On the variability of cold region flooding

On the variability of cold region flooding •Trends in hydrological signatures show variability in cold region catchments.•Trends indicate shift from snowmelt-dominated to rainfall-dominated flow regime.•Variability at catchment scale can be explained by catchments’ physical properties.•Results depend highly on the record period chosen.•Spatial variability in streamflow reflects the influence of permafrost. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Journal of Hydrology Elsevier

On the variability of cold region flooding

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Publisher
Elsevier
Copyright
Copyright © 2016 Elsevier B.V.
ISSN
0022-1694
eISSN
1879-2707
D.O.I.
10.1016/j.jhydrol.2016.01.055
Publisher site
See Article on Publisher Site

Abstract

•Trends in hydrological signatures show variability in cold region catchments.•Trends indicate shift from snowmelt-dominated to rainfall-dominated flow regime.•Variability at catchment scale can be explained by catchments’ physical properties.•Results depend highly on the record period chosen.•Spatial variability in streamflow reflects the influence of permafrost.

Journal

Journal of HydrologyElsevier

Published: Mar 1, 2016

References

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