Glaciers of the Orulgan Range: assessment of the current state and possible development for the middle of the 21st century

Author:

Ananicheva Maria D.ORCID,Karpachevsky Andrey

Publisher

Springer Science and Business Media LLC

Subject

Earth-Surface Processes,Geology,Pollution,Soil Science,Water Science and Technology,Environmental Chemistry,Global and Planetary Change

Reference17 articles.

1. Ananicheva MD, Krenke AN (2005) Evolution of climatic snow line and equilibrium line altitudes—North-Eastern Siberia Mountains in the 20th century. In: Ice and climate news, The WCRP climate and cryosphere newsletter. vol 6, pp 1–6

2. Ananicheva MD, Krenke AN (2007) Mountain glaciation (by the example of Northeastern Siberia and Kamchatka) in the chapter “Glaciation and snow cover in North Eurasia in immediate future. In: Kotlyakov VM (ed) Glaciation in North Eurasia in the recent past and immediate future. Moscow, “Nauka”, pp 277–293

3. Ananicheva MD, Krenke AN, Barry RG (2010) The Northeast Asia mountain glaciers in the near future by AOGCM scenarios. Cryosphere 4:435–445

4. Atlas of climatic characteristics of temperature and wind in middle stratosphere of the Northern Hemisphere Red (1982). In: Guterman IG, Ignatyushina EN (eds) Research institute of hydrometeorological information, Would data center. Moscow, Hydromentizdat. p 155. (in Russian)

5. Bogdanova AG (1976) Method of for calculation of solid and mixed precipitation proportion in their monthly standart. Data Glaciol Stud 26:202–207 (in Russian, summary and figures captions in English)

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