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Bajura District
Bajura District ( ne, बाजुरा जिल्ला ), a part of Sudurpashchim Province, is one of the seventy-seven districts of Nepal. The district, with Martadi (today part of Badimalika municipality) as its district headquarters, covers an area of and had a population of 108,781 in 2001 and 134,912 in 2011. The annual rainfall is about 13,433 mm and temperatures vary from 0 °C to 40 °C. The livelihood of more than 80% of the district population depends on agriculture farming, mainly small scale livestock. Due to low level of agricultural production, the majority of the households face acute food shortages for a large part of the year. According to the National Census 2011, the total population of the district is 134,912 comprising 69,106 female (51%) and 65,806 male (49%) residing in 24,908 households. Bajura district has an average population density of around 62 people per square km. The average family size is 5.4. Life expectancy of the people ...
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Districts Of Nepal
Districts in Nepal are second level of administrative divisions after provinces. Districts are subdivided in municipalities and rural municipalities. There are seven provinces and 77 districts in Nepal. After the state's reconstruction of administrative divisions, Nawalparasi District and Rukum District were divided into Parasi District (officially Nawalparasi (West of Bardaghat Susta) District) and Nawalpur District (officially Nawalparasi (East of Bardaghat Susta) District), and Eastern Rukum District and Western Rukum District respectively. District official include: * Chief District Officer, an official under Ministry of Home Affairs is appointed by the government as the highest administrative officer in a district. The C.D.O is responsible for proper inspection of all the departments in a district such as health, education, security and all other government offices. * District Coordination Committee acts as an executive to the District Assembly. The DCC coordinates with ...
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List Of Cities In Nepal
Cities and towns in Nepal are Municipal corporation, incorporated under municipality. A municipality in Nepal is a sub-unit of a district. The Government of Nepal has set-out a minimum criteria for municipalities. These criteria include a certain population, infrastructure and revenues. Presently, there are 293 municipalities in Nepal among which 6 are metropolis, 11 are sub-metropolis and 276 are municipal councils. Other than that there are 460 rural municipalities totaling 753 local level government within Nepal. Kathmandu, the capital, is also the largest city. In terms of area, Pokhara is the largest Metropolitan City, metropolitan city covering a subtotal of 464.28 km2 while Lalitpur, Nepal, Lalitpur is the smallest, with an area of 36.12 km2. Ghorahi is the largest sub-metropolitan city with an area of 522.21 km2 where as Dhangadhi is the largest sub-metropolitan city by a population of 204,788. Budhanilkantha with a population of 179,688 is the largest m ...
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Chhetri
Chhetri (Kshetri, Kshettri, Kshetry or Chhettri), ( ne, क्षेत्री ; IAST: ''Kṣetrī'') historically called Kshettriya or Kshetriya or Khas are Nepali speakers of Khas community, some of whom trace their origin to migration from medieval India. Chhetri was a caste of administrators, governor and military elites in the medieval Khas Kingdom and Gorkha Kingdom (later unified Kingdom of Nepal). The nobility of the Gorkha Kingdom mainly originated from Chhetri families. They also had a strong presence in civil administration affairs. The bulk of prime ministers of Nepal before the democratization of Nepal belonged to this caste as a result of the old Gorkhali aristocracy. Gorkha-based aristocratic Chhetri families included the Pande dynasty, the Basnyat dynasty, the Kunwar family, and the Thapa dynasty, (Rana dynasty and other Kunwars). Khas Chhetris were traditionally considered a division of the Khas people with Khas Brahmin (commonly called Khas Bahun). They m ...
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Khas People
Khas people (; ne, खस) popularly known as Khas Arya are an Indo-Aryan peoples, Indo-Aryan ethno-linguistic group native to the Himalayas, Himalayan region of South Asia, what is now present-day Nepal, Indian states of Uttarakhand, West Bengal and Sikkim. Historically, Khas were the speakers of an ancient ''Khas language'' from the Indo-Aryan language family and the earliest recorded speakers of the Western Pahari languages. The large portion of the Indo-Aryan speakers throughout lower Himalayas were the Khas people. An Indo-Aryan migrations, intrusion of this tribe from the Western Himalayas, Western and Northwestern Himalayas into Central Himalayas is substantiated by the early linguistic evidences related to the Nepali language. They were also known as Parbatiyas/Parbates and are currently known as Paharis/Pahadis. They were also referred to as Yartse in Tibet and are also known as Khasan by Bhotia people. The term ''Khas'' has now become obsolete, as the Khas people hav ...
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Sherpa Language
Sherpa (also Sharpa, Xiaerba, or Sherwa) is a Tibetic language spoken in Nepal and the Indian state of Sikkim, mainly by the Sherpa. The majority speakers of the Sherpa language live in the Khumbu region of Nepal, spanning from the Chinese (Tibetan) border in the east to the Bhotekosi River in the west. About 200,000 speakers live in Nepal (2001 census), some 20,000 in Sikkim (1997) and some 800 in Tibetan Autonomous Region (1994). Sherpa is a subject-object-verb (SOV) language. Sherpa is predominantly a spoken language, although it is occasionally written using either the Devanagari or Tibetan script. Phonology Sherpa is a tonal language. Sherpa has the following consonants: Consonants * Stop sounds can be unreleased in word-final position. * Palatal sounds can neutralize to velar sounds when preceding . * can become a retroflex nasal when preceding a retroflex stop. * can have an allophone of when occurring in fast speech. Vowels * Vowel sounds have the ...
