THE INTERACTION OF SURFACE AND INTERNAL TIDES WITH BOUNDARY CURRENTS.MOOERS CNK.1977; LECTURE NOTES PHYS.; GERM.; DA. 1977; VOL. 64; PP. 172Article

RESOLUTION NUMERIQUE D'UN PROBLEME DE MODELE DE COURANT OCEANIQUEMITROFANOV VA.1976; OKEANOLOGIJA; S.S.S.R.; DA. 1976; VOL. 16; NO 2; PP. 212-215; ABS. ANGL.; BIBL. 5 REF.Article

LABORATORY EXPERIMENTS ON FRONTS. I: DENSITY-DRIVEN BOUNDARY CURRENTSGRIFFITHS RW; LINDEN PF.1982; GEOPHYS. ASTROPHYS. FLUID DYN.; ISSN 0309-1929; GBR; DA. 1982; VOL. 19; NO 3-4; PP. 159-187; BIBL. 14 REF.Article

FREE, STABLE CONTINENTAL SHELF WAVES IN A SHEARED, BAROTROPIC BOUNDARY CURRENT.BROOKS DA; MOOERS CNK.1977; J. PHYS. OCEANOGR.; U.S.A.; DA. 1977; VOL. 7; NO 3; PP. 380-388; BIBL. 21 REF.Article

GENERATION OF FIELD SCATTERED BY IMPERFECTLY CONDUCTING OBJECTS FROM THE SOLUTION OF A PERFECTLY CONDUCTING OBJECTSEBAK AA; SHAFAI L; MOHSEN A et al.1983; ELECTRON. LETT.; ISSN 0013-5194; GBR; DA. 1983; VOL. 19; NO 1; PP. 25-27; BIBL. 3 REF.Article

THE ADVECTION EFFECT OF PLANETARY VORTICITY ON SEA LEVEL SLOPE IN A WESTERN BOUNDARY CURRENT.CHEW F.1977; MAR. GEOD.; U.S.A.; DA. 1977; VOL. 1; NO 1; PP. 103-116; BIBL. 13 REF.Article

THE INFLUENCE OF A COSTAL HEADLAND ON OCEANIC BOUNDARY-CURRENTSWILLMOTT AJ.1983; GEOPHYSICAL AND ASTROPHYSICAL FLUID DYNAMICS; ISSN 0309-1929; GBR; DA. 1983; VOL. 23; NO 4; PP. 273-299; BIBL. 2 P.Article

FORAMINIFERA.MCGOWRAN B.1974; IN: INITIAL REP. DEEP SEA DRILLING PROJ. DARWIN, AUSTRALIA TO COLOMBO, CEYLON; 1972; WASHINGTON; U.S. GOV. PRINT. OFF.; DA. 1974; VOL. 22; PP. 609-627; BIBL. 14 REF.; 10 ILL.Book Chapter

BOUNDARY-LAYER DEVELOPMENT ON CIRCULAR CYLINDERSCELIK I; PATEL VC.1982; BOUNDARY-LAYER METEOROLOGY; ISSN 0006-8314; NLD; DA. 1982; VOL. 24; NO 3; PP. 281-293; BIBL. 11 REF.Article

ON THE INITIAL DEVELOPMENT OF BAROTROPIC INERTIAL BOUNDARY LAYERS.KING HELE JA; PAULSON RW.1976; DEEP SEA RES.; G.B.; DA. 1976; VOL. 23; NO 5; PP. 403-411; BIBL. 8 REF.Article

A THEORY OF THE WIND-DRIVEN CIRCULATION II. GYRES WITH WESTERN BOUNDARY LAYERSYOUNG WR; RHINES PB.1982; JOURNAL OF MARINE RESEARCH; ISSN 0022-2402; USA; DA. 1982; VOL. 40; NO 3; PP. 849-872; BIBL. 18 REF.Article

BACKSCATTER LASER VELOCIMETER FOR ENERGETIC BOTTOM BOUNDARY LAYERS: THE OPTICAL SIGNALAGRAWAL YC; TERRY WE JR; WILLIAMS AJ III et al.1982; IEEE J. OCEANIC ENG.; ISSN 0364-9059; USA; DA. 1982; VOL. 7; NO 4; PP. 150-154; BIBL. 6 REF.Article

LOESUNG DES RANDWERTPROBLEMS BEI ANWESSENHEIT LEITENDER KOERPER HOHER PERMEABILITAET IM ERREGENDEN MAGNETISCHEN WECHSELFELD = RESOLUTION DU PROBLEME AUX VALEURS LIMITES EN PRESENCE DE CORPS CONDUCTEURS DE HAUTE PERMEABILITE DANS UN CHAMP INDUCTEUR ALTERNATIFHANNAKAM L; ALBACH M.1982; ARCH. ELEKTROTECH. (BERL.); ISSN 0003-9039; DEU; DA. 1982; VOL. 65; NO 1-2; PP. 117-122; ABS. ENGArticle

