Includes bibliographical references and index.
|Statement||editor-in-chief : Shi Ya feng ; associate editors: Huang Maohuan, Yao Tandong, He Yuanqing.|
|LC Classifications||GB2537 .G53 2008|
|The Physical Object|
|Pagination||xv, 539 p. :|
|Number of Pages||539|
|LC Control Number||2009408846|
Glaciers and Related Environments in China by Shi Yafeng and a great selection of related books, art and collectibles available now at China. Kangshung Glacier - Tibet; Purugangri Glacier - Tibet; Rongbuk Glacier - Tibet; Mingyong Glacier - Yunnan; Indonesia. Carstensz Glacier; West Northwall Firn; East Northwall Firn; All three are on Puncak Meren Glacier on the summit disappeared at some time between and Up close, the sound of global warming at the face of the Urumqi No1 Glacier is a simple, steady drip, drip, drip. Just 30 metres from the main wall, the flood of meltwater becomes so powerful that. Glaciers of China. Wikimedia Commons has media related to Glaciers of China. Subcategories. This category has only the following subcategory. T Pages in category "Glaciers of China" The following 6 pages are in this category, out of 6 total. This list may not reflect recent changes.
Glaciers are usually found in high altitudes and latitudes. Classification Glaciers are of four chief types. Valley, or mountain, glaciers are tongues of moving ice sent out by mountain snowfields following valleys originally formed by streams. In the Alps there are more than 1, valley glaciers. 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. With a warming planet, snow may still fall during the winter, but it may not survive the summer, and the glaciers will get steadily smaller and mountain environments will dry up. We find that glaciers in China have lost a tremendous amount of ice mass since the Little Ice Age maximum: area and ice volume have decreased by and % of the respective amounts of.
Most of the world's glacial ice is found in Antarctica and Greenland, but glaciers are found on nearly every continent, even Africa. Because certain climatic and geographic conditions must be present for glaciers to exist, they are most commonly found above snow line: regions of high snowfall in winter, and cool temperatures in summer. This condition allows more snow to accumulate on the. The most obvious one is the decline in glaciers and snow precipitation in the west of China. Chinese scientists have found that the number of glaciers in this region have decreased by about Glaciers and Glaciation is the classic textbook for all students of glaciation. Stimulating and accessible, it has established a reputation as a comprehensive and essential resource. In this new edition, the text, references and illustrations have been thoroughly updated to give today's reader an up-to-the minute overview of the nature, origin and behaviour of glaciers and the geological and Cited by: Glaciers in China can be categorized into 3 types, i.e. the maritime (temperate) type, sub-continental (sub-polar) type and extreme continental (polar) type, which take 22%, 46% and 32% of the total existing glacier area (59 km2) respectively. Researches indicate that glaciers of the three types show different response patterns to the global by: