Threshold sensitivity of shallow Arctic lakes and sublake permafrost to changing winter climate

Abstract Interactions and feedbacks between abundant surface waters and permafrost fundamentally shape lowland Arctic landscapes. Sublake permafrost is maintained when the maximum ice thickness (MIT) exceeds lake depth and mean annual bed temperatures (MABTs) remain below freezing. However, declinin...

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Detalles Bibliográficos

Autores principales:	Christopher D. Arp, Benjamin M. Jones, Guido Grosse, Allen C. Bondurant, Vladimir E. Romanovsky, Kenneth M. Hinkel, Andrew D. Parsekian
Formato:	Artigo
Lenguaje:	Inglês
Publicado:	Wiley 2016-06-01
Colección:	Geophysical Research Letters
Materias:	thermokarst lakes permafrost lake ice taliks climate change
Acceso en línea:	https://doi.org/10.1002/2016GL068506
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