Ground Thawing is a geophysical process denoting the phase transition of pore ice in frozen soil to liquid water, distinguished by the reduction of negative pore pressures and the consequent loss of soil strength and stability within periglacial and seasonally frozen environments.
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Ground Thaw
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204
Permafrost temperature records: Indicators of climate change
V. E. Romanovsky, M M Burgess, Sharon L. Smith et al. · Eos · 2002 · 203 citations · Full text
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- SSSally Shoop
Cold Regions Research and Engineering Laboratory, United States
3 publications · 59 citations
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Chinese Academy of Sciences
Beijing, China
26 h-index
127 publications
8.6K citations
Northwest Institute of Eco-Environment and Resources
Lanzhou, China
14 h-index
53 publications
3K citations
University of Alaska Fairbanks
Fairbanks, United States
10 h-index
20 publications
3.1K citations
University of Chinese Academy of Sciences
Beijing, China
9 h-index
26 publications
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Lanzhou University
Lanzhou, China
6 h-index
13 publications
608 citations
Tsinghua University
Beijing, China
4 h-index
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Hokkaido University
Sapporo, Japan
4 h-index
8 publications
378 citations
Southwest Jiaotong University
Chengdu, China
3 h-index
9 publications
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- Cold Regions Science and Technology
17 publications · 843 citations
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- Permafrost and Periglacial Processes
9 publications · 503 citations
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- Arctic and Alpine Research
8 publications · 221 citations
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- Geophysical Research Letters
6 publications · 698 citations
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- Geografiska Annaler Series A Physical Geography
6 publications · 98 citations
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