An Extreme Sediment Transfer Event in a Canadian High Arctic Stream.

Two large suspended sediment concentration (SSC) pulses were recorded in 1998 in a small snowmelt-fed stream on Ellesmere Island in the Canadian High Arctic. The largest pulse occurred from 7 to 8 July, when 32% of the monitored seasonal sediment transport occurred in only four hours. SSC reached 83...

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Bibliographic Details
Main Authors: Lewis, Ted, Braun, Carsten, Hardy, Douglas R., Francus, Pierre, Bradley, Raymond S.
Format: Article in Journal/Newspaper
Language:English
Published: 2005
Subjects:
sédiments
cours d'eau
Canada
Arctique
Arctic
Ellesmere Island
Antarctic and Alpine Research
Arctique*
Online Access:https://espace.inrs.ca/id/eprint/9576/
https://espace.inrs.ca/id/eprint/9576/1/P1352.pdf
https://doi.org/10.1657/1523-0430(2005)037[0477:AESTEI]2.0.CO;2
Description
Summary:Two large suspended sediment concentration (SSC) pulses were recorded in 1998 in a small snowmelt-fed stream on Ellesmere Island in the Canadian High Arctic. The largest pulse occurred from 7 to 8 July, when 32% of the monitored seasonal sediment transport occurred in only four hours. SSC reached 83,760 mg L⁻¹, exceeding all previously recorded values from high arctic glacially-fed and snowmelt-fed rivers by more than one order of magnitude. The event occurred after the majority of snow in the watershed had melted, and was preceded by a long period of relatively high air temperature, and a small rainfall event on 7 July. We consider the most likely cause of the event to be a rapid mass movement.

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