Why is longwave cloud feedback positive?

Journal of Geophysical Research Atmospheres

Volumn 115, Issue 16, 2010, Pages

  Zelinka, Mark D ^a   Hartmann, Dennis L ^a  

^a UNIVERSITY OF WASHINGTON   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CLIMATE MODELS; CLOUDS; FEEDBACK; TOOLS; TROPOSPHERE;

ALTITUDE RANGE; CLIMATE WARMS; CLOUD TEMPERATURE; FIXED TEMPERATURE; GLOBAL CLIMATE MODEL; HARTMANN; INTERGOVERNMENTAL PANEL ON CLIMATE CHANGES; LARGE PARTS; LONG WAVES; MASS BALANCE; POSITIVE FEEDBACK; RADIATIVE COOLING; WARMING CLIMATE;

CLIMATE CHANGE;

ATMOSPHERIC CONVECTION; CLEAR SKY; CLIMATE CHANGE; CLIMATE MODELING; CLOUD; CLOUD RADIATIVE FORCING; CONVERGENCE; GLOBAL CLIMATE; MAGNITUDE; MASS BALANCE; TROPICAL ENVIRONMENT; TROPOSPHERE; WARMING;

EID: 77956338119     PISSN: 01480227     EISSN: None     Source Type: Journal    
DOI: 10.1029/2010JD013817     Document Type: Article

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