AN ANNUAL ZONALLY AVERAGED GLOBAL CLIMATIC MODEL WITH DIFFUSE CLOUDINESS FEEDBACK.LEE PS; SNELL FM.1977; J. ATMOSPH. SCI.; U.S.A.; DA. 1977; VOL. 34; NO 6; PP. 847-852; BIBL. 8 REF.Article

AN ANNUAL ZONALLY AVERAGED HEMISPHERICAL CLIMATIC MODEL WITH DIFFUSE CLOUDINESS FEEDBACK.TEMKIN RL; SNELL FM.1976; J. ATMOSPH. SCI.; U.S.A.; DA. 1976; VOL. 33; NO 9; PP. 1671-1685; BIBL. 42 REF.Article

A DIFFUSE THIN CLOUD ATMOSPHERIC STRUCTURE AS A FEEDBACK MECHANISM IN GLOBAL CLIMATIC MODELING.WEARE BC; SNELL FM.1974; J. ATMOSPH. SCI.; U.S.A.; DA. 1974; VOL. 31; NO 7; PP. 1725-1734; BIBL. 32 REF.Article

FEEDBACK COUPLING OF ABSORBED SOLAR RADIATION BY THREE MODEL ATMOSPHERES WITH CLOUDS.TEMKIN RL; WEARE BC; SNELL FM et al.1975; J. ATMOSPH. SCI.; U.S.A.; DA. 1975; VOL. 32; NO 5; PP. 873-880; BIBL. 22 REF.Article

AEROSOL AND CLIMATE: SOME FURTHER CONSIDERATIONS.WEARE BC; TEMKIN RL; SNELL FM et al.1974; SCIENCE; U.S.A.; DA. 1974; VOL. 186; NO 4166; PP. 827-828; BIBL. 9 REF.Article

COMMENTS ON "A DIFFUSE THIN CLOUD ATMOSPHERIC STRUCTURE AS A FEEDBACK MECHANISM IN GLOBAL CLIMATIC MODELING".HENDERSON SELLERS A; HENDERSON SELLERS B; WEARE BC et al.1975; J. ATMOSPH. SCI.; U.S.A.; DA. 1975; VOL. 32; NO 12; PP. 2358-2363; BIBL. 14 REF.Article