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Glaciers Of Bhutan
The glaciers of Bhutan, which covers about 3 percent of the total surface area, are responsible for feeding all rivers of Bhutan except the Amochu and Nyere Amachu. Not much historical information is available on these glacial systems; the first modern survey was conducted by Augusto Gansser-Biaggi in the 1970s, who developed a chronology of past glaciations, and warned of imminent glacial lake outburst floods (GLOF) in Lunana. This prompted the Geological Survey of India (GSI) and Geological Survey of Bhutan (GSB) to carry out joint surveys in the mid-80s, and their report rejected Biaggi's threat-assessment. On 7 October 1994, a GLOF from Luggye lake (part of Lunana glacial system) led to over 20 fatalities in Punakha. This disaster, the first of its kind in Modern Bhutan, increased the frequency of glacial-system-surveys by manifold. Evaluation of GLOF hazard has since formed a significant component of glacial expeditions. Multiple inventory-lists of glaciers and glacial lakes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bhutan
Bhutan (; dz, འབྲུག་ཡུལ་, Druk Yul ), officially the Kingdom of Bhutan,), is a landlocked country in South Asia. It is situated in the Eastern Himalayas, between China in the north and India in the south. A mountainous country, Bhutan is known as "Druk Yul," or "Land of the Thunder Dragon". Nepal and Bangladesh are located near Bhutan but do not share a land border. The country has a population of over 727,145 and territory of and ranks 133rd in terms of land area and 160th in population. Bhutan is a Constitutional Democratic Monarchy with King as head of state and Prime Minister as head of government. Mahayana and Vajrayana Buddhism is the state religion and the Je Khenpo is the head of state religion. The subalpine Himalayan mountains in the north rise from the country's lush subtropical plains in the south. In the Bhutanese Himalayas, there are peaks higher than above sea level. Gangkhar Puensum is Bhutan's highest peak and is the highest uncl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mo Chhu
Mo Chhu is a major river in Bhutan. The word "Chhu" means "river" or "water" in Dzongkha, the official national language in Bhutan. The river rises in Gasa Dzongkhag (district) near the border between Bhutan and Tibet. From there, the Mo Chhu flows generally southward to Punakha in central Bhutan, where it joins the Pho Chhu from the northeast. The confluence of the two streams is immediately below the Punakha Dzong, which is the winter home of the Dratshang Lhentshog (Central Monk Body) and the Je Khenpo. The combined streams are then joined by the Dang Chhu near the town of Wangdue Phodrang, and the name of the river becomes the Puna Tsang Chhu. The river then flows through Dagana and Tsirang Districts. After leaving Bhutan near the town of Lhamoidzingkha, formerly known as Kalikhola,From Damphu to Lhamoidzingkha, in the Bhutanese daily "Kuensel", 21 May 2020 https://kuenselonline.com/from-damphu-to-lhamoidzingkha/ the river enters Assam in India and is known as the Sankosh. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Government Of Bhutan
The Government of Bhutan has been a constitutional monarchy since 18 July 2008. The King of Bhutan is the head of state. The executive power is exercised by the Lhengye Zhungtshog, or council of ministers, headed by the Prime Minister. Legislative power is vested in the bicameral Parliament, both the upper house, National Council, and the lower house, National Assembly. A royal edict issued on April 22, 2007 lifted the previous ban on political parties in anticipation of the National Assembly elections in the following year. In 2008, Bhutan adopted its first modern Constitution, codifying the institutions of government and the legal framework for a democratic multi-party system. Sovereignty Bhutanese external relations and foreign policies were put under British control following the 1910 Treaty of Punakha. However, due to the policy of self-imposed isolationism, the effect of the treaty was limited to an extent. After Indian independence in 1949, Bhutan and India agreed to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sankosh River
