Fast response of cold ice-rich permafrost in northeast Siberia to a warming climate
Siberian Arctic permafrost contains vast stores of carbon, the fate of which is dependent on the climate. Here the authors use models of future scenarios to show that under the direst climate changes up to 2/3 of the stored organic carbon could thaw.
Guardado en:
Autores principales: | Jan Nitzbon, Sebastian Westermann, Moritz Langer, Léo C. P. Martin, Jens Strauss, Sebastian Laboor, Julia Boike |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2020
|
Materias: | |
Acceso en línea: | https://doaj.org/article/66dd5105f36b4e719a9be40adaddbf9a |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
-
Permafrost is warming at a global scale
por: Boris K. Biskaborn, et al.
Publicado: (2019) -
The Ice-Rich Permafrost Sequences as a Paleoenvironmental Archive for the Kara Sea Region (Western Arctic)
por: I. D. Streletskaya, et al.
Publicado: (2021) -
Reconstructing Permafrost Sedimentological Characteristics and Post-depositional Processes of the Yedoma Stratotype Duvanny Yar, Siberia
por: Denis Shmelev, et al.
Publicado: (2021) -
Effect of Permafrost Thawing on Discharge of the Kolyma River, Northeastern Siberia
por: Kazuyoshi Suzuki, et al.
Publicado: (2021) -
Icings and groundwater conditions in permafrost catchments of northwestern Canada
por: Hugo Crites, et al.
Publicado: (2020)