Sensible and latent heat flux response to diurnal variation in soil surface temperature and moisture under different freeze/thaw soil conditions in the seasonal frozen soil region of the central Tibetan Plateau

Environmental Earth Sciences

Volumn 63, Issue 1, 2011, Pages 97-107

  Guo, Donglin ^a,b,c   Yang, Meixue ^b   Wang, Huijun ^a  

^a INSTITUTE OF ATMOSPHERIC PHYSICS   (China)

^b Chinese Academy of Sciences   (China)

^c UNIVERSITY OF CHINESE ACADEMY OF SCIENCES   (China)

Author keywords

Freeze thaw; Latent heat flux; Soil water; Tibetan Plateau

Indexed keywords

AIR TEMPERATURE CHANGES; CENTRAL TIBETAN PLATEAU; DIURNAL RANGES; DIURNAL VARIATION; FREEZE/THAW; FREEZING AND THAWING; SENSIBLE AND LATENT HEAT FLUXES; SOIL CONDITIONS; SOIL SURFACE TEMPERATURES; SOIL TEMPERATURE; SOIL WATER; SOIL WATER CONTENT; TEMPORAL CHANGE; TIBETAN PLATEAU;

ATMOSPHERIC TEMPERATURE; FREEZING; FROZEN SOILS; LATENT HEAT; SOIL MOISTURE; SOLAR RADIATION; SUN; SURFACE PROPERTIES; THAWING; WATER CONTENT;

HEAT FLUX;

AIR TEMPERATURE; DIURNAL VARIATION; FREEZE-THAW CYCLE; FREEZING; LATENT HEAT FLUX; MOISTURE; NUMERICAL MODEL; SEASONAL VARIATION; SENSIBLE HEAT FLUX; SOIL DEPTH; SOIL TEMPERATURE; SOIL TYPE; SOIL WATER; SOLAR RADIATION; SURFACE TEMPERATURE;

CHINA; QINGHAI-XIZANG PLATEAU;

EID: 79954415978     PISSN: 18666280     EISSN: 18666299     Source Type: Journal    
DOI: 10.1007/s12665-010-0672-6     Document Type: Article

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