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Results 1 to 25 of 894

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REMOVAL OF PYROTECHNIC GENERATED TRACER PLACED BY AIRCRAFT IN A CONVECTIVE UPDRAFT.DINGLE AN.1974; IN: SCI. CONF. WEATHER MODIF. PROC.; TASHKENT; 1973; GENEVA; WORLD METEOROL. ORGAN.; DA. 1974; PP. 507-520; BIBL. 5 REF.Conference Paper

THE INITIATION OF PRECIPITATION IN UPDRAFTSROKICKI ML; YOUNG KC.1978; J. APPL. METEOROL.; USA; DA. 1978; VOL. 17; NO 6; PP. 745-754; BIBL. 28 REF.Article

ESTIMATING UPDRAFT VELOCITY FROM AN AIRPLANE RESPONSE.LENSCHOW DH.1976; MONTH. WEATHER REV.; U.S.A.; DA. 1976; VOL. 104; NO 5; PP. 618-627; BIBL. 10 REF.Article

FURTHER STUDY OF THE SEVERE STORM WITH A ROTATING UPDRAFT CONFIGURATIONYEONG JER LIN; MARTIN DE.1972; TELLUS; SUEDE; DA. 1972; VOL. 24; NO 3; PP. 216-229; ABS. RUSSE; BIBL. 1P.Serial Issue

SIZE SORTING OF HAIL IN A THREE-DIMENSIONAL UPDRAFT AND IMPLICATIONS FOR HAIL SUPPRESSIONPALUCH IR.1978; J. APPL. METEOROL.; USA; DA. 1978; VOL. 17; NO 6; PP. 763-777; BIBL. 29 REF.Article

DISCUSSION OF MEASUREMENTS INSIDE HIGH-SPEED THUNDERSTORM UPDRAFTS.DAVIES JONES RP.1974; J. APPL. METEOROL.; U.S.A.; DA. 1974; VOL. 13; NO 6; PP. 710-717; BIBL. 19 REF.Article

EINFLUSS DES THERMISCHEN AUFTREIBS BEIM SCHWEISSEN AUF DIE LUEFTUNGSVERHAELTNISSE AM ARBEITSPLATZ DES SCHWEISSERS = THE EFFECT OF THERMAL UPCURRENTS ON VENTILATION CONDITIONS AT THE WELDERS' WORKING STATION DURING WELDING = INFLUENCE DES COURANTS ASCENDANTS D'ORIGINE THERMIQUE SUR LES CONDITIONS DE VENTILATION AU POSTE DE SOUDAGEHOELZEL G; KOENIG R.1981; SCHWEISSEN+SCHNEIDEN; ISSN 0036-7184; DEU; DA. 1981; VOL. 33; NO 7; PP. 309-315; BIBL. 2 REF.; IDEM ENG; LOC. ISArticle

ROLE DES MOUVEMENTS ASCENDANTS DANS LA FORMATION DES PRECIPITATIONS ARTIFICIELLESSTALEVICH DD; UCHEVATKINA TS.1972; TRUDY GLAVN. GEOFIZ. OBS. A.I. VOEJKOVA, LENINGRAD; S.S.S.R.; DA. 1972; NO 278; PP. 19-28; BIBL. 14 REF.Serial Issue

OBSERVATIONS OF A CLOUD ARC TRIGGERED BY THUNDERSTROM OUTFLOWMATTHEWS DA.1981; MON. WEATHER REV.; ISSN 0027-0644; USA; DA. 1981; VOL. 109; NO 10; PP. 2140-2157; BIBL. 20 REF.Article

LOCATION OF UPDRAFT IN RELATION TO HIGH REFLECTIVITY ZONES.SAND WR; MUSIL DJ; SCHLEUSENER RA et al.sdIN: 4TH CONF. WEATHER MODIF. AM. METEOROL. SOC. PREPR.; FORT LAUDERDALE, FLA.; 1974; BOSTON, MASS; AM. METEOROL. SOC.; DA. S.D.; PP. 133-138; BIBL. 13 REF.Conference Paper

THE DISPERSAL OF SEEDING MATERIAL IN THE UPDRAFT OF STORMS.KYLE TG.sdIN: 4TH CONF. WEATHER MODIF. AM. METEOROL. SOC. PREPR.; FORT LAUDERDALE, FLA.; 1974; BOSTON, MASS.; AM. METEOROL. SOC.; DA. S.D.; PP. 69-72; BIBL. 8 REF.Conference Paper

UPDRAFT PROPERTIES DEDUCED STATISTICALLY FROM RAUVIN SOUNDINGS.DAVES JONES RP; HENDERSON JH.1975; PURE APPL. GEOPHYS.; SWITZ.; DA. 1975; VOL. 113; NO 5-6; PP. 787-801; BIBL. 15 REF.Article

