Carbon release through abrupt permafrost thaw

The permafrost zone is expected to be a substantial carbon source to the atmosphere, yet large-scale models currently only simulate gradual changes in seasonally thawed soil. Abrupt thaw will probably occur in <20% of the permafrost zone but could affect half of permafrost carbon through collapsi...

Celý popis

Uložené v:

Podrobná bibliografia
Vydané v:	Nature geoscience Ročník 13; číslo 2; s. 138 - 143
Hlavní autori:	Turetsky Merritt R, Abbott, Benjamin W, Jones, Miriam C, Walter, Anthony Katey, Olefeldt, David, Schuur, Edward A, Grosse Guido, Kuhry, Peter, Hugelius Gustaf, Koven, Charles, Lawrence, David M, Gibson, Carolyn, Sannel A Britta K, David, McGuire A
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	London Nature Publishing Group 01.02.2020
Predmet:	Atmospheric models Carbon Carbon emissions Carbon sinks Carbon sources Carbon uptake Climate change Climate models Computer simulation Emissions Forecasting Lakes Landslides Large-scale models Permafrost Permafrost thaws Regrowth Scale models Soil Soil stabilization Soils Thawing Uptake Vegetation Vegetation regrowth Wetlands
ISSN:	1752-0894, 1752-0908
On-line prístup:	Získať plný text
Tagy:	Pridať tag Žiadne tagy, Buďte prvý, kto otaguje tento záznam!

Buďte prvý, kto okomentuje tento záznam!