Sankosh (also Mo Chu, and Svarnakosha) is a river that rises in northern Bhutan and empties into the Brahmaputra in the state of Assam in India. In Bhutan, it is known as the Puna Tsang Chu below the confluences of several tributaries near the town of Wangdue Phodrang. The two largest tributaries are the Mo Chhu and Pho Chhu, which flow together at Punakha. The Punakha dzong, which is situated immediately above the confluence of the two rivers, is one of the most beautiful dzongs in Bhutan and the winter residence of the Dratshang Lhentshog. The upper reaches of the Pho Chhu are susceptible to ice blockages, and the dzong has been damaged on several occasions by glacial lake outburst floods. After it enters in India, it flows on the border of Assam and West Bengal. At Wangdue Phodrang, elevation , the river is joined by the west flowing Tang Chuu and it enters a precipitous gorge. The highway running south from Wangdue Phodrang to Dagana follows the river for much of its cou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lunana Gewog
Lunana Gewog is a gewog (village block) of Gasa District, Bhutan. The village Lunana is the administrative center of Lunana Gewog. The gewog lies almost entirely within protected areas, mostly in Jigme Dorji National Park, though eastern sections are part of Wangchuck Centennial Park. Lunana contains many of Bhutan's glaciers. In addition to the national language, Dzongkha, many locals speak Lunanakha. The closure of the Tibetan border following the Chinese invasion of Tibet brought changes to neighboring areas, as refugees from Tibet arrived with their yaks, which they sold off at low prices. However, because there were no direct routes into Lunana from Tibet, yaks were brought into Lunana from Laya and Sephu in Wangdue Phodrang District Wangdue Phodrang District ( Dzongkha: དབང་འདུས་ཕོ་བྲང་རྫོང་ཁག་; Wylie: ''Dbang-'dus Pho-brang rdzong-khag''; previously spelled "Wangdi Phodrang") is a dzongkhag (district) of central Bhu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Intergovernmental Panel On Climate Change
The Intergovernmental Panel on Climate Change (IPCC) is an intergovernmental body of the United Nations. Its job is to advance scientific knowledge about climate change caused by human activities. The World Meteorological Organization (WMO) and the United Nations Environment Programme (UNEP) established the IPCC in 1988. The United Nations endorsed the creation of the IPCC later that year. It has a secretariat in Geneva, Switzerland, hosted by the WMO. It has 195 member states who govern the IPCC. The member states elect a bureau of scientists to serve through an assessment cycle. A cycle is usually six to seven years. The bureau selects experts to prepare IPCC reports. It draws the experts from nominations by governments and observer organisations. The IPCC has three working groups and a task force, which carry out its scientific work. The IPCC informs governments about the state of knowledge of climate change. It does this by examining all the relevant scientific literature ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rock Glacier
Rock glaciers are distinctive geomorphological landforms, consisting either of angular rock debris frozen in interstitial ice, former "true" glaciers overlain by a layer of talus, or something in-between. Rock glaciers are normally found at high latitudes and/or elevations, and may extend outward and downslope from talus cones, glaciers or terminal moraines of glaciers. There are two types of rock glaciers: periglacial glaciers (or talus-derived glaciers), and glacial rock glaciers, such as the Timpanogos Glacier in Utah, which are often found where glaciers once existed. Possible Martian rock glacier features have been identified by the Mars Orbiter spacecraft. A rock glacier, especially if its origin is unclear, can be considered as a discrete debris accumulation. Formation The two known factors that must be present in order to create rock glaciers are low ice velocity and permafrost. Most glacial rock glaciers are created by the recession of debris covered glaciers. Glacial ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kuri Chhu
The Kuri Chhu, also known as the Lhozhag Xung Qu (tib. lho brag gzhung chu) or Norbu Lag Qu (tib. nor bu lag chu), is a major river of eastern Bhutan, that has formed a scenic valley with high peaks and steep hills. Kuri Chhu is a tributary of the Manas River system, which is the largest river of Bhutan and a major tributary of the Brahmaputra River that drains most of eastern Bhutan. Course The Kuri Chhu originates from the Kula Kangri Glacier in the Tibet Autonomous Region of People's Republic of China where it is known as the Lhozhag Nub Qu (Tibetan: ''lho brag nub chu'', Roman Dzongkha: ''Lhobrak Chhu'') and Xung Qu (Tibetan: gzhung chu), and another origin is the Lhozhag Xar Qu (Tibetan: ''lho brag shar chu'') a.k.a. Damxoi Xung Qu (tib. ''gtam zhol gzhung chu'') originates between the Xoijin Qênri and the Tar Lhari. It crosses into Bhutan at a relatively low elevation of , flowing in a southerly direction up to Nye and changes its course to south-easterly until it reach ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
