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WEAK ABSORPTION BY ATMOSPHERIC WATER VAPOUR IN THE VISIBLE AND NEAR-INFRA-RED SPECTRAL REGIONTOMASI C.1979; NUOVO CIMENTO, C; ITA; DA. 1979; VOL. 2; NO 5; PP. 511-526; ABS. ITA/RUS; BIBL. 21 REF.Article

PRECIPITABLE WATER VAPOR IN ATMOSPHERES CHARACTERIZED BY TEMPERATURE INVERSIONS.TOMASI C.1977; J. APPL. METEOROL.; U.S.A.; DA. 1977; VOL. 16; NO 3; PP. 237-243; BIBL. 14 REF.Article

DETERMINATION OF THE TOTAL PRECIPITABLE WATER BY VARYING THE INTERCEPT IN REITAN'S RELATIONSHIPTOMASI C.1981; J. APPL. METEOROL.; ISSN 0021-8952; USA; DA. 1981; VOL. 20; NO 9; PP. 1058-1069; BIBL. 17 REF.Article

NON-SELECTIVE ABSORPTION BY ATMOSPHERIC WATER VAPOUR AT VISIBLE AND NEAR INFRARED WAVE LENGTHSTOMASI C.1979; Q. J. R. METEOROL. SOC.; GBR; DA. 1979; VOL. 105; NO 446; PP. 1027-1040; BIBL. 2 P.Article

NON-SELECTIVE ABSORPTION BY ATMOSPHERIC WATER VAPOUR AT VISIBLE AND NEAR INFRARED WAVELENGTHSTOMASI C.1979; QUART. J. R. METEOROL. SOC.; GBR; DA. 1979; VOL. 105; NO 446; PP. 1027-1040; BIBL. 2 P.Article

ON THE WATER VAPOUR ABSORPTION IN THE 8-13 MU M SPECTRAL REGION FOR DIFFERENT ATMOSPHERIC CONDITIONSTOMASI C.1978; PURE APPL. GEOPHYS.; CHE; DA. 1978; VOL. 116; NO 6; PP. 1063-1076; BIBL. 15 REF.Article

LA CARTE ORANGETOMASI C.1975; TRANSPORTS; FR.; DA. 1975; NO 206; PP. 484-485; ABS. ANGL.Serial Issue

EVALUATION OF THE ATMOSPHERIC CONTENT OF PARTICULATE MASS FROM VISIBILITY OBSERVATIONSTOMASI C.1982; NUOVO CIMENTO SOC. ITAL. FIS., SEZ. C; ISSN 0390-5551; ITA; DA. 1982; VOL. 5; NO 2; PP. 223-246; ABS. ITA/RUS; BIBL. 44 REF.Article

INTERPOLATION METHODS FOR ESTIMATING ATMOSPHERIC PRECIPITABLE WATER VAPOUR DURING THE NIGHT FROM SURFACE METEOROLOGICAL DATA AND USING DIURNAL INFRARED HYGROMETER MEASUREMENTSTOMASI C.1978; MEM. SOC. ASTR. ITAL.; ITA; DA. 1978; VOL. 49; NO 1; PP. 119-125; BIBL. 9 REF.Conference Paper

THE NOCTURNAL SURFACE INVERSION HEIGHT IN THE PO VALLEYTOMASI C.1983; ATMOSPHERIC ENVIRONMENT; ISSN 0004-6981; GBR; DA. 1983; VOL. 17; NO 6; PP. 1123-1129; BIBL. 8 REF.Article

FEATURES OF THE SCALE HEIGHT FOR PARTICULATE EXTINCTION IN HAZY ATMOSPHERESTOMASI C.1982; J. APPL. METEOROL.; ISSN 0021-8952; USA; DA. 1982; VOL. 21; NO 7; PP. 931-944; BIBL. 2 P.Article

Vertical distribution features of atmospheric water vapor in the Mediterranean, Red Sea, and Indian OceanTOMASI, C.JGR. Journal of geophysical research. D. Atmospheres. 1984, Vol 89, Num 2, pp 2563-2566Article

MEASUREMENTS OF ATMOSPHERIC TURBIDITY AND VERTICAL MASS LOADING OF PARTICULATE MATTER IN MARINE ENVIRONMENTS (RED SEA, INDIAN OCEAN, AND SOMALIAN COAST)TOMASI C; PRODI F.1982; J. GEOPHYS. RES.; ISSN 0022-1406; USA; DA. 1982; VOL. 87; NO C2; PP. 1279-1286; BIBL. 17 REF.Article