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2011 Nepal Census
Nepal conducted a widespread national census in 2011 by the Nepal Central Bureau of Statistics. Working with the 58 municipalities and the 3915 Village Development Committees at a district level, they recorded data from all the municipalities and villages of each district. The data included statistics on population size, households, sex and age distribution, place of birth, residence characteristics, literacy, marital status, religion, language spoken, caste/ethnic group, economically active population, education, number of children, employment status, and occupation. *Total population in 2011: 26,494,504Central Bureau of Statistics of Nepal: ''Major Highlights''.
*Increase since last census 2001: 3,343,081 *Annual population growth rate (exponental growth): 1.35 *Number of households ...
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Snow Line
The climatic snow line is the boundary between a snow-covered and snow-free surface. The actual snow line may adjust seasonally, and be either significantly higher in elevation, or lower. The permanent snow line is the level above which snow will lie all year. Background 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 temporal and 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, and therefore may be different from year to year. The snow line is measured using automatic cameras, 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 ...
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Montane Ecology
Montane ecosystems are found on the slopes of mountains. The alpine climate in these regions strongly affects the ecosystem because temperatures fall as elevation increases, causing the ecosystem to stratify. This stratification is a crucial factor in shaping plant community, biodiversity, metabolic processes and ecosystem dynamics for montane ecosystems. Dense montane forests are common at moderate elevations, due to moderate temperatures and high rainfall. At higher elevations, the climate is harsher, with lower temperatures and higher winds, preventing the growth of trees and causing the plant community to transition to montane grasslands, shrublands or alpine tundra. Due to the unique climate conditions of montane ecosystems, they contain increased numbers of endemic species. Montane ecosystems also exhibit variation in ecosystem services, which include carbon storage and water supply. Life zones As elevation increases, the climate becomes cooler, due to a decrease in a ...
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Temperate Climate
In geography, the temperate climates of Earth occur in the middle latitudes (23.5° to 66.5° N/S of Equator), which span between the tropics and the polar regions of Earth. These zones generally have wider temperature ranges throughout the year and more distinct seasonal changes compared to tropical climates, where such variations are often small and usually only have precipitation changes. In temperate climates, not only do latitudinal positions influence temperature changes, but sea currents, prevailing wind direction, continentality (how large a landmass is) and altitude also shape temperate climates. The Köppen climate classification defines a climate as "temperate" C, when the mean temperature is above but below in the coldest month to account for the persistency of frost. However, other climate classifications set the minimum at . Zones and climates The north temperate zone extends from the Tropic of Cancer (approximately 23.5° north latitude) to the Arctic ...
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Subtropics
The subtropical zones or subtropics are geographical and climate zones to the north and south of the tropics. Geographically part of the temperate zones of both hemispheres, they cover the middle latitudes from to approximately 35° north and south. The horse latitudes lie within this range. Subtropical climates are often characterized by hot summers and mild winters with infrequent frost. Most subtropical climates fall into two basic types: humid subtropical (Koppen climate Cfa), where rainfall is often concentrated in the warmest months, for example Southeast China and the Southeastern United States, and dry summer or Mediterranean climate (Koppen climate Csa/Csb), where seasonal rainfall is concentrated in the cooler months, such as the Mediterranean Basin or Southern California. Subtropical climates can also occur at high elevations within the tropics, such as in the southern end of the Mexican Plateau and in Da Lat of the Vietnamese Central Highlands. The six climate cl ...
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Tropical Climate
Tropical climate is the first of the five major climate groups in the Köppen climate classification identified with the letter A. Tropical climates are defined by a monthly average temperature of 18 °C (64.4 °F) or higher in the coolest month, and feature hot temperatures all year-round. Annual precipitation is often abundant in tropical climates, and shows a seasonal rhythm but may have seasonal dryness to varying degrees. There are normally only two seasons in tropical climates, a wet (rainy / monsoon) season and a dry season. The annual temperature range in tropical climates is normally very small. Sunlight is intense in these climates. There are three basic types of tropical climates within the tropical climate group: tropical rainforest climate (Af), tropical monsoon climate (Am) and tropical wet and dry climate or tropical savannah (Aw for dry winters, and As for dry summers), which are classified and distinguished by the precipitation and the precipitation lev ...
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Geography Of Nepal
Nepal measures about along its Himalayan axis by across. It has an area of . Nepal is landlocked by China's Tibet Autonomous Region to the north and India on other three sides. West Bengal's narrow ''Siliguri Corridor'' separate Nepal and Bangladesh. To the east are Bhutan and India. Landform regions For a country of its size, Nepal has tremendous geographic diversity. It rises from as low as elevation in the tropical Terai—the northern rim of the Gangetic Plain, through beyond the perpetual snow line to 90 peaks over including Earth's highest ( Mount Everest or ''Sagarmatha''). In addition to the continuum from tropical warmth to cold comparable to polar regions, average annual precipitation varies from as little as in its narrow proportion of the rainshadow north of the Himalayas to as much as on windward slopes, the maximum mainly resting on the magnitude of the South Asian monsoon. Forming south-to-north transects, Nepal can be divided into three belts: Terai, ...
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