Martadi is a town and seat of Bajura District in the Seti Zone of north-western Nepal. At the time of the 1991 Nepal census it had a population of 4,618 and had 942 houses in the town but now it has increased by growth rate of 2.62. The town and surrounding area is under the jurisdiction of the Martadi District Police. At the time of the 2011 Nepal census it had a population of 8,807 people living in 1,290 individual Households. Bajura Multiple CampusIt has been conditioning the bachelor level programs with affiliation to Tribhuwan University, Kathmandu, Nepal. Badimalika English Boarding School Converse Academy Shree Malika Higher Secondary School
The climatic snow line is the boundary between a snow-covered and snow-free surface. The actual snow line may adjust seasonally, be either higher in elevation, or lower; the permanent snow line is the level above which snow will lie all year. Snow line is an umbrella term for different interpretations of the boundary between snow-covered surface and snow-free surface; the definitions of the snow line may have different spatial focus. In many regions the changing snow line reflect seasonal dynamics; the final height of the snow line in a mountain environment at the end of the melting season is subject to climatic variability, therefore may be different from year to year. The snow line is measured using aerial photographs, or satellite images; because the snow line can be established without on-the-ground measurements, it can be measured in remote and difficult to access areas. Therefore, the snow line has become an important variable in hydrological models; the average elevation of a transient snow line is called the "climatic snow line" and is used as a parameter to classify regions according to climatic conditions.
The boundary between the accumulation zone and the ablation zone on glaciers is called the "annual snow line". The glacier region below this snow line was subject to melting in the previous season; the term "orographic snow line" is used to describe the snow boundary on surfaces other than glaciers. The term "regional snow line" is used to describe large areas; the "permanent snow line" is the level. 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 4,500 meters above sea level; as one moves towards the Tropic of Cancer and Tropic of Capricorn, the parameter at first increases: in the Himalayas the permanent snow line can be as high as 5,700 metres, whilst on the Tropic of Capricorn no permanent snow exists at all in the Andes because of the extreme aridity. Beyond the Tropics the snow line becomes progressively lower as the latitude increases, to just below 3,000 metres in the Alps and falling all the way to sea level itself at the ice caps near the poles.
In addition, the relative location to the nearest coastline can influence the altitude of the snow line. Areas near a coast might have a lower snow line than areas of the same altitude and latitude situated in a landmass interior due to more winter snowfall and because the average summer temperature of the surrounding lowlands would be warmer away from the sea.. A higher altitude is therefore necessary to lower the temperature further against the surroundings and keep the snow from melting. Furthermore, large-scale oceanic currents such as the North Atlantic Current can have significant affects over large areas. In the northern hemisphere the snow line on the north facing slopes is at a lower altitude, as the north facing slopes receive less sun light than south facing slopes; the glacier equilibrium line is the point of transition between the accumulation zone and ablation zone. It is the line. Depending on the thickness of the glacier, this line can seem as though it is leaning more towards one zone but it is determined by the actual mass of ice in either zone.
The rates of ablation and accumulation can be used to determine the location of this line. This point is an important location to use in determining whether a glacier is shrinking. A higher glacier equilibrium line will indicate that the glacier is shrinking, whereas a lower line will indicate that the glacier is growing; the terminus of a glacier advances or retreats based on the location of this equilibrium line. Scientists are using remote sensing to better estimate the locations of this line on glaciers around the world. Using satellite imagery, scientists are able to identify whether the glacier is receding; this is a helpful tool for analyzing glaciers that are difficult to access. Using this technology we can better gauge the effects of climate change on glaciers around the world; 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.. The quaternary era. With special reference to its glaciation, vol. I. London, Edward Arnold Ltd, 700 pp. Flint, R. F.. Glacial and Pleistocene