Influences and interactions of inundation, peat, and snow on active layer thickness

Abstract Active layer thickness (ALT), the uppermost layer of soil that thaws on an annual basis, is a direct control on the amount of organic carbon potentially available for decomposition and release to the atmosphere as carbon‐rich Arctic permafrost soils thaw in a warming climate. We investigate...

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Principais autores:	Adam L. Atchley, Ethan T. Coon, Scott L. Painter, Dylan R. Harp, Cathy J. Wilson
Formato:	Artigo
Idioma:	Inglês
Publicado em:	Wiley 2016-05-01
coleção:	Geophysical Research Letters
Assuntos:	active layer thickness thermal hydrology inundation and soil moisture ALT sensitivity organic soil thermal properties snow depth
Acesso em linha:	https://doi.org/10.1002/2016GL068550
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