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SOLUTION NUMERIQUE DU SYSTEME D'EQUATIONS DU MOUVEMENT TURBULENT DANS LA COUCHE SUPERIEURE DE L'OCEANKALATSKIJ VI.1975; GIDROMETEOROL. NAUCH.-ISSLEDOVAT. CENTR S.S.S.R., TRUDY; S.S.S.R.; DA. 1975; NO 119; PP. 61-69; BIBL. 9 REF.Article

CALCUL DES VARIATIONS SAISONNIERES DE L'EPAISSEUR ET DE LA TEMPERATURE DE LA COUCHE SUPERIEURE QUASI-HOMOGENE DE L'OCEANRESNYANSKIJ YU D.1976; GIDROMETEOROL. NAUCH.-ISSLEDOVAT. CENTR. S.S.S.R., TRUDY; S.S.S.R.; DA. 1976; NO 182; PP. 27-36; BIBL. 13 REF.Article

EXPERIMENTAL MEASUREMENTS IN SUPERSONIC REACTING (F+H2) MIXING LAYERS.SHACKLEFORD WL; WITTE AB; BROADWELL JE et al.1974; A.I.A.A. J., NEW YORK; U.S.A.; DA. 1974; VOL. 12; NO 8; PP. 1009-1010; BIBL. 5 REF.Article

STRUCTURE AND HEAT ENERGY BUDGET OF MIXED LAYER CAPPED BY INVERSION DURING THE PERIOD OF POLAR OUTBREAK OVER KUROSHIO REGION.NINOMIYA K; AKIYAMA T.1976; J. METEOROL. SOC. JAP.; JAP.; DA. 1976; VOL. 54; NO 3; PP. 160-174; ABS. JAP.; BIBL. 15 REF.Article

MIXING LAYERS FOR HIGHLY UNDEREXPANDED SUPERSONIC JETS IN HYPERSONIC STREAMS.MORAN JP.1974; J. FLUID MECH.; G.B.; DA. 1974; VOL. 65; NO 1; PP. 153-175; BIBL. 1 P. 1/2Article

MODELLING BUOYANCY DRIVEN MIXED LAYERS.ZEMAN O; LUMLEY JL.1976; J. ATMOSPH. SCI.; U.S.A.; DA. 1976; VOL. 33; NO 10; PP. 1974-1988; BIBL. 30 REF.Article

SIMULATION PAR MODELE NUMERIQUE DES PROCESSUS DE TRANSFERT TURBULENT DANS LA ZONE DE MELANGEKURBATSKIJ AF.1975; P.M.T.F.; S.S.S.R.; DA. 1975; NO 3; PP. 125-133; BIBL. 15 REF.Article

THEORIE DE SIMILITUDE POUR LA COUCHE LIMITE OCEANIQUEZHOLUDEV VD.1983; OKEANOLOGIJA; ISSN 0030-1574; SUN; DA. 1983; VOL. 23; NO 1; PP. 27-35; ABS. ENG; BIBL. 30 REF.Article

MODELE POUR LE CALCUL DE L'EPAISSEUR DE LA COUCHE DE MELANGE DANS L'OCEANKIL'MATOV TR; PROTASOV SN.1980; METEOROL. I GIDROL.; SUN; DA. 1980; NO 3; PP. 59-64; ABS. ENG; BIBL. 8 REF.Article

A NUMERICAL INVESTIGATION OF MIXED-LAYER DYNAMICSKUNDU PK.1980; J. PHYS. OCEANOGR.; USA; DA. 1980; VOL. 10; NO 2; PP. 220-236; BIBL. 34 REF.Article

VARIATIONS DE LA DENSITE DANS LA COUCHE ACTIVE DE L'OCEANKUTALO AA.1975; GIDROMETEOROL. NAUCH.-ISSLEDOVAT. CENTR S.S.S.R., TRUDY; S.S.S.R.; DA. 1975; NO 161; PP. 26-34; BIBL. 3 REF.Article

EXPERIMENTATION RELATIVE A LA DETERMINATION DE L'EPAISSEUR DE LA COUCHE DE TURBULENCE DANS LES ONDES DU TYPE MONOCHROMATIQUEDOBROKLONSKIJ SV; KONTOBOJTSEVA NV.1973; IZVEST. AKAD. NAUK S.S.S.R., FIZ. ATMOSF. OKEANA; S.S.S.R.; DA. 1973; VOL. 9; NO 2; PP. 210-212; H.T. 1; BIBL. 4 REF.Serial Issue