THE RELATIVE IMPORTANCE OF VARIATIONS IN CCN SPECTRA AND UPDRAFT STRENGTH.JOHNSON DB.1976; J. ATMOSPH. SCI.; U.S.A.; DA. 1976; VOL. 33; NO 2; PP. 345-346; BIBL. 2 REF.Article

PREVISION DES VITESSES ASCENDANTES DES PLANEURS EN CONVECTION THERMIQUE DE PLAINE.VAILLANT R.1977; METEOROLOGIE; FR.; DA. 1977; VOL. 6; NO 40; PP. 77-91; BIBL. 2 REF.Article

ON THE CONDENSED WATER MASS IN RISING AIR.KESSLER E.1975; PURE APPL. GEOPHYS.; SWITZ.; DA. 1975; VOL. 113; NO 5-6; PP. 971-981; BIBL. 10 REF.Article

CALCULATIONS OF UPDRAFT SHAPES IN STORMS1972; J. ATMOSPH. SCI.,; U.S.A.; DA. 1972; VOL. 29; NO 8; PP. 1516-1519; BIBL. 14REF.Serial Issue

A DIAGNOSTIC STUDY OF INTERACTION OF CUMULUS UPDRAFTS AND DOWNDRAFTS WITH LARGE-SCALE MOTIONS IN GATENITTA T.1978; J. METEOROL. SOC. JAP.; JPN; DA. 1978; VOL. 56; NO 4; PP. 232-242; ABS. JAP; BIBL. 19 REF.Article

FORMATION DES CORDONS DE TOURBILLONS DES COURANTS ASCENDANTS AU-DESSUS D'UN LIQUIDE DANS LE CAS D'EVAPORATIONVLADIMIROV VA.1977; DOKL. AKAD. NAUK S.S.S.R.; S.S.S.R.; DA. 1977; VOL. 236; NO 2; PP. 316-318; BIBL. 2 REF.Article

STUDIES ON THE FLUID MOTION ON THE HEAVY MEDIA SEPARATION PROCESS.SUNDAMURTI NS; MISRA VN; SESHADRI V et al.1976; J. INSTIT. ENGRS (INDIA), MING METAL DIV.; INDIA; DA. 1976; VOL. 57; NO 1; PP. 26-29; BIBL. 7 REF.Article

A STUDY OF UPDRAFT-DOWNDRAFT INTERACTION BASED ON PERTURBATION PRESSURE AND SINGLE-DOPPLER RADAR DATA.BONESTEELE RG; LIN YJ.1978; MONTH. WEATHER REV.; U.S.A.; DA. 1978; VOL. 106; NO 1; PP. 62-68; BIBL. 17 REF.Article

A NUMERICAL MODEL OF THE UPDRAFT-DOWNDRAFT INTERACTION IN CB CLOUDSNIEWIADOMSKI M.1979; ACTA GEOPHYS. POLON.; POL; DA. 1979; VOL. 27; NO 3; PP. 277-291; ABS. POL; BIBL. 9 REF.Article

DISPOSITIF POUR DETERMINER LA POSITION DU MAXIMUM DE V ASCENTIONNELLE D'UN COURANT D'AIR ASCENDANTLAVROVA AT; CHUBIKOV VN.1975; IZVEST. VYSSH. UCHEBN. ZAVED., PRIBOROSTR.; S.S.S.R.; DA. 1975; VOL. 18; NO 5; PP. 92-96; BIBL. 4 REF.Article

DOPPLER RADAR RELATIONSHIPS FOR HAIL AT VERTICAL INCIDENCE.ULBRICH CW.1977; J. APPL. METEOROL.; U.S.A.; DA. 1977; VOL. 16; NO 12; PP. 1349-1359; BIBL. 13 REF.Article

EXPERIMENTAL STUDY OF UPSTREAM INFLUENCE IN THE TWO-DIMENSIONAL FLOW OF A STRATIFIED FLUID OVER AN OBSTACLE.WEI SN; KAO TW; HSIEN PING PAO et al.1975; GEOPHYS. FLUID DYNAM.; G.B.; DA. 1975; VOL. 6; NO 4; PP. 315-336; BIBL. 18 REF.Article

INCLUSION OF MESOSCALE UPDRAFTS AND DOWNDRAFTS IN COMPUTATIONS OF VERTICAL FLUXES BY ENSEMBLES OF TROPICAL CLOUDSHOUZE RA JR; CHEE PONG CHENG.1981; J. ATMOS. SCI.; ISSN 0022-4928; USA; DA. 1981; VOL. 38; NO 8; PP. 1751-1770; BIBL. 22 REF.Article

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