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THE LOWER ST. LAWRENCE ESTUARY AS A PHYSICAL OCEANOGRAPHIC SYSTEM.EL SABH MI.sdIN: SOC. METEOROL. CAN. CONGR. ANNU. 10; QUEBEC; 1976; S.L.; DA. S.D.; PP. (2P.)Conference Paper

COMMENT ON "CHARACTERISTICS OF A TIDE-INDUCED ESTUARINE FRONT" BY R. GRANT INGRAM. REPLY.GERARD R; INGRAM RG.1977; J. GEOPHYS. RES.; U.S.A.; DA. 1977; VOL. 82; NO 6; PP. 995-996; BIBL. DISSEM.Article

CALIBRATION OF ESTUARINE CURRENT CROSSESKJERFVE B.1982; ESTUARINE, COASTAL AND SHELF SCIENCE; ISSN 0272-7714; GBR; DA. 1982; VOL. 15; NO 5; PP. 553-559; BIBL. 6 REF.Article

ESTUARY CIRCULATION. ASSESSMENT AND APPLICATIONCOLLAR RHF.1978; PROC. R. SOC. EDINBURGH, B; GBR; DA. 1978; VOL. 76; NO 1-3; PP. 37-54; BIBL. 18 REF.Conference Paper

INVESTIGATIONS ON DISSOLVED URANIUM, SILICON AND ON PARTICULATE TRACE ELEMENTS IN ESTUARIES.BOROLE DV; KRISHNASWAMI S; SOMAYAJULU BLK et al.1977; ESTUAR. COAST. MAR. SCI.; G.B.; DA. 1977; VOL. 5; NO 6; PP. 743-754; BIBL. 29 REF.Article

A SEMI-IMPLICIT TWO-DIMENSIONAL MODEL OF ESTUARINE CIRCULATIONDONG PING WANG; KRAWITZ DW.1980; J. PHYS. OCEANOGR.; USA; DA. 1980; VOL. 10; NO 3; PP. 441-454; BIBL. 21 REF.Article

ON THE EFFECT OF BAROTROPIC CURRENT FLUCTUATIONS ON THE TWO-LAYER TRANSPORT CAPACITY OF A CONSTRICTION.STIGEBRANDT A.1977; J. PHYS. OCEANOGR.; U.S.A.; DA. 1977; VOL. 7; NO 1; PP. 118-122; BIBL. 6 REF.Article

MODELLING METHODS FOR UNSTEADY FLOWS.MCDOWELL DM.1976; IN: INT. SYMP. UNSTEADY FLOW OPEN CHANNELS. PROC.; NEWCASTLE-UPON-TYNE; 1976; CRANFIELD, BEDFORD; BHRA FLUID ENG.; DA. 1976; PP. B.1-B.10; BIBL. 15 REF.Conference Paper

SIMULATION ELECTRIQUE DU MOUVEMENT NON PERMANENT DE L'EAU DANS UN ESTUAIREMAKAROV VA.1974; ARKTICH. ANTARKTICH. NAUCHNO-ISSLEDOVAT. INST., TRUDY, LENINGRAD; S.S.S.R.; DA. 1974; VOL. 308; PP. 20-27; BIBL. 13 REF.Article

RESULTAT DE L'ETUDE DES COURANTS DANS L'EMBOUCHURE DE L'ENISEI DURANT L'ETE ET L'AUTOMNEGRAEVSKIJ AP; KOTREKHOV EP; MATVEEV AA et al.1980; TRUDY ARKTICH. ANTARKTICH. NAUCHNO-ISSLEDOVAT. INST., LENINGRAD; SUN; DA. 1980; NO 358; PP. 54-74; BIBL. 7 REF.Article

BATHYMETRY AS AN INDICATOR OF NET CIRCULATION IN WELL MIXED ESTUARIESKJERFVE B.1978; LIMNOL. AND OCEANOGR.; USA; DA. 1978; VOL. 23; NO 4; PP. 816-821; BIBL. 13 REF.Article

A MECHANISM GOVERNING THE ESTUARINE CIRCULATION IN DEEP, STRONGLY STRATIFIED FJORDSSTIGEBRANDT A.1981; ESTUAR. COAST. SHELF SCI.; ISSN 502944; GBR; DA. 1981; VOL. 13; NO 2; PP. 197-211; BIBL. 16 REF.Article

SALINITY INDUCED HORIZONTAL ESTUARINE CIRCULATION.ELLIOTT BA; REID RO.1976; PROC. AMER. SOC. CIV. ENGRS, J. WATERWAYS HARBORS COAST. ENGNG DIV.; U.S.A.; DA. 1976; VOL. 102; NO 4; PP. 425-442; BIBL. 25 REF.Article

