Variability in Greenhouse Gas Emissions from Permafrost Thaw Ponds

Arctic climate change is leading to accelerated melting of permafrost and the mobilization of soil organic carbon pools that have accumulated over thousands of years. Photochemical and microbial transformation will liberate a fraction of this carbon to the atmosphere in the form of CO₂ and CH₄. We q...

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Vydané v:	Limnology and oceanography Ročník 55; číslo 1; s. 115 - 133
Hlavní autori:	Laurion, Isabelle, Vincent, Warwick F., MacIntyre, Sally, Retamal, Leira, Dupont, Christiane, Francus, Pierre, Pienitz, Reinhard
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	Waco, TX American Society of Limnology and Oceanography 01.01.2010
Predmet:	Earth sciences Earth, ocean, space Engineering and environment geology. Geothermics Exact sciences and technology Marine and continental quaternary Pollution, environment geology Soils Surficial geology Canada Quebec Eastern Canada PN, Arctic atmosphere ponds carbon dioxide models bacteria thermal stratification air-water interface concentration covariance North America greenhouse gas optical properties prokaryotes depth permafrost photochemistry winds methane soils organic carbon climate change
ISSN:	0024-3590, 1939-5590
On-line prístup:	Získať plný text
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