geology. John Wiley & Sons, Inc. New York, xiii+553+555 pp. Kalesnik, S. V.. Obshchaya glyatsiologiya. Uchpedgiz, Leningrad, 328 pp. Tronov, M. V.. Voprosy svyazi mezhdu klimatom i oledeneniem. Izdatel'stvo Tomskogo Universiteta, Tomsk, 202 pp. Wilhelm, F.. Schnee- und Gletscherkunde, De Gruyter, Berlin, 414 pp. Braithewaite, R. J. and Raper, S. C. B. "Estimating Equilibrium Line Altitude From Glacier Inventory Data." Annals of Glaciology, 50, pp. 127–132. Doi:10.3189/172756410790595930. Leonard, K. C. and Fountain, A. G.. "Map-Based Methods for Estimating Glacier Equilibrium-Line Altitudes." Journal of Glaciology, vol. 49, no. 166, pp. 329–336. Doi:10.3189/172756503781830665. Ohmura, A. Kasser, P. and Funk, M.. "Climate at the Equilibrium Line
Sudurpashchim Pradesh is one of the seven provinces established by the new constitution of Nepal, adopted on 20 September 2015. It borders the Tibet Autonomous Region of China to the north, Karnali Pradesh and Province No. 5 to the east, the Indian states of Uttarakhand to the west and Uttar Pradesh to the south. Known as Province No. 7, the newly elected Provincial Assembly adopted Sudurpashchim Pradesh as the permanent name for the province in September 2018. As per a 28 September 2018 Assembly voting, the city of Godawari has been declared the capital of the Province; the province is coterminous with Nepal. Doti was an ancient kingdom in far western region of Kumaon, formed after the disintegration of the Katyuri Kingdom of Kumaon around the 13th century. Doti was one of eight different princely states Katyuri Kingdom was divided into eight for their eight prince's and became different independent kingdoms. On, the whole land between Ramganga on the west and the Karnali on the east, came under the Raikas after the origin of Raikas of Katyuris in Doti.
"Brahma Dev Mandi" at Kanchanpur District of Mahakali Zone was established by Katyuri king Brahma Dev. Before announcement of new provinces in Nepal, the area of this province was known as Far-Western development region of Nepal. There was no changes made in this province. Niranjan Malla Dev was the founder of Doti Kingdom around the 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. On Raikas, after defeating the Khas Malla of Karnali Zone, were able to establish a strong Raikas Kingdom in Far Western Region and Kumaun, Doti. During the period of Akbar's rule in the 16th century, the Mughals had attacked the Raikas of Doti, they invaded 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. According to `Abd al-Qadir Bada'uni, Indo-Persian historian during Mughal Empire, Mughal Army chief of Lukhnow, Hussian Khan, lured by the wealth and treasures of the kingdom of the Raikas, wanted to plunder the state, this being the motive behind the assault.
The historic place of war between the Doti Kingdom and Nepal during the period of Gorkha Expansion in 1790, according to the history of Nepal, is Nari-Dang, on the bank of the Seti River. The Dumrakot was the base of Doti Kingdom for fighting against the Gorkhalis. 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 the parts of his State or Zamindari, he succeeded in defeating the Banjaras rural of Khairigarh and establishing himself not only in that Pargana but in parts of Bhur. His state was merged with India In 1947 after Indian Independence; the Governor acts as the head of the province while the Chief Minister is the head of the provincial government. The Chief Judge of the Dipayal High Court is the head of the judiciary; the present Governor, Chief Minister and Chief Judge are Mohan Raj Malla, Trilochan Bhatta and Yagya Prasad Basyal. The province has 53 provincial assembly constituencies and 16 House of Representative constituencies.
Sudurpashchim Pradesh has a unicameral legislature, like all of the other provinces in Nepal. The term length of provincial assembly is five years; the Provincial Assembly of Sudurpashchim is temporarily housed at the District Coordination Committee Hall in Dhangadhi. The province is divided into nine districts. A district is administrated by the head of the District Coordination Committee and the District Administration Officer; the districts are further dived to rural municipalities. The municipalities include one sub-metropolitan city and 33 municipalities. There are 54 rural municipalities in the province. Achham District Baitadi District Bajhang District Bajura District Dadeldhura District Darchula District Doti District Kailali District Kanchanpur District The province has a population of 2,552,517, 9.63% of the total population of Nepal. The population density is about 130 persons per square kilometre; the province has a population growth rate of 1.53%. The sex ratio is 912 males for 1000 females, with a total of 1,217,887 males and 1,334,630 females recorded in 2011.
