dot
Detailansicht
Katalogkarte GBA
Katalogkarte ISBD
Suche präzisieren
Drucken
Download RIS
Hier klicken, um den Treffer aus der Auswahl zu entfernen
Titel Surface water types in the Western Canadian Arctic: geochemical evolution and aquatic carbon transport
VerfasserIn Joshua F. Dean, Mike F. Billett, Kerry J. Dinsmore, Jason S. Lessels, Lorna Street, Ian Washbourne, Jens-Arne Subke, Doerthe Tetzlaff, Robert Baxter, Philip A. Wookey
Konferenz EGU General Assembly 2015
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 17 (2015)
Datensatznummer 250113256
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2015-13454.pdf
 
Zusammenfassung
Arctic surface waters are a substantial conduit for terrestrial C flow as well as a potential source of GHGs to the atmosphere – a significant positive feedback to global climate warming and a key component of the net ecosystem carbon balance in permafrost regions. As temperatures rise in the Arctic, permafrost thaw deepens releasing C from the landscape into the aquatic system making streams and lakes increasingly important conduits and reactors of both allochthonous and autochthonous C. The HYDRA project (“Permafrost catchments in transition: hydrological controls on carbon cycling and greenhouse gas budgets”), aims to quantify the assimilation of C and the controls of C movement between the plant-soil-water-atmosphere continuum. The specific aspect of the project presented here considers the different aquatic pathways in warming Arctic permafrost catchments, and the potential role that they play in GHG emissions and aquatic C cycling. This study presents the surface water geochemistry of Siksik Creek, a small (