TURBULENT TRANSFER IN THE ATMOSPHERIC LAYER WITH SMALL WIND SHEAR.SHIMANUKI A.1975; J. METEOROL. SOC. JAP.; JAP.; DA. 1975; VOL. 53; NO 5; PP. 355-359; ABS. JAP.; BIBL. 5 REF.Article

RICERCA DI UN CRITERIO PER LA DETERMINAZIONE DELLE CAUSE DEL WIND-SHEAR VERIFICATOSI NELL' AEROPORTO DI PUNTA RAISI ATTRAVERSO I DATI STATISTICI RILEVATI DA REGISTRAZIONI BAROGRAFICHE = RECHERCHE D'UN CRITERE POUR LA DETERMINATION DES CAUSES DU CISAILLEMENT DU VENT, QUI S'EST VERIFIE A L'AEROPORT DE PUNTA RAISI, AU MOYEN DES DONNEES STATISTIQUES ELABOREES SUR LA BASE DES ENREGISTREMENTS BAROGRAPHIQUESCOSENTINO O; FERLAZZO G.1981; RIV. METEOROL. AERONAUT.; ISSN 0035-6328; ITA; DA. 1981; VOL. 41; NO 2; PP. 127-135; ABS. FRE/ENG; BIBL. 7 REF.Article

THE IMPORTANCE OF MOISTURE FLUCTUATIONS AND WIND SHEAR IN ACOUSTIC BACKSCATTER IN GATEGAYNOR JE.1979; J. APPL. METEOROL.; USA; DA. 1979; VOL. 18; NO 11; PP. 1472-1480; BIBL. 36 REF.Article

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

BEHAVIOR OF SPHERICAL BALLOONS IN WIND SHEAR LAYERSFICHTL GH.1972; J. GEOPHYS. RES.; U.S.A.; DA. 1972; VOL. 77; NO 21; PP. 3931-3935; BIBL. 4REF.Serial Issue

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

MEAN WIND-DIRECTION SHEAR THROUGH A FOREST CANOPY.SMITH FB; CARSON DJ; OLIVER HR et al.1972; BOUNDARY-LAGER METEOROL.,; NETHERL.; DA. 1972; VOL. 3; NO 2; PP. 178-190; BIBL. 9REF.Serial Issue

WIND SHEAR EFFECTS ON THE LANDING OF AIRCRAFT.LUERS JK; REEVES JB.1975; J. AIRCR.; U.S.A.; DA. 1975; VOL. 12; NO 7; PP. 565-566; BIBL. 5 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

INFLUENCE DU CISAILLEMENT VERTICAL DU VENT SUR L'EVOLUTION D'UN SYSTEME DE NUAGES DE CONVECTION ET SUR LA FORMATION DES AVERSESLEBEDEV SL.1976; METEOROL. I GIDROL.; S.S.S.R.; DA. 1976; NO 1; PP. 40-46; ABS. ANGL.; BIBL. 9 REF.Article

GEOSTROPHIC DRAG AND HEAT TRANSFER RELATIONS FOR THE ATMOSPHERIC BOUNDARY LAYER.ARYA SPS.1975; QUART. J.R. METEOROL. SOC.; G.B.; DA. 1975; VOL. 101; NO 427; PP. 147-161; BIBL. 1 P. 1/2Article

VERTICAL WIND SHEAR MEASUREMENTS IN THE LOWER STRATOSPHERE.CADET D.1975; QUART. J. R. METEOROL. SOC.; G.B.; DA. 1975; VOL. 101; NO 429; PP. 485-493; BIBL. 10 REF.Article

AN INVESTIGATION OF EXTREME LOW-LEVEL WIND SHEAR AT SELECTED STATIONS IN THE CONTERMINOUS UNITED STATES.GROSSMAN RL; BERAN DW.1975; J. APPL. METEOROL.; U.S.A.; DA. 1975; VOL. 14; NO 4; PP. 506-512; BIBL. 31 REF.Article

THE INFLUENCE OF GEOSTROPHIC SHEAR ON THE CROSS-ISOBAR ANGLE OF THE SURFACE WIND.THOMPSON RORY.1974; BOUNDARY-LAYER METEOROL.; NETHERL.; DA. 1974; VOL. 6; NO 3-4; PP. 515-518; BIBL. 5 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

ASPECTS OF THE INFLUENCE OF LOW-LEVEL WIND SHEAR ON AVIATION OPERATIONSKRAUS KA.sdIN: INT. CONF. AEROSP. AERONAUT. METEOROL. WASHINGTON, D.C., 1972; BOSTON, MASS.; AM. METEOROL. SOC.; DA. S.D.; PP. 332-333; BIBL. 9REF.Conference Proceedings

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

CONTINUOUS REPRESENTATION OF WIND STRESS AND WIND STRESS CURL OVER THE WORLD OCEAN.EVENSON AJ; VERONIS G.1975; J. MAR. RES.; U.S.A.; DA. 1975; VOL. 33; SUPPL.; PP. 131-144; BIBL. 11 REF.Article

THE GEOSTROPHIC DRAG COEFFICIENT.SWINBANK WC.1974; BOUNDARY-LAYER METEOROL.; NETHERL.; DA. 1974; VOL. 7; NO 1; PP. 125-127; BIBL. 5 REF.Article

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

THE EFFECTS OF VERTICAL WIND SHEAR ON THE EVOLUTION OF CONVECTIVE CLOUDS.PASTUSHKOV RS.1975; QUART. J. R METEOROL. SOC.; G.B.; DA. 1975; VOL. 101; NO 428; PP. 281-291; BIBL. 12 REF.Article

INTERNAL GRAVITY WAVES IN A ATMOSPHERE WITH WIND SHEAR: VALIDITY OF THE WKB APPROXIMATION AT CRITICAL LAGERS IN THE PRESENCE OF BUOYANCY FORCESWHITTEN RC; RIEGEL CA.1973; J. ATMOSPH. SCI.; U.S.A.; DA. 1973; VOL. 30; NO 2; PP. 313-316; BIBL. 12REF.Serial Issue