Simulated high-latitude soil thermal dynamics during the past 4 decades

Simulated high-latitude soil thermal dynamics during the past 4 decades

Soil temperature (<i>T</i><sub>s</sub>) change is a key indicator of the dynamics of permafrost. On seasonal and interannual timescales, the variability of <i>T</i><sub>s</sub> determines the active-layer depth, which regulates hydrological soil proper...

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Bibliographic Details
Main Authors: S. Peng, P. Ciais, G. Krinner, T. Wang, I. Gouttevin, A. D. McGuire, D. Lawrence, E. Burke, X. Chen, B. Decharme, C. Koven, A. MacDougall, A. Rinke, K. Saito, W. Zhang, R. Alkama, T. J. Bohn, C. Delire, T. Hajima, D. Ji, D. P. Lettenmaier, P. A. Miller, J. C. Moore, B. Smith, T. Sueyoshi
Format: Article
Language:English
Published: Copernicus Publications 2016-01-01
Series:The Cryosphere
Online Access:http://www.the-cryosphere.net/10/179/2016/tc-10-179-2016.pdf

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http://www.the-cryosphere.net/10/179/2016/tc-10-179-2016.pdf

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