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Chengguan, Chamdo
Chengguan (; ) synonymously referred to as Chamdo or Qamdo is a major town in the historical region of Kham in the eastern Tibet Autonomous Region of China. The seat of Karub District and Chamdo Prefecture, it is Tibet's third largest city after Lhasa and ShigatseBuckley and Straus 1986, p. 215. with a population of 45,861 in 2010. It is located about east of Lhasa. By road, the distance is via the southern route or via the northern route. It is at an altitude of at the confluence of the rivers Za Qu and Ngom Qu which form the Lancang River (Mekong). Historically, Chamdo was a hub of the Tea Horse Road, leading from Sichuan to Bengal via the Nathu La pass. At the turn of the 20th century it had a population of about 12,000, a quarter of whom were monks. Galden Jampaling Monastery Chengguan was visited by Je Tsongkhapa in 1373 who suggested a monastery be built there. Galden Jampaling Monastery was constructed between 1436 and 1444 by a disciple of Tsongkhapa, Jansem Shera ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Towns Of The People's Republic Of China
When referring to political divisions of China, town is the standard English translation of the Chinese (traditional: ; ). The Constitution of the People's Republic of China classifies towns as third-level administrative units, along with for example townships (). A township is typically smaller in population and more remote than a town. Similarly to a higher-level administrative units, the borders of a town would typically include an urban core (a small town with the population on the order of 10,000 people), as well as rural area with some villages (, or ). Map representation A typical provincial map would merely show a town as a circle centered at its urban area and labeled with its name, while a more detailed one (e.g., a map of a single county-level division) would also show the borders dividing the county or county-level city into towns () and/or township () and subdistrict (街道) units. The town in which the county level government, and usually the division's main ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sichuan
Sichuan (; zh, c=, labels=no, ; zh, p=Sìchuān; alternatively romanized as Szechuan or Szechwan; formerly also referred to as "West China" or "Western China" by Protestant missions) is a province in Southwest China occupying most of the Sichuan Basin and the easternmost part of the Tibetan Plateau between the Jinsha River on the west, the Daba Mountains in the north and the Yungui Plateau to the south. Sichuan's capital city is Chengdu. The population of Sichuan stands at 83 million. Sichuan neighbors Qinghai to the northwest, Gansu to the north, Shaanxi to the northeast, Chongqing to the east, Guizhou to the southeast, Yunnan to the south, and the Tibet Autonomous Region to the west. In antiquity, Sichuan was the home of the ancient states of Ba and Shu. Their conquest by Qin strengthened it and paved the way for Qin Shi Huang's unification of China under the Qin dynasty. During the Three Kingdoms era, Liu Bei's state of Shu was based in Sichuan. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Qamdo Bangda Airport
Qamdo Bamda Airport , also known as Changdu Bangda Airport, is an airport serving Qamdo (Changdu), Tibet Autonomous Region, China. It is located in the village of Bamda (Bangda). Background At an elevation of above sea level, Qamdo Airport was formerly the highest airport in the world. It was surpassed by Daocheng Yading Airport, with an elevation of , on 16 September 2013. It has a very long runway, at , a necessary feature due to the reduction in engine and lift performance that aircraft are subject to at altitude, requiring higher than normal lift-off speeds and therefore longer take-off and landing runs. Runway repairs took place in 2007 and 2013 after decay from the weather. Construction of a new runway has been completed, and the original runway has been closed. Airlines and destinations [Baidu] |
China National Highway 317
China National Highway 317 (G317) runs broadly west to east from Chengdu, Sichuan to Gar County, Ngari Prefecture, Tibet. It is 2,028 kilometres in length and forms an important transportation route in Tibet. As of 2017, Highway 317 passes through the highest vehicular tunnel in the world in the Chola Mountains of Dêgê County. Part of the route is concurrent with the Sichuan-Tibet Highway. Route and distance References See also * China National Highways The China National Highways (CNH/Guodao) () is a network of trunk roads across mainland China. Apart from the expressways of China that are planned and constructed later, most of the CNH are not controlled-access highways. History The bui ... {{China National Highways Transport in Chengdu Transport in Sichuan Roads in Tibet 317 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
China National Highway 214
China National Highway 214 (G214) runs from Xining, Qinghai to Jinghong, Yunnan. It is 3,256 kilometres in length and runs south from Xining towards Tibet, and ends in Yunnan Province. Route and distance See also * China National Highways The China National Highways (CNH/Guodao) () is a network of trunk roads across mainland China. Apart from the expressways of China that are planned and constructed later, most of the CNH are not controlled-access highways. History The bui ... External linksOfficial website of Ministry of Transport of PRC 214 Transport in Qinghai Roads in Tibet Transport in Yunnan {{PRChina-road-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diurnal Temperature Variation
