4 edition of Glaciers and Environment on the Qinghai-Xizang (Tibet Plateau) found in the catalog.
Glaciers and Environment on the Qinghai-Xizang (Tibet Plateau)
August 1995 by Science Pr .
Written in English
|Contributions||Xie Zichu (Editor), V. M. Kotlyakov (Editor)|
|The Physical Object|
Book Review (1) Arctic, Antarctic, and Alpine Research. VIEW ALL ABSTRACTS + Articles. Mountain Birch Seedlings in the Treeline Ecotone, Subarctic Finland: Variation in Above- and Below-Ground Growth Depending on Microtopography Precipitation Distribution along the Qinghai-Xizang (Tibetan) Highway, Summer The cryosphere consists of water in the solid form at the Earth's surface and includes, among others, snow, sea ice, glaciers and ice sheets. Since the s the cryosphere and its components have often been considered as indicators of global warming because rising temperatures can enhance the melting of solid water (e.g. Barry et al Seismological Press. This book contains black and white pictures of damage from eight earthquakes of magnitude. The earthquakes all occurred in China between and While the book is in Chinese, the photos are self-explanatory and quite interesting, well worth the price of the book.
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Glaciers and environment in the Qinghai-Xizang (Tibet) Plateau. Beijing, China: Science Press, (OCoLC) Document Type: Book: All Authors / Contributors: Suihan Yao; Shengchao Peng; Zhongguo ke xue yuan. Lanzhou bing chuan dong tu yan jiu suo.; Rossiĭskai︠a︡ akademii︠a︡ nauk.
Institute of Geography. China Scientific Books Glaciers and Related Environments in China - Author: Editor-in-Chief: Shi YafengLanguage: EnglishISBN/ISSN: Published on: HardcoverThis book represents the culmination of a half century of Chinese research into the cryospheric sciences that was initiated and led by its Editor-in-Chief Professor Shi Yafeng, the father of glaciology in China.
The Tibetan Plateau (Tibetan: བོད་ས་མཐོ།, Wylie: bod sa mtho), also known in China as the Qinghai–Tibet Plateau or the Qing–Zang Plateau (Chinese: 青藏高原; pinyin: Qīng–Zàng Gāoyuán) or as the Himalayan Plateau in India, is a vast elevated plateau in Central Asia and East Asia, covering most of the Tibet Autonomous Region, Northwestern Yunnan, Western Range coordinates: 33°N 88°E /.
The Comprehensive Scientific Expedition to the Qinghai-Xizang Plateau, Academia Sinica, pp. Science Press, Beijing (in Chinese).
Zheng, B.X. and Li, J.J. Quaternary glaciation of the Qinghai-Xizang Plateau. In:Geologicaland EcologicalStudiesof the Qinghai-Xizang Plateau, Vol. 2 -Environment and Ecology, pp. Cited by: Periglaciation (adjective: "periglacial", also referring to places at the edges of glacial areas) describes geomorphic processes that result from seasonal thawing of snow in areas of permafrost, the runoff from which refreezes in ice wedges and other structures.
"Periglacial" suggests an environment located on the margin of past glaciers. However, freeze and thaw. Wu, L. Poiqu (Bhote-Sun Koshi) and Rongxer (Tama Koshi) Basins, Tibet Autonomous Region, PR China.
Inventory of glaciers and glacial lakes and the identification of potential glacial lake outburst floods (GLOFs) affected by global warming in the Mountains of Himalayan by: 1. The Periglacial Environment, Fourth Edition, is an authoritative overview of the worlds cold, non-glacial environments.
First published in and subsequently revised in andthe text has been the international standard for nearly 40 years. The Fourth Edition continues to be a personal interpretation of the frost-induced conditions, geomorphic processes and landforms.
glaciers in Tibet are retreating due to the ongoing changes in the climatic variables over the plateau. The dramatic retreat of all the glaciers on the Tibetan Plateau in ’s is related to the continuous warming on the plateau since s.
In a more recent study about the sensitivity of cold glaciers, it was indicated that changes (rise). Recent Shrinkage and Hydrological Response of Hailuogou Glacier, A Monsoon Temperate Glacier on the East Slope of Mount Gongga, China Article (PDF Available) in Journal of Glaciology 56() A Proposal for International Multi-Institutional Ice-Coring Project in Central Asia () N.
Takeuchi. Stable-isotope time series and precipitation origin from firn cores and snow samples, Altai glaciers, Siberia. Glaciers and Environment in the Qinghai-Xizang (Tibet) Plateau.
