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AN OBSERVATIONAL STUDY OF LEE WAVES USING RADIOSONDE DATEREID SJ.1972; TELLUS; SUEDE; DA. 1972; VOL. 24; NO 6; PP. 593-596; BIBL. 1REF.Serial Issue

MODELES DES ONDES SOUS LE VENT DANS UNE TOPOSPHERE BAROCLINE COMPRESSIBLEZEJTUNYAN R KH.1979; IZVEST. AKAD. NAUK S.S.S.R., FIZ. ATMOSF. OKEANA; SUN; DA. 1979; VOL. 15; NO 5; PP. 498-507; ABS. ENG; BIBL. 8 REF.Article

TWO-DIMENSIONAL LINEAR LEE WAVE MODES FOR MODELS INCLUDING A STRATOSPHERE.BERKSHIRE FH.1975; QUART. J. R. METEOROL. SOC.; G.B.; DA. 1975; VOL. 101; NO 428; PP. 259-266; BIBL. 14 REF.Article

LEEWELLENBEOBACHTUNGEN IM WESERBERGLAND. - EINIGE BEISPIELE = OBSERVATIONS D'ONDES SOUS LE VENT DANS LE WESERBERGLAND - QUELQUES EXEMPLESMULLER D.1983; METEOROLOGISCHE RUNDSCHAU; ISSN 0026-1211; DEU; DA. 1983; VOL. 36; NO 3; PP. 166-168; BIBL. 25 REF.Article

MARTIAN ATMOSPHERIC LEE WAVES.PIRRAGLIA JA.1976; ICARUS; U.S.A.; DA. 1976; VOL. 27; NO 4; PP. 517-530; BIBL. 13 REF.Article

LEEWELLEN HINTER GEBIRGEN, MODELLE UND BERECHNUNGEN. II. BERECHNUNGEN. = ONDES SOUS LE VENT D'UNE MONTAGNE, MODELE ET CALCULS. II. CALCULSMAYER I.1976; METEOROL. RDSCH.; DTSCH.; DA. 1976; VOL. 29; NO 6; PP. 161-180Article

OBSERVATIONS OF LEE WAVES OVER CANTERBURY AND COMPARISONS WITH THEORETICAL MODELS.CHERRY NJ.sdIN: NELCON'74. 11TH NEW ZEALAND NATL. ELECTRON. GEOPHYS. CONV. PROC.; AUCKLAND; 1974; AUCKLAND; UNIV.; DA. S.D.; PP. 1-12; H.T. 7; BIBL. 6 REF.Conference Paper

THREE-DIMENSIONAL LEE-WAVE PATTERNGJEVIK B; MARTHINSEN T.1978; QUART. J. R. METEOROL. SOC.; GBR; DA. 1978; VOL. 104; NO 442; PP. 947-957; BIBL. 12 REF.Article

AN EXAMINATION OF THE FORMATION OF LINEAR LEE WAVES GENERATED BY GIANT MARTIAN VOLCANOESPICKERSGILL AO; HUNT GE.1981; J. ATMOS. SCI.; ISSN 0022-4928; USA; DA. 1981; VOL. 38; NO 1; PP. 40-51; BIBL. 13 REF.Article

CALCUL DE LA T DE RECHAUFFEMENT PROVOQUE PAR LA DISSIPATION DES ONDES SOUS LE VENT D'UNE MONTAGNEBLANK AD.1980; IZVEST. AKAD. NAUK S.S.S.R., FIZ. ATMOSF. OKEANA; SUN; DA. 1980; VOL. 16; NO 6; PP. 643-647; BIBL. 9 REF.Article

A CASE STUDY OF LEE WAVES IN SOUTH-WESTERLY AIRFLOW OVER BANK'S PENINSULA, NEW ZEALANDSTURMAN AP.1980; WEATER; GBR; DA. 1980; VOL. 35; NO 2; PP. 32-39; BIBL. 12 REF.Article

THE DYNAMICS OF WAVE INDUCED DOWNSLOPE WINDS.KLEMP JB; LILLY DK.1975; J. ATMOSPH. SCI.; U.S.A.; DA. 1975; VOL. 32; NO 2; PP. 320-339; BIBL. 18 REF.Article

EXPERIENCE NUMERIQUE RELATIVE AU CALCUL DES ONDES DE GRAVITE NON STATIONNAIRES DANS UNE ATMOSPHERE LIBREKISEL'NIKOVA VZ.1975; METEOROL. I GIDROL.; S.S.S.R.; DA. 1975; NO 4; PP. 23-30; ABS. ANGL.; BIBL. 4 REF.Article