The urban population of the region is 1,504,279 and the rural population is 1,048,238. List of provinces of Nepal List of districts of Nepal
The subtropics are geographic and climate zones located between the tropics at latitude 23.5° and temperate zones north and south of the Equator. Subtropical climates are characterized by warm to hot summers and cool to mild winters with infrequent frost. Most subtropical climates fall into two basic types: humid subtropical, where rainfall is concentrated in the warmest months, dry summer climate or, where seasonal rainfall is concentrated in the cooler months. Subtropical climates can occur at high elevations within the tropics, such as in the southern end of the Mexican Plateau and in Vietnam and Taiwan. Six climate classifications use the term to help define the various temperature and precipitation regimes for the planet Earth. A great portion of the world's deserts are located within the subtropics, due to the development of the subtropical ridge. Within savanna regimes in the subtropics, a wet season is seen annually during the summer, when most of the yearly rainfall falls. Within Mediterranean climate regimes, the wet season occurs during the winter.
Areas bordering warm oceans are prone to locally heavy rainfall from tropical cyclones, which can contribute a significant percentage of the annual rainfall. Plants such as palms, mango, pistachio and avocado are grown within the subtropics; the tropics have been defined as lying between the Tropic of Cancer and Tropic of Capricorn, located at latitudes 23.45° north and south, respectively. According to the American Meteorological Society, the poleward fringe of the subtropics is located at latitudes 35° north and south, respectively. Several methods have been used to define the subtropical climate. In the Trewartha climate classification, a subtropical region should have at least eight months with a mean temperature greater than 10 °C and at least one month with a mean temperature under 18 °C. German climatologists Carl Troll and Karlheinz Paffen defined Warm temperate zones as plain and hilly lands having an average temperature of the coldest month between 2 °C and 13 °C in the Northern Hemisphere and between 6 °C and 13 °C in the Southern Hemisphere, excluding oceanic and continental climates.
According to the Troll-Paffen climate classification, there exists one large subtropical zone named the warm-temperate subtropical zone, subdivided into seven smaller areas. According to the E. Neef climate classification, the subtropical 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 subtropical zone is divided into three parts: high-continental and maritime. According to the Siegmund/Frankenberg climate classification, subtropical is one of six climate zones in the world. Heating of the earth near the equator leads to large amounts of upward motion and convection along the monsoon 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 leads to the formation of the subtropical ridge. Many of the world's deserts are caused by these climatological high-pressure areas, located within the subtropics; this regime is known as an arid subtropical climate, located in areas adjacent to powerful cold ocean currents. Examples of this climate are the coastal areas of southern Africa, the south of the Canary Islands and the coasts of Peru and Chile; the humid subtropical climate is located on the western side of the subtropical high. Here, unstable tropical airmasses in summer bring convective overturning and frequent tropical downpours, summer is the season of peak annual rainfall. In the winter the monsoon retreats, the drier trade winds bring more stable airmass and dry weather, frequent sunny skies. Areas that have this type of subtropical climate include Australia, Southeast Asia, parts of South America, the deep south of the United States. In areas bounded by warm ocean like the southeastern United States and East Asia, tropical cyclones can contribute to local rainfall within the subtropics.
Japan receives over half of its rainfall from typhoons. The Mediterranean climate is a subtropical climate with a wet season in winter and a dry season in the summer. Regions with this type of climate include the rim lands of the Mediterranean Sea, southwestern Australia around the Perth area, parts of the west coast of South American around Santiago, the coastal areas of western Mexico, coastal California in the United States; these climates do not see hard frosts or snow, which allows plants such as palms and citrus to flourish. As one moves toward the tropical side the slight winter cool season disappears, while at the poleward threshold of the subtropics the winters become cooler; some crops which have been traditionally farmed in tropical climates, such as mango and avocado, are cultivated in the subtropics. Pest control of the crops is less difficult than within the tropics, due to the cooler winters. Tree ferns are grown within subtropical areas within the subtropics and within topography within the tropics.
