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Results 1 to 25 of 1083

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SHEAR LINE WEATHER REGIME OVER HAWAII.LARSON RN.1976; MONTH. WEATHER REV.; U.S.A.; DA. 1976; VOL. 104; NO 8; PP. 1081-1083Article

WIND SHEAR IN MONSOON DEPRESSIONSRAMAN CRV; RAO YP; SUBRAMANIAN SK et al.1979; WEATHER; GBR; DA. 1979; VOL. 34; NO 7; PP. 252-257; BIBL. 6 REF.Article

ATMOSPHERIC BIREFRINGENCE UNDER WITH SPEED GRADIENT SHEAR.BOYER GR; LAMOUROUX B; PRADE BS et al.1978; J. OPT. SOC. AMER.; U.S.A.; DA. 1978; VOL. 68; NO 4; PP. 471-474; BIBL. 8 REF.Article

A HIGH-FREQUENCY RADIO ACOUSTIC SOUNDER FOR REMOTE MEASUREMENT OF ATMOSPHERIC WINDS AND TEMPERATURE.FRANKEL MS; CHANG NJF; SANDERS MJ JR et al.1977; BULL. AMER. METEOROL. SOC.; U.S.A.; DA. 1977; VOL. 58; NO 9; PP. 928-934; BIBL. 8 REF.Article

WIND SHEAR OBSERVATIONS IN THUNDERSTORM DENSITY CURRENTS.HALL FF JR; NEFF WD; FRAZIER TV et al.1976; NATURE; G.B.; DA. 1976; VOL. 264; NO 5585; PP. 408-411; BIBL. 10 REF.Article

REQUIREMENTS FOR AN AIRPORT GROUND-BASED WIND SHEAR DETECTION SYSTEM.KALAFUS RM; HALLOCK JN.sdIN: CONF. AEROSP. AERONAUT. METEOROL. 7. SYMP. REMOTE SENSING SATELL.; MELBOURNE, FLA.; 1976; BOSTON; AM. METEOROL. SOC.; DA. S.D.; PP. 182-187; BIBL. 12 REF.Conference Paper

THE EFFECT OF WIND VELOCITY ON THE AMPLITUDE SCINTILLATIONS OF MILLIMETRE RADIO WAVES.HO KL; COLE RS; MAVROKOUKOULAKIS ND et al.1978; J. ATMOSPH. TERRESTR. PHYS.; G.B.; DA. 1978; VOL. 40; NO 4; PP. 443-448; BIBL. 11 REF.Article

COMMENTS ON INTERACTIONS BETWEEN A DISCRETE CONVECTIVE ELEMENT AND A SHEARING ENVIRONMENT: A NUMERICAL SIMULATIONPEARSON RA; WILKINS EM; SASAKI YK et al.1978; MONTH. WEATHER REV.; USA; DA. 1978; VOL. 106; NO 9; PP. 1376-1379; BIBL. 20 REF.Article

THE RELATION BETWEEN CLOUD PATTERN MOTION AND WIND SHEAR.HUBERT LF.1976; MONTH. WEATHER REV.; U.S.A.; DA. 1976; VOL. 104; NO 9; PP. 1167-1171; BIBL. 4 REF.Article

CISAILLEMENT DU VENT DANS LA COUCHE INFERIEURE, DE LA ZONE DES FRONTS ATMOSPHERIQUESVASIL'EV AA.1979; TRUDY GIDROMETEOROL. NAUCH.-ISSLEDOVAT. CENTRA S.S.S.R.; SUN; DA. 1979; NO 215; PP. 79-82; BIBL. 7 REF.Article

A WIND SHEAR AND GUST FRONT WARNING SYSTEM.BERAN DW; MANDICS PA; BEDARD AJ et al.sdIN: CONF. AEROSP. AERONAUT. METEOROL. 7. SYMP. REMOTE SENSING SATELL.; MELBOURNE, FLA.; 1976; BOSTON; AM. METEOROL. SOC.; DA. S.D.; PP. 167-174; BIBL. 13 REF.Conference Paper

THE DOWNWIND SPREAD OF AN INITIALLY VERTICAL COLUMN OF PARTICLES IN A SHEARED ENVIRONMENTSTEWART RE; MARWITZ JD.1982; J. APPL. METEOROL.; ISSN 0021-8952; USA; DA. 1982; VOL. 21; NO 8; PP. 1191-1193; BIBL. 5 REF.Article

SPORADIC-E LAYERS AND UNSTABLE WIND SHEARSSMITH LG; MILLER KL.1980; J. ATMOSPH. TERRESTR. PHYS.; GBR; DA. 1980; VOL. 42; NO 1; PP. 45-50; BIBL. 6 REF.Article

