Response of a stably stratified atmosphere to large-scale diabatic forcing with applications to wind patters in Brazil and the Sahel

Journal of Geophysical Research Atmospheres

Volumn 101, Issue D3, 1996, Pages 7049-7073

  Wang, T A ^a   Lin, Y L ^a   Semazzi, H F M ^a   Janowitz, G S ^a  

^a NORTH CAROLINA STATE UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ATMOSPHERIC MODELLING; DIABATIC FORCING; RAINFALL ANOMALY; SEA SURFACE TEMPERATURE; STRATIFIED ATMOSPHERE;

AFRICA, SAHEL; BRAZIL;

EID: 0030456144     PISSN: 01480227     EISSN: None     Source Type: Journal    
DOI: 10.1029/95JD03761     Document Type: Article

References (6)

1. Asselin, R., Frequency filter for time integrations, Mon. Weather Rev., 100, 487-490, 1972.
2. Bjerknes, J., A possible response of the atmospheric Hadley circulation to equatorial anomalies of ocean temperature, Tellus, IS, 820-829, 1966.
3. Chervin, R. M., and S. H. Schneider, On determining the statistical significance of climate experiments with general circulation models, J. Atmos. Sci, 33, 405-412, 1976.
4. Druyan, L., GCM studies of the African summer monsoon, Clim. Dyn., 2, 117-126, 1987.
5. Druyan, L., Advances in the study of Sub-Saharan drought. Int. J. Clim., 9, 77-90, 1989.
6. Egger, J., On the linear theory of the atmospheric response to sea surface temperature anomalies, J. Atmos. Sci., 34, 603-614, 1977.