AN UNSTABLE UNIFORM SLAB MODEL OF THE MIXED LAYER AS A SOURCE OF DOWNWARD PROPAGATION NEAR-INERTIAL MOTION. I: STEADY MEAN FLOWKROLL J.1982; JOURNAL OF MARINE RESEARCH; ISSN 0022-2402; USA; DA. 1982; VOL. 40; NO 4; PP. 1013-1033; BIBL. 12 REF.Article

MEASUREMENTS OF AEROSOL SIZE DISTRIBUTIONS IN THE LOWER TROPOSPHERE OVER NORTHERN EUROPEFITCH BW; CRESS TS.1981; J. APPL. METEOROL.; ISSN 0021-8952; USA; DA. 1981; VOL. 20; NO 10; PP. 1119-1128; BIBL. 13 REF.Article

THE EFFECT OF THE MIXING LAYER ON THE SEA BREEZE CIRCULATION AND THE DIFFUSION OF POLLUTANTS ASSOCIATED WITH LAND-SEA BREEZESKONDO H; GAMBO K.1979; J. METEOROL. SOC. JAP.; JPN; DA. 1979; VOL. 57; NO 6; PP. 560-575; BIBL. 22 REF.Article

AN INVESTIGATION OF THE IMPORTANCE OF THIRD-ORDER CORRELATIONS AND CHOICE OF LENGTH SCALE IN MIXED LAYER MODELLINGWARN VARNAS AC; PIACSEK SA.1979; GEOPHYS. ASTROPHYS. FLUID DYNAM.; GBR; DA. 1979; VOL. 13; NO 1-3; PP. 225-243; BIBL. 20 REF.Article

CALCUL DES CARACTERISTIQUES DE LA COUCHE DE MELANGE DANS LA ZONE DE L'OCEAN EQUATORIALPOLONSKIJ AB.1980; METEOROL. I GIDROL.; SUN; DA. 1980; NO 3; PP. 65-72; ABS. ENG; BIBL. 19 REF.Article

THE TURBULENCE STRUCTURE OF A HIGHLY CURVED MIXING LAYER.CASTRO IP; BRADSHAW P.1976; J. FLUID MECH.; G.B.; DA. 1976; VOL. 73; NO 2; PP. 265-304; BIBL. 38 REF.Article

COMPARISON OF OBSERVED MIXED-LAYER DEPTHS TO MODEL ESTIMATES USING OBSERVED TEMPERATURES AND WINDS, AND MOS FORECASTSGARRETT AJ.1981; J. APPL. METEOROL.; ISSN 0021-8952; USA; DA. 1981; VOL. 20; NO 11; PP. 1277-1283; BIBL. 12 REF.Article

A SIMPLE OCEAN SURFACE LAYER MODEL.DYKE PPG.1977; RIV. ITAL. GEOFIS. SCI. AFF.; ITAL.; DA. 1977; VOL. 4; NO 1-2; PP. 31-34; BIBL. 1/2 P.Article

ASYMPTOTIC REGIMES IN MIXED-LAYER DEEPENING.DE SZOECKE RA; RHINES PB.1976; J. MAR. RES.; U.S.A.; DA. 1976; VOL. 34; NO 1; PP. 111-116; BIBL. 4 REF.Article

THE DENSITY OF ORGANIZED VORTICES IN A TURBULENT MIXING LAYER.MOORE DW; SAFFMAN PG.1975; J. FLUID MECH.; G.B.; DA. 1975; VOL. 69; NO 3; PP. 465-473; BIBL. 7 REF.Article

THE TROPICAL MIXED LAYER AND CUMULUS PARAMETERIZATION.SARACHIK ES.1974; J. ATMOSPH. SCI.; U.S.A.; DA. 1974; VOL. 31; NO 8; PP. 2225-2230; BIBL. 14 REF.Article

VARIABILITE HORIZONTALE DANS LA COUCHE SUPERIEURE DE MELANGE: RESULTATS DE L'EXPERIENCE MILDEX EN MEDITERRANEENIHOUL JCJ; LEWALLE A; LOFFET A et al.1981; BULL. SOC. R. SCI. LIEGE; ISSN 0037-9565; BEL; DA. 1981; VOL. 50; NO 11-12; PP. 483-493; BIBL. 10 REF.Conference Paper

STRUCTURE DE LA COUCHE MELANGEE DANS UN FLUIDE STRATIFIEPOPOV VA; CHASHECHKIN YU D.1980; IZVEST. AKAD. NAUK S.S.S.R., FIZ. ATMOSF. OKEANA; SUN; DA. 1980; VOL. 16; NO 3; PP. 284-293; ABS. ENG; BIBL. 16 REF.Article

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