Cargando…
Extremely wet summer events enhance permafrost thaw for multiple years in Siberian tundra
Permafrost thaw can accelerate climate warming by releasing carbon from previously frozen soil in the form of greenhouse gases. Rainfall extremes have been proposed to increase permafrost thaw, but the magnitude and duration of this effect are poorly understood. Here we present empirical evidence sh...
Autores principales: | Magnússon, Rúna Í., Hamm, Alexandra, Karsanaev, Sergey V., Limpens, Juul, Kleijn, David, Frampton, Andrew, Maximov, Trofim C., Heijmans, Monique M. P. D. |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2022
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8943195/ https://www.ncbi.nlm.nih.gov/pubmed/35322039 http://dx.doi.org/10.1038/s41467-022-29248-x |
Ejemplares similares
-
Design of the tundra rainfall experiment (TRainEx) to simulate future summer precipitation scenarios
por: Grysko, Raleigh, et al.
Publicado: (2021) -
Summer thaw duration is a strong predictor of the soil microbiome and its response to permafrost thaw in arctic tundra
por: Romanowicz, Karl J., et al.
Publicado: (2022) -
Drying of tundra landscapes will limit subsidence-induced acceleration of permafrost thaw
por: Painter, Scott L., et al.
Publicado: (2023) -
Continentality determines warming or cooling impact of heavy rainfall events on permafrost
por: Hamm, Alexandra, et al.
Publicado: (2023) -
Isotopic compositions of ground ice in near-surface permafrost in relation to vegetation and microtopography at the Taiga–Tundra boundary in the Indigirka River lowlands, northeastern Siberia
por: Takano, Shinya, et al.
Publicado: (2019)