Permafrost and lakes control river isotope composition across a boreal Arctic transect in the Western Siberian lowlands

The Western Siberian Lowlands (WSL) store large quantities of organic carbon that will be exposed and mobilized by the thawing of permafrost. The fate of mobilized carbon, however, is not well understood, partly because of inadequate knowledge of hydrological controls in the region which has a vast...

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Hlavní autoři:	P Ala-aho, C Soulsby, O S Pokrovsky, S N Kirpotin, J Karlsson, S Serikova, R Manasypov, A Lim, I Krickov, L G Kolesnichenko, H Laudon, D Tetzlaff
Médium:	Artigo
Jazyk:	Inglês
Vydáno:	IOP Publishing 2018-01-01
Edice:	Environmental Research Letters
Témata:	stable water isotopes Western Siberia Lowlands mean transit time hydrological connectivity permafrost
On-line přístup:	https://doi.org/10.1088/1748-9326/aaa4fe
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