, there exists one large subtropical zone named the warm-temperate subtropical zone. According to the E. Neef climate classification, the zone is divided into two parts, Rainy winters of the west sides and Eastern subtropical climate. According to the Wilhelm Lauer & Peter Frankenberg climate classification, the zone is divided into three parts, high-continental, continental, and maritime. According to the Siegmund/Frankenberg climate classification, subtropical is one of six zones in the world. Heating of the earth near the equator leads to large amounts of upward motion and convection along the trough or Intertropical convergence zone. The upper-level divergence over the near-equatorial trough leads to air rising and moving away from the equator aloft, as the air moves towards the Mid-Latitudes, it cools and sinks, which leads to subsidence near the 30th parallel of both hemispheres. This circulation is known as the Hadley cell and leads to the formation of the subtropical ridge, many of the worlds deserts are caused by these climatological high-pressure areas, located within the subtropics
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Snow line
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The climatic snow line is the point above which snow and ice cover the ground throughout the year. The actual snow line may seasonally be significantly lower, the interplay of altitude and latitude affects the precise placement of the snow line at a particular location. At or near the equator, it is situated at approximately 4,500 meters above sea level. In addition, the location to the nearest coastline can influence the altitude of the snow line. A higher altitude is necessary to lower the temperature further against the surroundings. Furthermore, large-scale oceanic currents such as the North Atlantic Current can have significant affects over large areas, the highest mountain in the world below the snow line is Ojos del Salado. Compare the usage of snow line indicating the boundary between snow and non-snow, Frost line Frost line Glacier High Alps Ice cap climate Tree line Charlesworth J. K. With special reference to its glaciation, vol. I, london, Edward Arnold Ltd,700 pp. Flint, R. F. New York, xiii+553+555 pp. Kalesnik, S. V, uchpedgiz, Leningrad,328 pp. Tronov, M. V. Voprosy svyazi mezhdu klimatom i oledeneniem, izdatelstvo Tomskogo Universiteta, Tomsk,202 pp. Wilhelm, F. Schnee- und Gletscherkunde, De Gruyter, Berlin,414 pp
6.
Dharchula
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Dharchula is a town and a nagar panchayat in Pithoragarh district in the northern state of Uttarakhand, India. Dharchula is an ancient trading town for the trade routes. It is surrounded by mountains and is situated in a valley. Dharchula lies about 83 km northerly of Pithoragarh along the route of the Kailash-Mansarovar pilgrimage tour, the name of the town may originate from the Hindi words for mountain peak and stove because the valley in which it lies resembles a stove. Dharchula is cold during winters, but it usually does not get snow, Nepal has a town with a similar name, Darchula, across the river Mahakali - which acts as the natural border between India and Nepal over a long stretch. People of both towns have similar traditions, culture, and lifestyle and move across the border without hindrance, the area has a mixture of Kumaouni and Tibetean language, traditions and culture. As per the 2011 census, Dharchula Nagar Palika has population of 18,039 of which 9,797 are males while 8,242 are females, population of Children with age of 0-6 is 2190 which is 12. 64% of total population of Dharchula. Female Sex Ratio is of 854 against state average of 963, child Sex Ratio in Dharchula is around 824 compared to Uttarakhand state average of 890. Literacy rate of Dharchula city is 88. 68% higher than average of 78. 82%. In Dharchula, Male literacy is around 95. 10% while female literacy rate is 81. 20%, Dharchula Nagar Palika has total administration over 1,712 houses to which it supplies basic amenities like water and sewerage. It is also authorized to build roads within Nagar Palika limits, primary religion followed is Hinduism, followed by Islam, Christianity and Sikhism. As per the 2001 census Dharchula had a population of 6424, males constituted 54% of the population and females, 46%. Dharchula had a literacy rate of 75%, higher than the national average of 59. 5%. Male literacy was 80% and female literacy was 69%, in Dharchula, 12% of the population was under 6 years of age. Rung Kalyan Sanstha is an institution which binds together the entire Rung community, Dharchula has the Rung Community School. The town is situated in a valley at 915 m elevation and is 83 km from its district headquarters. The way from Pithoragarh to Dharchula is alongside the Kali River and is a 3 to 3.5 hour journey, the chief modes of transportation available are private jeeps and state government buses. However, reaching Pithoragarh itself from the plains is a tiring journey, one can reach Pithoragarh from either Haldwani or from Tanakpur
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Doti
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Doti division covers the nine districts of Seti and Mahakali Zone, four in Mahakali and five in Seti Zone respectively. The name Doti is believed to have originated form the word Dovati, other view is that the original name of Doti was devatavi= dev+aatavi or aalaya. Doti was an ancient kingdom in far western region of Nepal which was formed after the disintegration of the Katyuri Kingdom of Kumaon around 13th century, Doti was one of eight different princely states Katiyuri Kingdom was divided into Eight for their eight Prince and became different independent Kingdom. Brahma Dev Mandi at Kanchanpur District of Mahakali Zone was established by Katyuri king Brahma Dev, Niranjan Malla Dev was the founder of Doti Kingdom around 13th century after the fall of the Katyuri Kingdom. He was the son of Last Katyuris of united Katyuris kingdom, kings of Doti were called Raikas. Later on Raikas, after defeating the Khas Malla of Karnali Zone, were able to establish a strong Raikas Kingdom in Far Western Region and Kumaun which was Doti. So far, the evidences of following Raikas have been discovered, Niranjan Malla Dev Nagi Malla Ripu Malla Nirai Pal. In the war with the Gorkhalis, the Doti kingdom was defeated, during the period of Akbars rule in the 16th century, the Moguls had attacked the Raikas of Doti. They invaded Ajemeru, capital of the Raika Kingdom, Ajemeru is now in Dadeldhura District of far western region of Nepal. Hussain Khan, army chief