A NOTE ON ESTUARINE MEAN FLOW ESTIMATION.WEISBERG RH.1976; J. MAR. RES.; U.S.A.; DA. 1976; VOL. 34; NO 3; PP. 387-394; BIBL. 13 REF.Article

ETUDE DU MATERIEL PARTICULAIRE EN SUSPENSION DANS L'ESTUAIRE MARITIME DU SAINT-LAURENT. 1. TAILLE, CONCENTRATION ET BIOMASSE.POULET SA; COSSA D; MARTY JC et al.sdIN: SOC. METEOROL. CAN. CONGR. ANNU. 10; QUEBEC; 1976; S.L.; DA. S.D.; PP. (2P.)Conference Paper

A SIMPLE THEORETICAL MODEL FOR THE FLOW OF AN ESTUARY ONTO A CONTINENTAL SHELF.BEARDSLEY RC; HART J.1978; J. GEOPHYS. RES.; U.S.A.; DA. 1978; VOL. 83; NO 2; PP. 873-883; ABS. 10 REF.Article

NUMERICAL MODEL OF ESTUARINE CIRCULATION.BLUMBERG AF.1977; PROC. AMER. SOC. CIV. ENGRS, J. HYDRAUL. DIV.; U.S.A.; DA. 1977; VOL. 103; NO 3; PP. 295-310; BIBL. 19 REF.Article

EVALUATION OF CIRCULATION IN ESTUARIES.ABOOD KA; BOURODIMOS EL.1976; PROC. AMER. SOC. CIV. ENGRS, J. HYDRAUL. DIV.; U.S.A.; DA. 1976; VOL. 102; NO 9; PP. 1211-1224; BIBL. 23 REF.Article

MODELE NUMERIQUE DE CIRCULATION DES EAUX DANS LA PARTIE MARITIME D'UN ESTUAIRE, COMPTE TENU DES EFFETS DU DEBIT, ET DES FLUX THERMIQUE ET IONIQUEMOLCHANOV VN.1976; ARKTICH. ANTARKTICH. NAUCHNO-ISSLEDOVAT. INST., TRUDY, LENINGRAD; S.S.S.R.; DA. 1976; NO 314; PP. 36-43; BIBL. 9 REF.Article

ESTUARINE GEODYNAMICS IN AN AREA OF HIGH TIDAL RANGE.PATTON GD.1975; GEOL. SURV. CANADA, PAPER; CANADA; DA. 1975; NO 1, PART. A; PP. 161-162Article

VELOCITY AVERAGING IN ESTUARIES CHARACTERIZED BY A LARGE TIDAL RANGE TO DEPTH RATIO. = VITESSE MOYENNE DU COURANT DANS LES ESTUAIRES CARACTERISES PAR UNE GRANDE ZONE DE MAREE PAR RAPPORT A LA PROFONDEURKJERFVE B.1975; ESTUAR. COAST. MAR. SCI.; G.B.; DA. 1975; VOL. 3; NO 3; PP. 311-323; BIBL. 17 REF.Article

ETUDE DU MATERIEL PARTICULAIRE EN SUSPENSION DANS L'ESTUAIRE MARITIME DU SAINT-LAURENT. II. COMPOSES ORGANIQUES.MARTY JC; POULET SA; COSSA D et al.sdIN: SOC. METEOROL. CAN. CONGR. ANNU. 10; QUEBEC; 1976; S.L.; DA. S.D.; PP. (2P.)Conference Paper

ETUDE DU MATERIEL PARTICULAIRE EN SUSPENSION DANS L'ESTUAIRE MARITIME DU SAINT-LAURENT. III. TENEURS EN METAUX TRACES.COSSA D; MARTY JC; POULET SA et al.sdIN: SOC. METEOROL. CAN. CONGR. ANNU. 10; QUEBEC; 1976; S.L.; DA. S.D.; PP. (2P.)Conference Paper

ETUDE DU FROTTEMENT EN LOIRE MARITIME.MAUVAIS JL; SALOMON JC.1974; HOUILLE BLANCHE; FR.; DA. 1974; NO 1-2; PP. 149-154; BIBL. 3 REF.; (EQUILIBRE DYN. ESTUAIRES. ASPECTS PHYS. ECOL. SOC. HYDROTECH. FR. COM. TECH. NO 98, C.R.; 1973)Conference Paper

THE INFLUENCE OF DENSITY VARIATIONS ON ESTUARINE TIDES AND CIRCULATIONS.BLUMBERG AF.1978; ESTUAR. COAST. MAR. SCI.; G.B.; DA. 1978; VOL. 6; NO 2; PP. 209-215; BIBL. 5 REF.Article

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