Short‐term discharge and suspended sediment fluctuations in the proglacial Skeldal River, north‐east Greenland

Abstract The summer discharge pattern of the Skeldal River, which drains a 560 km 2 partly glacierized catchment in north‐east Greenland, is dominated by diurnal oscillations reflecting variations in the melt rate of snow and ice in the basin. Superimposed on this diurnal pattern are numerous short‐...

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Bibliographic Details
Published in:Hydrological Processes
Main Authors: Stott, T. A., Grove, J. R.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2001
Subjects:
Online Access:http://dx.doi.org/10.1002/hyp.156
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.156
https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.156