Characteristics and Significance of the Transition Zone in Drained Thaw-Lake Basins of the Arctic Coastal Plain, Alaska

In the three-component conceptual model of arctic soils, the transition zone is recognized as a layer intermediate between the seasonally thawed active layer above and the stable permafrost below. Although typically frozen and therefore part of the near-surface permafrost, the transition zone episod...

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Bibliographic Details
Published in:ARCTIC
Main Authors: Bockheim, J.G., Hinkel, K.M.
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 2010
Subjects:
Ice
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/63515