Snowmelt runoff from northern alpine tundra hillslopes: major processes and methods of simulation

In northern alpine tundra, large slope gradients, late-lying snow drifts and shallow soils overlying impermeable substrates all contribute to large hillslope runoff volumes during the spring freshet. Understanding the processes and pathways of hillslope runoff in this environment is, therefore, crit...

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Bibliographic Details
Published in:Hydrology and Earth System Sciences
Main Authors: Quinton, W. L., Carey, S. K., Goeller, N. T.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2004
Subjects:
Online Access:https://doi.org/10.5194/hess-8-877-2004
https://noa.gwlb.de/receive/cop_mods_00034617
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00034571/hess-8-877-2004.pdf
https://hess.copernicus.org/articles/8/877/2004/hess-8-877-2004.pdf