The Gongga Mountain, Science Press, Beijing, New. The mountains formed a barrier against the incursion of the Indian monsoon, so that precipitation decreased sharply on the northern flank of the Himalayas, and the climate to the north became cold and dry.
All of the glaciers on the Qinghai-Xizang Plateau underwent extensive by: The Periglacial Environment, Fourth Edition, is an authoritative overview of the worlds cold, non-glacial environments. First published in and subsequently revised in andthe text has been the international standard Pages: Glaciers in the Hengduan Mountains （out of print), The Hengduan Range is complicated in geological structure and active in new tectonic movements.
It lies on the east flank of the juncture area where south Asia and Eurasis are mounted. It is the tr,All books from China,especially scientific and academic books,export Chinese and English version books to libraries and book.
Uplift of Qinghai-Xizang (Tibet) Plateau Past Glaciations, Permafrost and Frozen Ground Extent of Past Glaciations Relict Permafrost Pleistocene Periglacial Environments General Considerations Problems of Palaeo-Environmental Reconstruction Ice Age Mammals.
Abstract. The uplift of the Himalaya and Qinghai-Xizang plateau began at the end of Pliocene to the beginning of Early Pleistocene, changing the atmospheric circulation in Asia, enhancing the South Asian monsoon and enormously effecting the climatic conditions and glacial by: Although lake-level highstands in Tibet are often attributed to the melting of glaciers (Li et al., ; Wang et al., ; Kong et al., b), the relation between lake-level changes and the.
"Mass-balance changes and climatic characteristics of the Golubina and Djankuat glaciers" (Tien Shan, Caucasus). 2 maps in scale. Book: Atlas of World Snow and Ice Resources, International Hydrological Project. Moscow, RUSSIA. Aizen V.B., Aizen E. et al. Book: Glaciers and Environment in the Qinghai-Xizang (Tibet) Plateau.
Qinghai-Xizang (Tibet) Plateau 38 Alpine Climates 39 Climates of Low Annual Temperature Range 39 Antarctica: A Special Case 40 Ground Climates 40 The n-Factor 41 The Thermal Offset 42 Periglacial Climates and the Cryosphere 44 Advanced Reading 45 Discussion Topics Alpine Exploration in Central Asia glacier-climatic research group at the University of Idaho Aizen E.
et al., Book: Glaciers and Environment in the Qinghai-Xizang (Tibet) Plateau. The Gongga Mountain, Science Press, Beijing, New York, p.
Aizen V.B., Aizen E. et al. Monograph, Glaciers and Environment in the Qinghai. The Periglacial Environment, Third Edition**,** provides an authoritative overview of the worldâ??s cold, non-glacial is is placed upon the North American and Eurasian polar lowlands, but examples are also drawn from Antarctica, the Qinghai-Xizang (Tibet) Plateau, and the northern : Wiley.
Climate change and its impacts on water resources and crop production is a major force with which China and the rest of the world will have to Cited by: The Periglacial Environment, Third Edition, provides an authoritative overview of the world's cold, non-glacial environments.
Emphasis is placed upon the North American and Eurasian polar lowlands, but examples are also drawn from Antarctica, the Qinghai-Xizang (Tibet) Plateau, and the northern : $ Map of the Glaciers, Frozen Ground and Deserts in China (1: ), The data sources of the Map of Glaciers, Frozen Ground and Deserts of China (1: two standard-sized sheets) are mainly from recent scientific achievements-the data source of the glaciers: G,All books from China,especially scientific and academic books,export Chinese and English version books to libraries and book.
Highlights of this report: As the Chinese government released a new white paper claiming it supports “ecological conservation” in Tibet, state media announced that China has stepped up production of bottled water from Tibet’s endangered glaciers, and news emerged of more major hydropower schemes in central Tibet, financed by the state.
The Periglacial Environment, Third Edition, provides an authoritative overview of the worldaAA's cold, non-glacial environments.
Emphasis is placed upon the North American and Eurasian polar lowlands, but examples are also drawn from Antarctica, the Qinghai-Xizang (Tibet) Plateau, and the northern mid-latitudes.5/5(2). The Periglacial Environment, Third Edition, provides an authoritative overview of the world’s cold, non-glacial environments.
Emphasis is placed upon the North American and Eurasian polar lowlands, but examples are also drawn from Antarctica, the Qinghai-Xizang (Tibet) Plateau, and the northern mid-latitudes.
