Convective heat transfer of spring meltwater accelerates active layer phase change in Tibet permafrost areas
<p>Convective heat transfer (CHT) is one of the important processes that control the near-ground surface heat transfer in permafrost areas. However, this process has often not been considered in most permafrost studies, and its influence on freezing–thawing processes in the active layer lacks...
| Main Authors: | , , , |
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| 格式: | Article |
| 語言: | English |
| 出版: |
Copernicus Publications
2022-03-01
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| 叢編: | The Cryosphere |
| 在線閱讀: | https://tc.copernicus.org/articles/16/825/2022/tc-16-825-2022.pdf |