Convective heat transfer of spring meltwater accelerates active layer phase change in Tibet permafrost areas
Abstract ∘ C higher, respectively, than under the scenarios ignoring CHT. The ending dates of the zero-curtain effect were substantially advanced when CHT was considered due to its heating effect. However, the opposite cooling effect was also present but not as frequently as heating due to upward liquid fluxes and thermal differences between soil layers. In some periods, the advection flow from the cold layer reduced the shallow and intermediate depth temperatures by an average of about - - ∘ C, respectively. The overall annual effect of CHT due to liquid flux is to increase soil temperature in the active layer and favor thawing of frozen ground at the study site.
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Convective heat transfer of spring meltwater accelerates active layer phase change in Tibet permafrost areas ; volume:16 ; number:3 ; year:2022 ; pages:825-849 ; extent:25
The Cryosphere ; 16, Heft 3 (2022), 825-849 (gesamt 25)
- Creator
- DOI
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10.5194/tc-16-825-2022
- URN
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urn:nbn:de:101:1-2022031704302254313943
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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15.08.2025, 7:32 AM CEST
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Associated
- Zhao, Yi
- Nan, Zhuotong
- Ji, Hailong
- Zhao, Lin
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