Permafrost Thaw and Liberation of Inorganic Nitrogen in Eastern Siberia

The currently observed climate warming will lead to widespread degradation of near‐surface permafrost, which may release substantial amounts of inorganic nitrogen (N) into arctic ecosystems. We studied 11 soil profiles at three different sites in arctic eastern Siberia to assess the amount of inorga...

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Veröffentlicht in:	Permafrost and periglacial processes 2017-10, Vol.28 (4), p.605-618
Hauptverfasser:	Beermann, Fabian, Langer, Moritz, Wetterich, Sebastian, Strauss, Jens, Boike, Julia, Fiencke, Claudia, Schirrmeister, Lutz, Pfeiffer, Eva‐Maria, Kutzbach, Lars
Format:	Artikel
Sprache:	eng
Schlagworte:	Active layer Ammonium Ammonium compounds Arctic soils Carbon emissions Climate Climate change Ecosystems Environmental changes Global warming Nitrogen Permafrost Permafrost soils permafrost thaw Polar environments polygonal tundra Profiles Soil Soil analysis Soil profiles Soil properties Thickening Thickness
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