EFFECTS OF BOTTOM TOPOGRAPHY AND DENSITY STRATIFICATION ON THE FORMATION OF WESTERN BOUNDARY CURRENTS. I: WIND-DRIVEN GENERAL CIRCULATION MODELMIURA H; SUGINOHARA N.1980; J. OCEANOGR. SOC. JAP.; JPN; DA. 1980; VOL. 35; NO 6; PP. 215-223; ABS. JAP; BIBL. 10 REF.Article

EVIDENCE FOR THE INFLUENCE OF FORM DRAG ON BOTTOM BOUNDARY LAYER FLOWCHRISS TM; CALDWELL DR.1982; J. GEOPHYS. RES.; ISSN 0022-1406; USA; DA. 1982; VOL. 87; NO C6; PP. 4148-4154; BIBL. 23 REF.Article

BENTHIC BOUNDARY-LAYER VELOCITY PROFILES: DEPENDENCE ON AVERAGING PERIODLESHT BM.1980; J. PHYSIC. OCEANOGR.; ISSN 0022-3670; USA; DA. 1980; VOL. 10; NO 6; PP. 985-991; BIBL. 12 REF.Article

INTERACTION BETWEEN THE MAGNETOSPHERIC BOUNDARY LAYERS AND THE IONOSPHEREVASYLIUNAS VM.1979; MAGNETOSPHERIC BOUNDARY LAYERS. SYDNEY CHAPMAN CONFERENCE/1979/ALPBACH; NLD; NOORDWIJK: ESA SCIENTIFIC AND TECHNICAL PUBLICATIONS BRANCH; DA. 1979; PP. 387-393; BIBL. 29 REF.Conference Paper

QUASI-THREE-DIMENSIONAL ANALYSIS OF A COMBUSTION MHD GENERATORSATYAMURTHY P; VENKATRAMANI N; ROHATGI VK et al.1982; ENERGY CONVERSION AND MANAGEMENT; ISSN 0196-8904; GBR; DA. 1982; VOL. 22; NO 3; PP. 243-250; BIBL. 13 REF.Article

VEINE LIMITE OCCIDENTALE DANS LE GOLFE DU BENGALESHCHERBININ AD; ARSEN'EV VS; GOL'DIN YU A et al.1979; DOKL. AKAD. NAUK S.S.S.R.; SUN; DA. 1979; VOL. 244; NO 4; PP. 987-989; BIBL. 5 REF.Article

EFFECTS OF A MARINE RIDGE TO WESTERN BOUNDARY CURRENT IN A THREE-DIMENSIONAL SOURCE-SINK FLOW MODELENDOH M.1978; J. OCEANOGR. SOC. JAP.; JPN; DA. 1978; VOL. 34; NO 6; PP. 303-306; ABS. JAP; BIBL. 3 REF.Article

STRONG WIND STRUCTURE NEAR A SEA-LAND ROUGHNESS DISCONTINUITYSACRE C.1981; BOUNDARY LAYER METEOROL.; NLD; DA. 1981; VOL. 21; NO 1; PP. 57-76; BIBL. 23 REF.Article

THE DISTRIBUTION OF DISSOLVED SILICA IN THE DEEP WESTERN NORTH ATLANTIC OCEANNEEDELL GJ.1980; DEEP-SEA RES., PART A, OCEANOGR. RES. PAP.; ISSN 0198-0149; USA; DA. 1980; VOL. 27; NO 11; PP. 941-950; BIBL. 14 REF.Article

Experimental study on neon isotope separation by DC arc dischargeSONE, T; AKATSUKA, H; SUZUKI, M et al.Journal of Nuclear Science and Technology. 1996, Vol 33, Num 5, pp 414-422, issn 0022-3131Article

A NUMERICAL STUDY OF DETACHED SHEAR LAYERS IN A ROTATING SLICED CYLINDERPAGE MA.1982; GEOPHYSICAL AND ASTROPHYSICAL FLUID DYNAMICS; ISSN 0309-1929; GBR; DA. 1982; VOL. 22; NO 1-2; PP. 51-69; BIBL. 14 REF.Article

Characteristics of the 22-year modulation of cosmic rays as seen by neutron monitorsWEBBER, W. R; LOCKWOOD, J. A.JGR. Journal of geophysical research. Part A, Space physics. 1988, Vol 93, Num 8, pp 8735-8740Article