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

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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Bibliographic Details
Main Authors: 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
Format: Article
Language:English
Published: IOP Publishing 2018-01-01
Series:Environmental Research Letters
Subjects:
stable water isotopes
Western Siberia Lowlands
mean transit time
hydrological connectivity
permafrost
Online Access:https://doi.org/10.1088/1748-9326/aaa4fe

Internet

https://doi.org/10.1088/1748-9326/aaa4fe

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