Titlebook: Rockglaciers; Indicators for the P Dietrich Barsch Book 1996 Springer-Verlag Berlin Heidelberg 1996 Permafrost.environment.hydrology

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書目名稱Rockglaciers影響因子(影響力)




書目名稱Rockglaciers影響因子(影響力)學(xué)科排名




書目名稱Rockglaciers網(wǎng)絡(luò)公開度




書目名稱Rockglaciers網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Rockglaciers被引頻次




書目名稱Rockglaciers被引頻次學(xué)科排名




書目名稱Rockglaciers年度引用




書目名稱Rockglaciers年度引用學(xué)科排名




書目名稱Rockglaciers讀者反饋




書目名稱Rockglaciers讀者反饋學(xué)科排名

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Summary and Outstanding Problems,If ice patches do not move they are called glacierets. Both, rockglaciers and glaciers, are, therefore, quite different features. The first are determined by thermal boundary conditions, the second by a surples of snow accumulation versus melting and sublimation of snow at the surface.

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Rockglaciers: Description and Morphometry,in different mountain systems but also locally. Nevertheless, a basic description can be given; a genetic approach, however, which has often been connected with a discussion of size and form in the past, is not intended.

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Introduction,ly important for the future development of high mountain systems in which the high mountain environments or cryogenic belts, e.g., the landscapes above the timberline, are especially endangered. Unfortunately, our knowledge of these geosystems is very limited. It is, therefore, essential to define d

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Definitions,ey indicate alpine or mountain permafrost belts, and, thus, possess a high geodynamic and geoecologic information value. Unfortunately, discussions about rockglaciers are often very confusing. Some students, influenced by semantics, believe that rockglaciers are just debris-covered glaciers (Llibout

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