of Akbar residing in Lucknow had led the attack, raja Deep Shahi was expelled from Nepal in 1790 A. D and on arriving to Terai of Oudh he established Khairgarh-Singhai State in Khairigarh under British India. Kanchanpur Praganna was also the parts of his State or Zamindari and he succeeded in defeating the Banjaras rural of Khairigarh and establishing himself not only in that Pargana but also in parts of Bhur. His state was merged with India In 1947 after Indian Independence, raja Akshya Vikram Shah,37, is the present ruler of Khairigarh. The Far-Western Development Region has the Mid-Western Development Region to the east, Uttar Pradesh to the south, Uttarakhand to the west, the highest mountain in the region is the Api Peak, with 7,132 m high, it is in the Darchula district. Other high mountain is Saipal,7,031 m high, the most important rivers in the Far-Western Development Region are the Seti and the Mahakali rivers, both rivers are tributaries of the Ghaghara or Karnali river.6 persons/km2. Dotiyali or Dotyali and Kumauni is the language spoken in Doti region or far western region of Nepal. Dotiyali which is similar to Kumauni language is one of language of Indo-European family, according to Rahul Sankrityayan, Dotiyali is the dialect of Kumauni language which was brought in Doti by section of Katyuri dynasty of kumaoun which had ruled over Doti till 1790. Local intellectuals and people speaking Dotiyali language were increasingly demanding that their language be recognized as one of the national languages of Nepal. Inhabitants of two terai districts Kailali District and Kanchanpur District speak different languages, rana-tharu and Dangaura-tharu speaks their own language
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House of Representatives (Nepal)
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The House of Representatives was the lower house of parliament during the 1990 Constitution in Nepal. It consisted of 205 members directly elected by the people and it had five-year terms, but it could be dissolved by the king on the advice of the prime minister before the ending of its term. The Pratinidhi Sabha was provisioned by the Constitution of the Kingdom of Nepal 1990 in October 1990, according to which the parliament was formed by the General Election held in April 1991. There were only three elections were held for the House of Representative, General Election 1991 Dissolved by PM Girija Prasad Koirala announcing Mid-term Election. Mid Term Election 1994 General Election 1999 Dissolved by PM Sher Bahadur Deuba announcing Mid-term Election which could not held later,1999 Elected parliament body reinstated by King Gyanendras address in April 2006 and transformed into Interim Legislature Parliament in January 15,2007. The House of Representative as well as the National Assembly has been dissolved on 1 February,2005 by King Gyanendra, political parties in Nepal have been agitating against the royal coup with demand of reinstatement of the parliament. There was a peoples uprising known as Peoples Movement 2006. Finally the king who was using extreme authority was compelled to step down, by the King Gyanendra Address in April 2006 Both houses were reinstated. On January 15,2007, the Pratinidhi Sabha was transformed into interim legislature, the new interim legislature was largely composed of former Pratinidhi Sabha MPs and 79 members from the rebel Communist Party Maoist
9.
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
10.
Temperate climate
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In geography, temperate or tepid latitudes of Earth lie between the tropics and the polar regions. The temperatures in these regions are relatively moderate, rather than extremely hot or cold. The north temperate zone extends from the Tropic of Cancer to the Arctic Circle, the south temperate zone extends from the Tropic of Capricorn to the Antarctic Circle. In some climate classifications, the zone is often divided into several smaller climate zones. These include Humid subtropical climate, Mediterranean climate, oceanic, subtropical climates are located between 23. 5° and 35. 0° north or south latitude on the eastern or leeward sides of landmasses. This climate has long, generally hot, summers and short, mild winters and these climates may occur in southern Asia, the southeastern United States, parts of eastern Australia, and in eastern coastal South America. Mediterranean climates, occur between 30° and 42° north and south latitude, on the sides of landmasses. This climate has hot summers and short mild winters, however, seasonal rainfall is the opposite of that of the subtropical humid type. These climates occur near the rimlands of the Mediterranean Sea, in western Australia, in California, the oceanic climates occur in the higher middle latitudes, between 45° and 60° north and south latitude. They are created by the flow from the cool high latitude oceans to their west. This causes the climate to have cool summers and cool winters, annual rainfall is spread throughout the entire year. Regions with this climate include Western Europe, northwestern North America, the Continental climates occur in middle latitudes, between 35° or 40° to 55°. These climates are normally inland or on sides of landmasses. They feature warm to hot summers and cold winters, with a large temperature variation. Regions with this climate include northern temperate Asia, the northern United States, southern Canada, the vast majority of the worlds human population resides in temperate zones, especially in the northern hemisphere, due to its greater mass of land. The richest temperate flora in the world is found in southern Africa, geographical zone Habitat Köppen climate classification Middle latitudes Polar circle Subtropics
Listen (help·info), a part of Province No. 7, is one of the seventy-seven districts of Nepal. The district, with Khalanga, Mahakali (today part of Mahakali Municipality) as its district headquarters, covers an area of 2,322 km² and has a population (2011) of 133,274.[1] The number of male 63,609 and female 69,855. Decadal Change(%) 9.40, Annual Growth Rate(%) 0.90, Sex Ratio(males per 100 females) 91, Absent (abroad) Population Total 6,867, where number of male 5,880 and female 987. Total Number of House 22,948. Total Number of Household 25,802. Average Household Size 5.17. Population Density 57 km2. The town has an Indian counterpart to its northwest, named Dharchula. The split between the two towns is just virtual as the traditions, culture, and lifestyle of the people living across both the regions are quite similar.[citation needed]
Darchula
