A complementary relationship evaporation model referring to the Granger model and the advection-aridity model

Hydrological Processes

Volumn 25, Issue 13, 2011, Pages 2094-2101

  Han, Songjun ^a,b,c   Hu, Heping ^a   Yang, Dawen ^a   Tian, Fuqiang ^a  

^a TSINGHUA UNIVERSITY   (China)

^b CHINA INSTITUTE OF WATER RESOURCES AND HYDROPOWER RESEARCH   (China)

^c National Center of Efficient Irrigation Engineering and Technology Research   (China)

Author keywords

Advection aridity model; Complementary relationship; Evaporation; Penman equation

Indexed keywords

ADVECTION-ARIDITY MODEL; ATMOSPHERIC CONDITIONS; COMPLEMENTARY RELATIONSHIP; DIMENSIONLESS VARIABLES; DRY CONDITION; EVAPORATION MODEL; LAND COVER; NEW MODEL; OBSERVED DATA; OPTIMIZED PARAMETER; PENMAN EQUATION; POTENTIAL EVAPORATION; SYSTEM BIAS;

ADVECTION; EVAPORATION; LANDFORMS;

PHASE TRANSITIONS;

ADVECTION; ARIDITY; EVAPORATION; NUMERICAL MODEL; PREDICTION;

EID: 79959262846     PISSN: 08856087     EISSN: 10991085     Source Type: Journal    
DOI: 10.1002/hyp.7960     Document Type: Article

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