Interactions between freeze–thaw actions, wind erosion desertification, and permafrost in the Qinghai–Tibet Plateau-Reference-Cited by-同舟云学术

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Interactions between freeze–thaw actions, wind erosion desertification, and permafrost in the Qinghai–Tibet Plateau

Published:2016-10-01 Issue:2 Volume:85 Page:829-850
ISSN:0921-030X
Container-title:Natural Hazards
language:en
Short-container-title:Nat Hazards

Author:

Xie Shengbo,Qu Jianjun,Xu Xiangtian,Pang Yingjun

Funder

National Natural Science Foundation of China (CN)

China Postdoctoral Science Foundation

Science and Technology Program of Gansu Province

Special Fund for Forest Scientific Research in the Public Welfare

Publisher

Springer Science and Business Media LLC

Subject

Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Water Science and Technology

Link

http://link.springer.com/content/pdf/10.1007/s11069-016-2606-4.pdf

Reference65 articles.

1. Bai W, Wang GX, Liu GS (2012) Effects of elevated air temperatures on soil thermal and hydrologic processes in the active layer in an alpine meadow ecosystem of the Qinghai–Tibet Plateau. J Mt Sci-Engl 9(2):243–255

2. Bhumralkar CM (1975) Numerical experiments on the computation of ground surface temperature in an atmospheric general circulation model. J Appl Meteorol 14:1246–1258

3. Chang J, Wan GX, Gao YH et al (2014) The influence of seasonal snow on soil thermal and water dynamics under different vegetation covers in a permafrost region. J Mt Sci-Engl 11(3):727–745

4. Chepil WS (1942) Relation of wind erosion to water stable and dry cold structure of soil. Soil Sci 55(2):275–287

5. Duan AM, Wu GX, Zhang Q et al (2006) New proofs of the recent climate warming over the Tibetan Plateau as a result of the increasing greenhouse gases emissions. Chin Sci Bull 51:1396–1400

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