Decade of experimental permafrost thaw reduces turnover of young carbon and increases losses of old carbon, without affecting the net carbon balance

Thicker snowpacks and their insulation effects cause winter‐warming and invoke thaw of permafrost ecosystems. Temperature‐dependent decomposition of previously frozen carbon (C) is currently considered one of the strongest feedbacks between the Arctic and the climate system, but the direction and ma...

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Vydáno v:	Global change biology Ročník 26; číslo 10; s. 5886 - 5898
Hlavní autoři:	Olid, Carolina, Klaminder, Jonatan, Monteux, Sylvain, Johansson, Margareta, Dorrepaal, Ellen
Médium:	Journal Article
Jazyk:	angličtina
Vydáno:	England Blackwell Publishing Ltd 01.10.2020
Témata:	age-depth modelling Arctic region Arctic Regions Biological Sciences Bryophytes Carbon carbon accumulation carbon cycle carbon sequestration carbon sinks climate climate change Climate Research Climate Science Climate system Decomposition Deep layer Earth and Related Environmental Sciences Ecology Ecosystem Ekologi Fluxes Geovetenskap och relaterad miljövetenskap global change Growth models Insulating materials Insulation Klimatforskning Klimatvetenskap Leaching Lead isotopes Melting Natural Sciences Naturgeografi Naturvetenskap net ecosystem production Peat peat dating Permafrost permafrost thawing Permafrost thaws Physical Geography Primary production primary productivity production snow addition Snowpack Soil Soil layers Storage subsidence Temperature dependence Thawing Waterlogging Winter winter-warming Arctic Regions Arctic region permafrost thawing peat dating production snow addition decomposition carbon cycle winter-warming carbon accumulation age-depth modelling climate change
ISSN:	1354-1013, 1365-2486, 1365-2486
On-line přístup:	Získat plný text
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