Dracaena and yucca can grow within the subtropics. Tre
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, the plant community transitions to grasslands or tundra; as elevation increases, the climate becomes cooler, due to a decrease in atmospheric pressure and the adiabatic cooling of airmasses. The change in climate by moving up 100 meters on a mountain is equivalent to moving 80 kilometers towards the nearest pole; the characteristic flora and fauna in the mountains tend to depend on elevation, because of the change in climate. 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 subalpine zone, become twisted krummholz, fail to grow. Therefore, montane forests contain trees with twisted trunks; 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 subalpine zone is between 3 and 6 °C. Above the tree line the ecosystem is called the alpine zone or alpine tundra, dominated by grasses and low-growing shrubs; the biotemperature of the alpine zone is between 1.5 and 3 °C. Many different plant species live in the alpine environment, including perennial grasses, forbs, cushion plants and lichens. Alpine plants must adapt to the harsh conditions of the alpine environment, which include low temperatures, ultraviolet radiation, a short growing season. Alpine plants display adaptations such as rosette structures, waxy surfaces, hairy leaves; because of the common 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 ice. Montane forests occur between the subalpine zone; the elevation at which one habitat changes to another varies across the globe by latitude. The upper limit of montane forests, the forest line or timberline, is marked by a change to hardier species that occur in less dense stands. For example, in the Sierra Nevada of California, the montane forest has dense stands of lodgepole pine and red fir, while the Sierra Nevada subalpine zone contains sparse stands of whitebark pine; the lower bound of the montane zone may be a "lower timberline" that separates the montane forest from drier steppe or desert region. Montane forests differ from lowland forests in the same area; the climate of montane forests is colder than lowland climate at the same latitude, so the montane forests have species typical of higher-latitude lowland forests. Humans can disturb montane forests through agriculture. On isolated mountains, montane forests surrounded by treeless dry regions are typical "sky island" ecosystems.
Montane forests in temperate climate are one of temperate coniferous forest or temperate broadleaf and mixed forest, forest types that are well known from northern Europe, northern United States, southern Canada. The trees are, however not identical to those found further north: geology and climate causes different related species to occur in montane forests. Montane forests around the world tend to be more species-rich than those in Europe, because major mountain chains in Europe are oriented east-west. Montane forests in temperate climate occur in Europe, in North America, south-western South America, New Zealand and Himalaya. Montane forests in Mediterranean climate are warm and dry except in winter, when they are wet and mild; these forests are mixed conifer and broadleaf forests, with only a few conifer species. Pine and Juniper are typical trees found in Mediterranean montane forests; the broadleaf trees show more variety and are evergreen, e.g. evergreen Oak. This type of forest is found in the Mediterranean Basin, North Africa and the southwestern US, Iran and Afghanistan.
In the tropics, montane forests can consist of broadleaf forest in addition to coniferous forest. One example of a tropical montane forest is a cloud forest, which gains its moisture from clouds and fog. Cloud forests exhibit an abundance of mosses covering the ground and vegetation, in which case they are referred to as mossy forests. Mossy forests develop on the saddles of mountains, where moisture introduced by settling clouds is more retained. Depending on latitude, the lower limit of montane rainforests on large mountains is between 1,500 and 2,500 metres while the upper limit is from 2,400 to 3,300 metres; the subalpine zone is the biotic zone below the tree line around the world. In tropical regions of Southeast Asia the tree line may be above 4,000 m, whereas in Scotland it may be as low as 450 m. Species that occur in this zone depend on the location of the zone on the Earth, for example, snow gum in Australia, or subalpine larch, mountain h
Nepal the Federal Democratic Republic of Nepal, is a landlocked country in South Asia. It is located in the Himalayas but includes parts of the Indo-Gangetic Plain. With an estimated population of 26.4 million, it is 48th largest country by population and 93rd largest country by area. It borders China in the north and India in the south and west while Bangladesh is located within only 27 km of its southeastern tip and Bhutan is separated from it by the Indian state of Sikkim. Nepal has a diverse geography, including fertile plains, subalpine forested hills, eight of the world's ten tallest mountains, including Mount Everest, the highest point on Earth. Kathmandu is largest city. Nepal is a multiethnic nation with Nepali as the official language; the name "Nepal" is first recorded in texts from the Vedic period of the Indian subcontinent, the era in ancient India when Hinduism was founded, the predominant religion of the country. In the middle of the first millennium BCE, Gautama Buddha, the founder of Buddhism, was born in Lumbini in southern Nepal.
Parts of northern Nepal were intertwined with the culture of Tibet. The centrally located Kathmandu Valley is intertwined with the culture of Indo-Aryans, was the seat of the prosperous Newar confederacy known as Nepal Mandala; the Himalayan branch of the ancient Silk Road was dominated by the valley's traders. The cosmopolitan region developed distinct traditional architecture. By the 18th century, the Gorkha Kingdom achieved the unification of Nepal; the Shah dynasty established the Kingdom of Nepal and formed an alliance with the British Empire, under its Rajput Rana dynasty of premiers. The country was never colonized but served as a buffer state between Imperial China and British India. Parliamentary democracy was introduced in 1951, but was twice suspended by Nepalese monarchs, in 1960 and 2005; the Nepalese Civil War in the 1990s and early 2000s resulted in the proclamation of a secular republic in 2008, ending the world's last Hindu monarchy. The Constitution of Nepal, adopted in 2015, establishes Nepal as a federal secular parliamentary republic divided into seven provinces.