INTERACTIONS BETWEEN A DISCRETE CONVECTIVE ELEMENT AND A SHEARING ENVIRONMENT: A NUMERICAL SIMULATION.WILKINS EM; SASAKI YK; JOHNSON HL et al.1977; MONTH. WEATHER REV.; U.S.A.; DA. 1977; VOL. 105; NO 3; PP. 261-269; BIBL. 13 REF.Article

AN ANALYSIS OF THREE WEATHER-RELATED AIRCRAFT ACCIDENTS.FUJITA TT; CARACENA F.1977; BULL. AMER. METEOROL. SOC.; U.S.A.; DA. 1977; VOL. 58; NO 11; PP. 1164-1181; BIBL. 29 REF.Article

THE RESPONSE OF AN EQUATORIAL OCEAN TO SIMPLE WIND STRESS PATTERNS. II: NUMERICAL RESULTSCANE MA.1979; J. MAR. RES.; USA; DA. 1979; VOL. 37; NO 2; PP. 253-299; BIBL. 2 P.Article

A THREE-DIMENSIONAL NUMERICAL MODEL OF AN ISOLATED THUNDERSTOM. I. COMPARATIVE EXPERIMENTS FOR VARIABLE AMBIENT WIND SHEAR.SCHLESINGER RE.1978; J. ATMOSPH. SCI.; U.S.A.; DA. 1978; VOL. 35; NO 4; PP. 690-713; BIBL. 39 REF.Article

THE ATTENUATION OF VERTICALLY PROPAGATING INTERNAL GRAVITY WAVES BY A RANDOMLY VARYING WIND/CURRENT SHEAR.THOMSON RE.1976; J. ATMOSPH. SCI.; U.S.A.; DA. 1976; VOL. 33; NO 1; PP. 52-58; BIBL. 12 REF.Article

VERTICAL WIND SHEARS, TURBULENCE AND NON-TURBULENCE IN THE TROPOSPHERE AND STRATOSPHEREWEINSTOCK J.1980; GEOPHYS. RES. LETT.; ISSN 0094-8276; USA; DA. 1980; VOL. 7; NO 10; PP. 749-752; BIBL. 17 REF.Article

WIND AND TEMPERATURE PROFILE PREDICTION FOR DIABATIC SURFACE LAYERS INCLUDING STRONG INVERSION CASESLETTAU HH.1979; BOUNDARY-LAYER METEOROL.; NLD; DA. 1979; VOL. 17; NO 4; PP. 443-464; BIBL. 1 P.Article

WINDSCHERUNGEN IN DEN UNTEREN 700 M DER ATMOSPHAERE IN ABHAENGIGKEIT VON TOEGESZEIT UND DIFFUSIONSKLASSE. = CISAILLEMENT DU VENT DANS LES 700 PREMIERS METRES DE L'ATMOSPHERE, COMME FONCTION DE L'HEURE DE LA JOURNEE ET DES CLASSES DE DIFFUSIONAHRENS D.1977; METEOROL. RDSCH.; DTSCH.; DA. 1977; VOL. 30; NO 6; PP. 172-175; ABS. ANGL.; BIBL. 9 REF.Article

LOW LEVEL WIND SHEAR ASSOCIATED WITH CONVECTIVE STORMS.KADLEC PW.sdIN: CONF. AEROSP. AERONAUT. METEOROL. 7. SYMP. REMOTE SENSING SATELL.; MELBOURNE, FLA.; 1976; BOSTON; AM. METEOROL. SOC.; DA. S.D.; PP. 28-30; BIBL. 2 REF.Conference Paper

THERMAL STRUCTURE AND DYNAMICS OF SATURN AND JUPITERPIRRAGLIA JA; CONRATH BJ; ALLISON MD et al.1981; NATURE (LOND.); ISSN 0028-0836; GBR; DA. 1981; VOL. 292; NO 5825; PP. 677-679; BIBL. 9 REF.Article

CARACTERISTIQUES STATISTIQUES DU CISAILLEMENT DU VENT INSTANTANE DANS LA COUCHE INFERIEURE DE L'ATMOSPHEREBYZOVA NL; VOLKOVITSKAYA ZI.1980; METEOROL. GIDROL.; ISSN 0130-2906; SUN; DA. 1980; NO 12; PP. 31-38; ABS. ENG; BIBL. 18 REF.Article

DESIGN OF A WIND SHEAR DETECTION RADAR FOR AIRPORTSCHADWICK RB; MORAN KP; CAMPBELL WC et al.1979; I.E.E.E. TRANS. GEOSCI. ELECTRON.; USA; DA. 1979; VOL. 17; NO 4; PP. 137-142; BIBL. 18 REF.Article

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