EXPERIMENTAL COMPARISON BETWEEN VISIBLE AND NEAR INFRARED ATTENUATION OF SOLAR RADIATION IN HAZES AND FOGS.TOMASI C; GUZZI R.1977; QUART. J. R. METEOROL. SOC.; G.B.; DA. 1977; VOL. 103; NO 435; PP. 191-197; BIBL. 10 REF.Article

SIZE DISTRIBUTIONS OF TROPOSPHERIC PARTICLES IN TERMS OF THE MODIFIED GAMMA FUNCTION AND RELATIONSHIPS BETWEEN SKEWNESS AND MODE RADIUS.TOMASI C; TAMPIERI R.1977; TELLUS; SUEDE; DA. 1977; VOL. 29; NO 1; PP. 66-74; ABS. RUSSE; BIBL. 26 REF.Article

ATTENUATION OF INFRARED RADIATION THROUGH THE LOW ATMOSPHERETOMASI C; VITTORI O.1978; MEM. SOC. ASTR. ITAL.; ITA; DA. 1978; VOL. 49; NO 1; PP. 127-140; BIBL. 21 REF.Conference Paper

INFRARED RADIATION EXTINCTION SENSITIVITY TO THE MODIFIED GAMMA DISTRIBUTION PARAMETERS FOR HAZE AND FOG DROPLET POLYDISPERSIONS.TOMASI C; TAMPIERI F.1976; APPL. OPT.; U.S.A.; DA. 1976; VOL. 15; NO 11; PP. 2906-2912; BIBL. 17 REF.Article

SIZE DISTRIBUTION MODELS OF SMALL WATER DROPLETS IN MIST AND THEIR VOLUME EXTINCTION COEFFICIENTS AT VISIBLE AND INFRARED WAVELENGTHS.TOMASI C; TAMPIERI F.1976; ATMOSPH. ENVIRONMENT; G.B.; DA. 1976; VOL. 10; NO 11; PP. 1005-1013; BIBL. 19 REF.Article

MEASUREMENTS OF SOLAR RADIATION ATTENUATION BY HAZE AND GROUND FOG AT 0.5 MU M AND 3.7 MU M.GUZZI R; TOMASI C.1975; RIV. ITAL. GEOFIS. SCI. AFF.; ITAL.; DA. 1975; VOL. 2; NO 2; PP. 73-76; ABS. ITAL.; BIBL. 8 REF.Article

SIZE DISTRIBUTION MODELS OF FOG AND CLOUD DROPLETS IN TERMS OF THE MODIFIED GAMMA FUNCTION.TAMPIERI F; TOMASI C.1976; TELLUS; SUEDE; DA. 1976; VOL. 28; NO 4; PP. 333-347; ABS. RUSSE; BIBL. 31 REF.Article

SIZE DISTRIBUTION MODELS OF STRATOSPHERIC PARTICLES IN TERMS OF THE MODIFIED GAMMA FUNCTION.TAMPIERI F; TOMASI C.1976; ARCH. METEOROL. GEOPHYS. BIOKLIMATOL., A; OESTERR.; DA. 1976; VOL. 25; NO 1; PP. 47-54; ABS. ALLEM.; BIBL. 7 REF.Article

SIZE DISTRIBUTION MODELS OF FOG AND CLOUD DROPLETS AND THEIR VOLUME EXTINCTION COEFFICIENTS AT VISIBLE AND INFRARED WAVELENGTHS.TAMPIERI F; TOMASI C.1976; PURE APPL. GEOPHYS.; SWITZ.; DA. 1976; VOL. 114; NO 4; PP. 571-586; BIBL. 12 REF.Article

HIGH PRECISION ATMOSPHERIC HYDROMETRY USING THE SOLAR INFRARED SPECTRUM.TOMASI C; GUZZI R.1974; J. PHYS. E; G.B.; DA. 1974; VOL. 7; NO 8; PP. 647-649; BIBL. 7 REF.Article

THE "SO2-NH3-SOLUTION DROPLETS" SYSTEM IN AN URBAN ATMOSPHERETOMASI C; GUZZI R; VITTORI O et al.1975; J. ATMOSPH. SCI.; U.S.A.; DA. 1975; VOL. 32; NO 8; PP. 1580-1586; BIBL. 12 REF.Article

ATMOSPHERIC TURBIDITY VARIATIONS CAUSED BY LAYERS OF SAHARA DUST PARTICLESTOMASI C; PRODI F; TAMPIERI F et al.1979; BEITR. PHYS. ATMOSPH.; DEU; DA. 1979; VOL. 52; NO 3; PP. 215-228; ABS. GER/FRE; BIBL. 24 REF.Article

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