Nepal was admitted to the United Nations in 1955, friendship treaties were signed with India in 1950 and the People's Republic of China in 1960. Nepal hosts the permanent secretariat of the South Asian Association for Regional Cooperation, of which it is a founding member. Nepal is a member of the Non Aligned Movement and the Bay of Bengal Initiative; the military of Nepal is the fifth largest in South Asia. Local legends have it that a Hindu sage named "Ne" established himself in the valley of Kathmandu in prehistoric times, that the word "Nepal" came into existence as the place was protected by the sage "Nemi", it is mentioned in Vedic texts. According to the Skanda Purana, a rishi called. In the Pashupati Purana, he is mentioned as a protector, he is said to have taught there. The name of the country is identical in origin to the name of the Newar people; the terms "Nepāl", "Newār", "Newāl" and "Nepār" are phonetically different forms of the same word, instances of the various forms appear in texts in different times in history.
Nepal is the learned Sanskrit form and Newar is the colloquial Prakrit form. A Sanskrit inscription dated 512 CE found in Tistung, a valley to the west of Kathmandu, contains the phrase "greetings to the Nepals" indicating that the term "Nepal" was used to refer to both the country and the people, it has been suggested that "Nepal" may be a Sanskritization of "Newar", or "Newar" may be a form of "Nepal". According to another explanation, the words "Newar" and "Newari" are vulgarisms arising from the mutation of P to V, L to R. Neolithic tools found in the Kathmandu Valley indicate that people have been living in the Himalayan region for at least eleven thousand years. Nepal is first mentioned in the late Vedic Atharvaveda Pariśiṣṭa as a place exporting blankets, in the post-Vedic Atharvashirsha Upanishad. In Samudragupta's Allahabad Pillar it is mentioned as a border country; the Skanda Purana has a separate chapter, known as "Nepal Mahatmya", with more details. Nepal is mentioned in Hindu texts such as the Narayana Puja.
Legends and ancient texts that mention the region now known as Nepal reach back to the 30th century BC. The Gopal Bansa were one of the earliest inhabitants of Kathmandu valley; the earliest rulers of Nepal were the Kiratas, peoples mentioned in Hindu texts, who ruled Nepal for many centuries. Various sources mention up to 32 Kirati kings. Around 500 BCE, small kingdoms and confederations of clans arose in the southern regions of Nepal. From one of these, the Shakya polity, arose a prince who renounced his status to lead an ascetic life, founded Buddhism, came to be known as Gautama Buddha. By 250 BCE, the southern regions had come under the influence of the Maurya Empire of North India and became a vassal state under the Gupta Empire in the 4th century CE. There is a quite detailed description of the kingdom of Nepal in the account of the renowned Chinese Buddhist pilgrim monk Xuanzang, dating from about 645 CE. Stone inscriptions in the Kathmandu Valley are important sources for the history of Nepal.
The kings of the Lichhavi dynasty have been found to have r
Gaunpalika or gaupalika is the newly formed lower administrative division in Nepal. The Ministry of Federal Affairs and Local Development dissolved the existing village development committees and announced the establishment of this new local body. There are 460 rural municipalities; the main purpose of a gaunpalika is similar to that of a village development committee. Besides this, this division has the authority to collect various taxes like entertainment tax, business tax and residential tax at the local level; the Village Development Committee was dissolved on 10 March 2017. Panchayat was dissolved and turned into VDC by the Constitution of Nepal 1990. According to the English translation of the Constitution of Nepal, the term "gaunpalika" has been used as "village body". However, the Ministry of Federal Affairs and Local Development explained that the term "rural municipality" was coined after opinions from experts and diverse sources; the chief is the head of a rural municipality. A total of 744 chiefs were selected by the government in 10 March 2017.
The rural municipalities will have an annual budget of at least Rs 10 million. Village development committees of Nepal topics