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• W2181334972 abstract "Upward migration of soil water and its eventual evaporation near the ground surface cools the active layer above permafrost during summer. The thermal magnitude of these effects was estimated using a numerical model based on conductive heat-transfer theory and incorporating fusion effects. The model utilizes precision measurements of soil temperature as initial and boundary conditions to simulate the evolution of the thermal profile over the annual cycle. The simulation indicates that upward water movement and near-surface evaporation cools the active layer several degrees during summer and depresses the mean annual ground temperature by about 0.4iC. Nonconductive cooling of the active layer also attenuates surface thermal variations and moderates the thermal signal that penetrates the upper permafrost. Because the ratio of the heat of evaporation to the heat of fusion is approximately seven, an increase in summer temperature may not cause dramatic permafrost degradation and surface subsidence at poorly drained sites." @default.
• W2181334972 created "2016-06-24" @default.
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• W2181334972 date "1998-01-01" @default.
• W2181334972 modified "2023-09-27" @default.
• W2181334972 title "ESTIMATING THE MAGNITUDE OF COUPLED-FLOW EFFECTS IN THE ACTIVE LAYER AND UPPER PERMAFROST, BARROW, ALASKA U.S.A." @default.
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• W2181334972 hasPublicationYear "1998" @default.
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