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WARM RAIN UNDER TRADE WIND INVERSION IN HAWAII.TAKAHASHI T.1976; IN: INT. CONF. CLOUD PHYS. PREPR.; BOULDER, COLO.; 1976; BOSTON, MASS.; AM. METEOROL. SOC.; DA. 1976; PP. 532-536; BIBL. 7 REF.Conference Paper

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NUMERICAL MODELING OF RAIN FORMATION IN A WARM CUMULUS.SERGUEYEV BN.1976; IN: INT. CONF. CLOUD PHYS. PREPR.; BOULDER, COLO.; 1976; BOSTON, MASS.; AM. METEOROL. SOC.; DA. 1976; PP. 528-531; BIBL. 14 REF.Conference Paper

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WARM CLOUD ELECTRICITY IN A SHALLOW AXISYMMETRIC CLOUD MODELTAKAHASHI T.1979; J. ATMOSPH. SCI.; AUS; DA. 1979; VOL. 36; NO 11; PP. 2236-2258; BIBL. 44 REF.Article

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ELECTRICAL AND MICROPHYSICAL MEASUREMENTS IN WARM CUMULUS CLOUDS BEFORE AND AFTER SEEDING.RAMACHANDRA MURTY AS; SELVAM AM; VIJAYAKUMAR R et al.1976; J. APPL. METEOROL.; U.S.A.; DA. 1976; VOL. 15; NO 12; PP. 1295-1301; BIBL. 14 REF.Article

ON THE DECREASE OF DROPLET NUMBER WITH HEIGHT IN THE EARLY STAGE OF GROWTH IN A CONVECTIVE WARM CLOUD.TAKAHASHI Y.1976; IN: INT. CONF. CLOUD PHYS. PREPR.; BOULDER, COLO.; 1976; BOSTON, MASS.; AM. METEOROL. SOC.; DA. 1976; PP. 37-40; BIBL. 9 REF.Conference Paper

ROLE DES AGENTS TENSIOACTIFS DANS LA CONDENSATION STOCHASTIQUEMERKULOVICH VM; STEPANOV AS.1980; IZVEST. AKAD. NAUK S.S.S.R., FIZ. ATMOSF. OKEANA; SUN; DA. 1980; VOL. 16; NO 9; PP. 981-985; BIBL. 7 REF.Article

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