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Volumn 375, Issue 3-4, 2009, Pages 438-449

The influence of freeze-thaw cycles of active soil layer on surface runoff in a permafrost watershed

Author keywords

Active soil freeze thaw depth; Permafrost watershed; Qinghai Tibet plateau; Runoff characteristics

Indexed keywords

ACTIVE LAYER; ACTIVE SOIL FREEZE-THAW DEPTH; ACTIVE SOILS; FREEZE-THAW; FREEZE-THAW CYCLES; FREEZE-THAW PROCESS; FREEZING AND THAWING; HYDROLOGICAL PROCESS; IN-CONTROL; INFLUENCE SURFACES; MAIN CHARACTERISTICS; PERMAFROST REGION; PRIMARY FACTORS; QINGHAI-TIBET PLATEAU; RECESSION PERIOD; RUNOFF CHARACTERISTICS; RUNOFF COEFFICIENTS; SEASONAL VARIATION; SOIL WATER DYNAMICS; SPRING FLOODS; STATISTICAL REGRESSION METHOD; SUMMER FLOODS; SURFACE RUNOFFS; UPPER LAYER; VEGETATION COVER; WATER BUDGET; WATER CYCLE;

EID: 69349088809     PISSN: 00221694     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jhydrol.2009.06.046     Document Type: Article
Times cited : (199)

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