A New Method to Determine the Upper Boundary Condition for a Permafrost Thermal Model: An Example from the Qinghai-Tibet Plateau-Reference-Cited by-同舟云学术

A New Method to Determine the Upper Boundary Condition for a Permafrost Thermal Model: An Example from the Qinghai-Tibet Plateau

Published:2012-10 Issue:4 Volume:23 Page:301-311
ISSN:1045-6740
Container-title:Permafrost and Periglacial Processes
language:en
Short-container-title:Permafrost and Periglac. Process.

Author:

Zhang Mingyi¹²,Min Ki-Hong²³,Wu Qingbai¹,Zhang Jianming¹,Harbor Jon²

Affiliation:

1. State Key Laboratory of Frozen Soil Engineering, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences; Lanzhou Gansu China

2. Department of Earth, Atmospheric, and Planetary Sciences; Purdue University; West Lafayette IN USA

3. Center for Atmospheric Remote Sensing; Kyungpook National University; Daegu South Korea

Publisher

Wiley

Subject

Earth-Surface Processes

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/ppp.1755/fullpdf

Reference41 articles.

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3. Thawing index and freezing index on the embankment surface in permafrost regions;Cheng;Journal of Glaciology and Geocryology,2003

4. Comparison of the diurnal precipitation cycle in convection-resolving and non-convection-resolving mesoscale models;Clark;Monthly Weather Review,2007

5. Mean, interannual variability and trends in a regional climate change experiment over Europe. I. Present-day climate (1961-1990);Giorgi;Climate Dynamics,2004

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