Spring warming in Yukon mountains is not amplified by the snow albedo feedback

Decreasing spring snow cover may amplify Arctic warming through the snow albedo feedback. To examine the impact of snowmelt on increasing temperature we used a 5,000 m elevation gradient in Yukon, Canada, extending from valley-bottom conifer forests, through middle elevation tundra, to high elevatio...

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Detalles Bibliográficos
Autores principales: Williamson, Scott N., Anslow, Faron S., Clarke, Garry K. C., Gamon, John A., Jarosch, Alexander H., Hik, David S.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5998050/
https://www.ncbi.nlm.nih.gov/pubmed/29899422
http://dx.doi.org/10.1038/s41598-018-27348-7

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5998050/
https://www.ncbi.nlm.nih.gov/pubmed/29899422
http://dx.doi.org/10.1038/s41598-018-27348-7

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