Table of contents for The periglacial environment / Hugh French. Bibliographic record and links to related information available from the Library of Congress catalog.
Note: Contents data are machine generated based on pre-publication provided by the publisher. Annual firn accumulation on the Rongbuk Glacier, which drains the north slope of Mt. Qomolangma, is to mm of water equivalent.
Inmm of glacier ice was melted. The ice melt contribution to the river discharge will be higher in dry years and lower, but compensated for by snow melt, in wet years. Using areas of clean ice measured from Landsat Author: R.
Krimmel. Finally, the extensive periglacial region of the Qinghai-Xizang (Tibet) Plateau has so far not been adequately described in the western literature, yet it is the same size as the North American or Eurasian periglacial regions. Thus, I have attempted to incorporate, wherever appropriate, data from this unusual environment.
The Periglacial Environment, Third Edition, provides an authoritative overview of the worlda s cold, non-glacial environments. Emphasis is placed upon the North American and Eurasian polar lowlands, but examples are also drawn from Antarctica, the Qinghai-Xizang (Tibet) Plateau, and the northern mid-latitudes.
The Tibetan (Qinghai-Xizang) Plateau, known as the “roof of the world”, is sparsely populated, with an average population density of people/km 2 in [10,11].It is a sensitive region to climate change [12,13], and has been regarded as an ideal place to study the impact of climate change on environment [14,15,16,17].Since“the Western Regions Development Cited by: The third Pole Environment Database focuses on scientific data sharing on Tibet Plateau.
Key data sets on cryosphere are also reviewed by this paper, which include glacier inventory data, glacial lake inventory in HKH region, permafrost maps in China and Tibet.
Li, Z. et al. Changes of climate, glaciers and runoff in China’s monsoonal temperate glacier region during the last several decades. Quat. Int. / (). The Periglacial Environment, Fourth Edition, is an authoritative overview of the world's cold, non-glacial environments.
First published in and subsequently revised in andthe text has been the international standard for nearly. China's glaciers have retreated by about 7, square km, an 18 percent retreat since the s, Chinese scientists have found.
December 09 Work began on the rail line from Chengdu, capital of southwest Sichuan Province to Ya'an, a city in the province on Saturday.
The km Chengdu-Ya'an section is an important part of the Sichuan-Tibet railway. Based on numerical experiments undertaken with nine climate models, the glacier equilibrium line altitudes (ELAs) in western China during the last glacial maximum (LGM) are investigated to deepen our understanding of the surface environment on the Tibetan Plateau.
Relative to the preindustrial period, the summer surface air temperatures decrease by 4–8°C. The Environment and Ecosystem in the Eastern Edge of Qinghai-Xizang Plateau. – (Sichuan University Press, ). Zhang R. Z., Zheng D. & Yang Q.
Physical Geography of Xizang (Tibet). 69–86 (Science Press, ). Bremond L., Alexandre A., Peyron O. & Guiot J. Grass water stress estimated from phytoliths in West by: This book will give you a firm basis for an understanding of greenhouse gases, the critical role they play in global warming, and how you can help make a difference in reducing them.
About the state of some of the Tien Shan glaciers during the period of the International Geophysical Year (IGY).
IASH Publ. 54 (General Assembly of Helsinki – Snow and Ice), - Zhang, T. and Yang, by: 3. 1 Introduction. China's Tibetan Plateau, also called the Qinghai‐Tibetan Plateau or the Qinghai‐Xizang Plateau, is a unique geographical unit due to its low temperatures, geographical location, high elevation (averaging more than m above sea level (asl)), and large expanse; it stretches between 25°N and 40°N and between 74°E and °E (Figure 1) and covers an Cited by:.
Research into projected climate and environmental changes across the Tibetan Plateau in the 21st century is reviewed. Climate and environmental factors involved include surface air temperature, rainfall, extreme weather and climate events, frozen soil, snow cover, glaciers, runoff, and vegetation.
Projections are mainly from climate model simulations under the .Global warming has accelerated the retreat of glaciers.
Over the past 30 years, the area of glaciers has decreased by sq km annually on the Qinghai-Tibet Plateau and the permafrost has experienced patches of degradation, manifested by reduction of the seasonal frozen depth and rising thaw depth.Atlas of Clouds Over the Qinghai-Xizang Plateau, Science Press & Academic Press, CCICED Task Force Summary Report: Strategy and Policies on Environment and Development.
in Western China, CCICED, State Council notice on National Main Function Zoning plan, No. scs 6 March