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EFFECTIVE STRATIFICATION FOR PLUME RISE AND BOUNDARY LAYER GROWTH COMPUTATIONSKERMAN BR.1983; ATMOSPHERIC ENVIRONMENT; ISSN 0004-6981; GBR; DA. 1983; VOL. 17; NO 2; PP. 235-238; BIBL. 4 REF.Article

A PROPOSED METHOD FOR ESTIMATING DIFFUSION IN A FREELY CONVECTIVE BOUNDARY LAYER BY ACOUSTIC SOUNDINGKERMAN BR.1978; ATMOSPH. ENVIRONMENT; GBR; DA. 1978; VOL. 12; NO 9; PP. 1827-1838; BIBL. 40 REF.Article

AN ENERGY BUDGET FOR WAVES AND TURBULENCE WITHIN AN INVERSION.KERMAN BR.1974; BOUNDARY-LAYER METEOROL.; NETHERL.; DA. 1974; VOL. 6; NO 3-4; PP. 443-458; BIBL. 25 REF.Article

A SIMILARITY MODEL OF SHORELINE FUMIGATIONKERMAN BR.1982; ATMOS. ENVIRON.; ISSN 0004-6981; GBR; DA. 1982; VOL. 16; NO 3; PP. 467-477; BIBL. 33 REF.Article

A SIMILARITY MODEL FOR MAXIMUM GROUND-LEVEL CONCENTRATION IN A FREELY CONVECTIVE ATMOSPHERIC BOUNDARY LAYERKERMAN BR.1979; BOUNDARY-LAYER METEOROL.; NLD; DA. 1979; VOL. 16; NO 4; PP. 395-408; BIBL. 19 REF.Article

THE DISCRETE TURBULENT GUST CONCEPT.KERMAN BR.1977; BOUNDARY-LAYER METEOROL.; NETHERL.; DA. 1977; VOL. 12; NO 4; PP. 425-437; BIBL. 16 REF.Article

A NOTE ON THE INTERPRETATION OF ACOUSTIC SOUNDER RETURNS.KERMAN BR.1976; BOUNDARY-LAYER METEOROL.; NETHERL.; DA. 1976; VOL. 10; NO 3; PP. 303-310; BIBL. 10 REF.Article

ON THE CONVERSION OF ENERGY AND ENSTROPHY ON THE MESO-SCALE.KERMAN BR.sdIN: SYMP. ATMOS. DIFFUS. AIR POLLUT. PREPR.; SANTA BARBARA, CALIF.; 1974; BOSTON, MASS.; AM. METEOROL. SOC.; DA. S.D.; PP. 41-48; BIBL. 21 REF.Conference Paper

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