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- > Tibet and High-Asia. Results of the Sino-German and Russian-German joint expeditions (III) (supprimer)
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Par Collection Par Auteur- KUHLE, M., (Editeur scientifique) (3)
- CHAOHAI, L. (1)
- FASTOOK, J.L. (1)
- KUHLE, M. (1)
- KUNAKHOVITCH, M.G. (1)
- MIKHALENKI, V.N. (1)
- USHNURTSEV, S.N. (1)
- ZICHU, X. (1)
- DYURGEROV, M.B. (1)
- GROSSWALD, M.G. (1)
- KUHLE, M. (1)
- 1994 (3)
- Altitude ; Asia ; Central Asia ; Climatic variation ; Glacier ; Glacier mass balance ; Model ; Tien Shan (1)
- Altitude ; Asie ; Asie centrale ; Bilan de masse ; Glacier ; Modèle ; Tjan'-Šan' ; Variation climatique (1)
- Asia ; Central Asia ; Glaciation ; Model ; Moraine ; Palaeogeography ; Quaternary ; Snow line ; Tien Shan ; Wurm (1)
- Asie ; Asie centrale ; Glaciation ; Limite d'enneigement ; Modèle ; Moraine ; Paléogéographie ; Quaternaire ; Tjan'-Šan' ; Würm (1)
- China ; Fluvioglacial features ; Glacial valley ; Glaciation ; Moraine ; Palaeogeography ; Quaternary ; Scientific expedition ; Snow line ; Tibet (1)
- Chine ; Expédition scientifique ; Fluvioglaciaire ; Glaciation ; Limite d'enneigement ; Moraine ; Paléogéographie ; Quaternaire ; Tibet ; Vallée glaciaire (1)
- Tibet and High-Asia. Results of the Sino-German and Russian-German joint expeditions (III) (3)
- On the cause of glacier mass balance variations in the Tian Shan Mountains (1)
- Present and Pleistocene glaciation on the north-western margin of Tibet between the Karakorum main ridge and the Tarim Basin, supporting the evidence of a Pleistocene inland glaciation in Tibet (1)
- Würm glaciation of Lake Issyk-Kul area, Tian Shan Mts.: a case study in glacial history of Central Asia (1)
- Asia ; Central Asia ; Glaciation ; Model ; Moraine ; Palaeogeography ; Quaternary ; Snow line ; Tien Shan ; Wurm
- : with a gradual and with an abrupt change in snow-line elevation. It yielded ice-marginal positions which agreed with the field observations.
- that the asynchronous changes in mass balance were primarily due to the increase of summer snow accumulation eastward the Tian Shan. The second reason was the difference in the altitudinal position of the glaciers.
- China ; Fluvioglacial features ; Glacial valley ; Glaciation ; Moraine ; Palaeogeography ; Quaternary ; Scientific expedition ; Snow line ; Tibet