Alpine permafrost could account for a quarter of thawed carbon based on Plio-Pleistocene paleoclimate analogue

Estimates of the permafrost-climate feedback vary in magnitude and sign, partly because permafrost carbon stability in warmer-than-present conditions is not well constrained. Here we use a Plio-Pleistocene lacustrine reconstruction of mean annual air temperature (MAAT) from the Tibetan Plateau, the...

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Detalles Bibliográficos
Autores principales: Cheng, Feng, Garzione, Carmala, Li, Xiangzhong, Salzmann, Ulrich, Schwarz, Florian, Haywood, Alan M., Tindall, Julia, Nie, Junsheng, Li, Lin, Wang, Lin, Abbott, Benjamin W., Elliott, Ben, Liu, Weiguo, Upadhyay, Deepshikha, Arnold, Alexandrea, Tripati, Aradhna
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8921200/
https://www.ncbi.nlm.nih.gov/pubmed/35288572
http://dx.doi.org/10.1038/s41467-022-29011-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8921200/
https://www.ncbi.nlm.nih.gov/pubmed/35288572
http://dx.doi.org/10.1038/s41467-022-29011-2

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