In meteorology, diurnal temperature variation is the variation between a high air temperature and a low temperature that occurs during the same day. Temperature lag Temperature lag is an important factor in diurnal temperature variation: peak daily temperature generally occurs ''after'' noon, as air keeps net absorbing heat even after noon, and similarly minimum daily temperature generally occurs substantially after midnight, indeed occurring during early morning in the hour around dawn, since heat is lost all night long. The analogous annual phenomenon is seasonal lag. As solar energy strikes the Earth's surface each morning, a shallow layer of air directly above the ground is heated by conduction. Heat exchange between this shallow layer of warm air and the cooler air above is very inefficient. On a warm summer's day, for example, air temperatures may vary by from just above the ground to waist height. Incoming solar radiation exceeds outgoing heat energy for many hours afte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subtropical Highland Climate
An oceanic climate, also known as a marine climate, is the humid temperate climate sub-type in Köppen classification ''Cfb'', typical of west coasts in higher middle latitudes of continents, generally featuring cool summers and mild winters (for their latitude), with a relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 45 and 63 latitude, most notably in northwestern Europe, northwestern America, as well as New Zealand. Precipitation Locations with oceanic climates tend to feature frequent cloudy conditions with precipitation, low hanging clouds, and frequent fronts and storms. Thunderstorms are normally few, since strong daytime heating and hot and cold air masses meet infrequently in the region. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter. M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Humid Continental
A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, typified by four distinct seasons and large seasonal temperature differences, with warm to hot (and often humid) summers and freezing cold (sometimes severely cold in the northern areas) winters. Precipitation is usually distributed throughout the year but often do have dry seasons. The definition of this climate regarding temperature is as follows: the mean temperature of the coldest month must be below or depending on the isotherm, and there must be at least four months whose mean temperatures are at or above . In addition, the location in question must not be semi-arid or arid. The cooler ''Dfb'', ''Dwb'', and ''Dsb'' subtypes are also known as hemiboreal climates. Humid continental climates are generally found between latitudes 30° N and 60° N, within the central and northeastern portions of North America, Europe, and Asia. They are rare and isolat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tsongkhapa
Tsongkhapa ('','' meaning: "the man from Tsongkha" or "the Man from Onion Valley", c. 1357–1419) was an influential Tibetan Buddhist monk, philosopher and tantric yogi, whose activities led to the formation of the Gelug school of Tibetan Buddhism.Tsong khapa (2006), pp. ix-x. He is also known by his ordained name Losang Drakpa (, Skt. Sumatikīrti) or simply as "Je Rinpoche" (, "Precious Lord"). He is also known by Chinese as Zongkapa Lobsang Zhaba or just Zōngkàbā (宗喀巴). Tsongkhapa was born in Amdo, the son of a Tibetan Longben Tribal leader who also once served as an official of the Yuan Dynasty. As a monk, he studied under numerous teachers of the various Tibetan Buddhist traditions which flourished in central Tibet, including Sakya, Jonang, Kagyu and Kadam. Tsongkhapa was a prolific author with a broad knowledge of Buddhist philosophy, logic, hermeneutics and practice. He wrote numerous works on madhyamaka philosophy (such as ''Ocean of Reasoning,'' a comment ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Galden Jampaling Monastery
Galden Jampaling Monastery () is a Buddhist monastery in Chamdo, Tibet, China China, officially the People's Republic of China (PRC), is a country in East Asia. It is the world's most populous country, with a population exceeding 1.4 billion, slightly ahead of India. China spans the equivalent of five time zones and .... Each year on 16 March the temple celebrates The Butter Sculpture Festival with the spectacular "Guqing" God DanceMayhew and Kohn 2005, p. 241. References Bibliography * Buckley, Michael and Straus, Robert (1986): ''Tibet: a travel survival kit'', Lonely Planet Publications. South Yarra, Victoria, Australia. . * Gruschke, Andreas (2004): ''Chamdo town'' in: ''The Cultural Monuments of Tibet’s Outer Provinces: Kham - vol. 1. The TAR part of Kham'', White Lotus Press, Bangkok 2004, pp. 36–45. * Mayhew, Bradley and Kohn, Michael. (2005). ''Tibet''. 6th Edition. Lonely Planet. {{Buddhism-stub Buddhist monasteries in Tibet Buddhist temples ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Je Tsongkhapa
Tsongkhapa ('','' meaning: "the man from Tsongkha" or "the Man from Onion Valley", c. 1357–1419) was an influential Tibetan Buddhist monk, philosopher and tantric yogi, whose activities led to the formation of the Gelug school of Tibetan Buddhism.Tsong khapa (2006), pp. ix-x. He is also known by his ordained name Losang Drakpa (, Skt. Sumatikīrti) or simply as "Je Rinpoche" (, "Precious Lord"). He is also known by Chinese as Zongkapa Lobsang Zhaba or just Zōngkàbā (宗喀巴). Tsongkhapa was born in Amdo, the son of a Tibetan Longben Tribal leader who also once served as an official of the Yuan Dynasty. As a monk, he studied under numerous teachers of the various Tibetan Buddhist traditions which flourished in central Tibet, including Sakya, Jonang, Kagyu and Kadam. Tsongkhapa was a prolific author with a broad knowledge of Buddhist philosophy, logic, hermeneutics and practice. He wrote numerous works on madhyamaka philosophy (such as ''Ocean of Reasoning,'' a comment ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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