Quantifying Reach‐Average Effects of Hyporheic Exchange on Arctic River Temperatures in an Area of Continuous Permafrost

Hyporheic exchange has the potential to significantly influence river temperatures in regions of continuous permafrost under low‐flow conditions given the strong thermal gradients that exist in river bed sediments. However, there is limited understanding of the impacts of hyporheic exchange on Arcti...

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Veröffentlicht in:	Water resources research 2019-03, Vol.55 (3), p.1951-1971
Hauptverfasser:	King, Tyler V., Neilson, Bethany T.
Format:	Artikel
Sprache:	eng
Schlagworte:	Arctic observations Arctic river temperature Computer simulation Conduction Conduction heating Energy balance Fluvial sediments Ground temperatures Heat Heat exchange Heat flux Heat loss Heat transfer hyporheic exchange Hyporheic zone Hyporheic zones Mean daily temperatures Permafrost River beds River channels river temperature River temperatures Riverbeds Rivers Sediments Solutes Temperature Temperature effects Temperature range Tracers
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