1.
Languages of Nepal
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The 2011 National census lists 123 Nepalese languages spoken as a mother tongue in Nepal. Most belong to the Indo-Aryan and Sino-Tibetan language families, the official language of Nepal is Nepali, formerly called Khaskura then Gorkhali. According to the 2011 national census, the percentage of Nepali Bhasi people is about 44. 6%, maithili is the second largest Nepalese language and according to 2011 Census, the percentage of Maithil people is 11. 57%. Three quarters of the 123 languages native to Nepal belong to the Tibeto-Burman language family, this includes Nepal Bhasa, the Dravidian languages are represented by Kurux, and the Munda languages of the Austroasiatic family by Santali and Mundari. The indigenous languages of Nepal that predated the influx of Indic, Tibeto-Burman, and other families barely survive in the Kusunda language, which is nearly extinct today. Nepal also has at several indigenous village sign languages, Jhankot Sign Language, Jumla Sign Language, and Ghandruk Sign Language, in addition to the Nepali Sign Language designed for national use
2.
Nepali language
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Nepali, originally known as Khas Kura, Parbate Bhasa or Gorkhali, is an Indo-Aryan language. It is the language and de facto lingua franca of Nepal. It is also spoken in parts of India, particularly by Indian Gorkha. In India, Nepali language is listed in the Eighth Schedule to the Constitution of India having a status in the Indian state of Sikkim. Nepali developed in proximity to a number of Indo-Aryan languages, most notably the Pahari languages and Magahi, however, owing to Nepals geographical area, it has also been influenced by Tibeto-Burman languages. Nepali is mainly differentiated from Central Pahari, both in grammar and vocabulary, by Tibeto-Burman idioms owing to close contact with the language group. Nepali language shares 40% lexical similarity with the Bengali language, in the nineteenth century, the British resident at Kathmandu Brian Houghton Hodgson observed that it was, in eight-tenths of its vocabulary, substantially Hindi. Historically, the language was first called the Khas language, then Gorkhali or Gurkhali before the term Nepali was adopted, in 1920, during Rana regime in Nepal, the term Nepal which resembled the Nepal Mandala was taken from its people. Soon after that, Nepal Bhasa was renamed into Newari and Parbate/Khas language took over as Nepali language, other names include Parbatiya and Dzongkha Lhotshammikha. It is also known as the Khey language or Partya language among the Newar people and Pahari language among Madhesi, however, due to protests for identity, Newars have restored their languages name as Nepal Bhasa and voices have been raise to re-instate Parbate language in its original name. Nepali developed a significant literature within a period of a hundred years in the 19th century. This literary explosion was fueled by Adhyatma Ramayana, Sundarananda Bara, Birsikka, a collection of folk tales. The contribution of trio-laureates Lekhnath Paudyal, Laxmi Prasad Devkota, the contribution of expatriate writers outside Nepal, especially in Darjeeling and Varanasi in India, is also notable. In the past decade, there have been many contributions to Nepali literature from the Nepali diaspora in Asia, Europe, America, according to the 2011 national census,44.6 percent of the population of Nepal speaks Nepali as a first language. The Ethnologue website reports 12,300,000 speakers within Nepal, Nepali is traditionally spoken in the Hill Region of Nepal, especially in the western part of the country. Although the Newar language dominated the Kathmandu valley, Nepali is currently the most dominant, Nepali is used in government and as the everyday language of a growing portion of the local population. Nevertheless, the use of Nepali in the courts and government of Nepal is being challenged. Recognition of other languages in Nepal was one of the objectives of the Communist Party of Nepals long war
3.
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
4.
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
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.
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
7.
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
8.
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
Listen (help·info)) a part of Karnali province, is one of the seventy-seven districts of Nepal. The district, with Dailekh as its district headquarters, covers an area of 1,502 km² and had a population of 225,201 in 2001[2] and 261,770 in 2011.[1]
