Thawing of massive ground ice in mega slumps drives increases in stream sediment and solute flux across a range of watershed scales

Journal of Geophysical Research: Earth Surface

Volumn 118, Issue 2, 2013, Pages 681-692

  Kokelj, S V ^a   Lacelle, D ^b   Lantz, T C ^c   Tunnicliffe, J ^d   Malone, L ^b   Clark, I D ^b   Chin, K S ^a  

^a Cumulative Impact Monitoring Program Northwest Territories Geoscience Office Aboriginal Affairs and Northern Development Canada ^*  (Canada)

^b UNIVERSITY OF OTTAWA   (Canada)

^c UNIVERSITY OF VICTORIA   (Canada)

^d CARLETON UNIVERSITY   (Canada)

Author keywords

Environmental change; Fluvial regime; Geochemistry; Hydrology; Thaw slump; Thermokarst

Indexed keywords

CONCENTRATION (COMPOSITION); DEBRIS FLOW; ENVIRONMENTAL CHANGE; FLUVIAL DEPOSIT; GEOCHEMISTRY; HYDROLOGY; PERMAFROST; SOLUTE; SUSPENDED SEDIMENT; THAWING; THERMOKARST; WATERSHED;

CANADA; MACKENZIE RIVER [NORTHWEST TERRITORIES]; NORTHWEST TERRITORIES; ONTARIO [CANADA]; PEEL;

EID: 84880694884     PISSN: None     EISSN: 21699011     Source Type: Journal    
DOI: 10.1002/jgrf.20063     Document Type: Article

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