AN INVESTIGATION OF TROPOSPHERIC WIND AND STATIC STABILITY CONDITIONS IN RELATION TO LEE-WAVE-LENGTHS, AND OF WIND CONDITIONS IN RELATION TO CONVECTIVE CELL PATTERNS, USING SATELLITE PICTURESRAUSTEIN E.1973; METEOROL. ANN.; NORGE; DA. 1973; VOL. 6; NO 6; PP. 125-140; BIBL. 10REF.Serial Issue

RESONANCE CHARACTERISTICS OF LINEAR LEE WAVES IN AN ATMOSPHERE OF THREE LAYERSBERKSHIRE FH; PICKERSGILL AO.1978; QUART. J. R. METEOROL. SOC.; GBR; DA. 1978; VOL. 104; NO 442; PP. 895-909; BIBL. 10 REF.Article

VISCOUS EFFECTS IN LEE WAVESSTEVENSON TN; CHANG WL; LAWS P et al.1979; GEOPHYS. ASTROPHYS. FLUID DYNAM.; GBR; DA. 1979; VOL. 13; NO 1-3; PP. 141-151; BIBL. 14 REF.Article

INFERENCE OF THE LOCAL WEATHER FROM THE LARGE-SCALE NUMERICAL WEATHER PREDICTION. A STUDY ON THE LEEWAVES TO THE EAST OF THE TAIHANG MOUNTAIN.TU HSING YUAN; HSU YOU FENG.1976; IN: SYMP. INTERPRETATION BROAD-SCALE NWP PROD. FOR LOCAL FORECASTING PURPOSES. WORLD METEOROL. ORGAN.; WARSAW; 1976; GENEVA; WORLD METEOROL. ORGAN.; DA. 1976; PP. 53-59Conference Paper

THE GENERATION OF LEE WAVES BY THE BLUE RIDGE.SMITH RB.1976; J. ATMOSPH. SCI.; U.S.A.; DA. 1976; VOL. 33; NO 3; PP. 507-519; BIBL. 17 REF.Article

WAVE DRAG BY THREE-DIMENSIONAL MOUTAIN LEE-WAVES IN NONPLANAR SHEAR FLOW.BLUMEN W; MCGREGOR CD.1976; TELLUS; SUEDE; DA. 1976; VOL. 28; NO 4; PP. 287-298; ABS. RUSSE; BIBL. 15 REF.Article

LEE WAVES IN STRATIFIED FLOWS WITH SIMPLE HARMONIC TIME DEPENDENCE.BELL TH.1975; J. FLUID MECH.; G.B.; DA. 1975; VOL. 67; NO 4; PP. 705-722; BIBL. 1 P.Article

DAS WINDFELD AM HAARDTRAND WAEHREND MESOKLIP: ABSCHAETZUNGEN DER HANGWINDZIRKULATION UND BEOBACHTUNGSERGEBNISSE = CHAMP D'ECOULEMENT D'AIR SUR LA BORDURE DU HAARDT, DURANT MESOKLIP. ESTIMATION DE LA CIRCULATION DE PENTE ET OBSERVATIONSHENNEMUTH B; SEMMLER H.1982; METEOROL. RUNDSCH.; ISSN 0026-1211; DEU; DA. 1982; VOL. 35; NO 4; PP. 113-121; ABS. ENG; BIBL. 22 REF.Article

AN ANALYSIS OF THREE-DIMENSIONAL MOUNTAIN LEE-WAVES IN A STRATIFIED SHEAR FLOW. IIBLUMEN W; DIETZE SC.1982; JOURNAL OF THE ATMOSPHERIC SCIENCES; ISSN 0022-4928; USA; DA. 1982; VOL. 39; NO 12; PP. 2712-2720; BIBL. 8 REF.Article

MOUNTAIN WAVES.BEER T.1976; SCI. PROGR.; G.B.; DA. 1976; VOL. 63; NO 249; PP. 1-25; BIBL. 1 P. 1/2Article

LEEWELLEN HINTER GEBIRGEN, MODELLE UND BERECHNUNGEN. I. THEORIE UND MODELLE. = ONDES SOUS LE VENT D'UNE CHAINE DE MONTAGNES, MODELE ET CALCULMAYER I.1976; METEOROL. RDSCH.; DTSCH.; DA. 1976; VOL. 29; NO 4; PP. 97-109; ABS. ANGL.; BIBL. 27 REF.Article

Observation de l'ozone dans des ondes sous le vent des montagnesGRUZDEV, A. N; ELANSKIJ, N. F.Izvestija Akademii nauk SSSR. Fizika atmosfery i okeana. 1984, Vol 20, Num 8, pp 705-714Article

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