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ECHANGE DE MASSE A LA FRONTIERE LIQUIDE D'UN COURANT DE FOND STRATIFIEPYRKIN YU G; SAMOLYUBOV BI; BELOSHAPKOV AV et al.1983; OKEANOLOGIJA; ISSN 0030-1574; SUN; DA. 1983; VOL. 23; NO 1; PP. 74-79; ABS. ENG; BIBL. 22 REF.Article

ENTRAINMENT BY BOTTOM CURRENTS IN LAKE ERIEIVEY GN; BOYCE FM.1982; LIMNOLOGY AND OCEANOGRAPHY; ISSN 0024-3590; USA; DA. 1982; VOL. 27; NO 6; PP. 1029-1038; BIBL. 11 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

ON DEEP MEAN FLOW GENERATION MECHANISMS AND THE ABYSSAL CIRCULATION OF NUMERICAL MODEL GYRESHARRISON DE.1982; DYN. ATMOS. OCEANS; ISSN 0377-0265; NLD; DA. 1982; VOL. 6; NO 3; PP. 135-152; BIBL. 21 REF.Article

THE EFFECT OF JET FORMATION ON THE VELOCITY DISTRIBUTION IN OSCILLATORY FLOW OVER FLAT BEDS OF SAND OR GRAVELSLEATH JFA.1982; COAST. ENG.; ISSN 0378-3839; NLD; DA. 1982; VOL. 6; NO 2; PP. 151-177; BIBL. 17 REF.Article

Radiolarian occurrences in surface sediments of the Indian ocean in relation to Bottom Water circulationSHARMA, V; MAHAPATRA, A. K.Journal of the Geological Society of India. 1990, Vol 35, Num 3, pp 251-261, issn 0016-7622, 11 p.Article

Bottom-current pathways in the Argentine Basin revealed by mean silt particle size = Type des courants de fond dans le Bassin Argentin d'après les données de dimension moyenne des particules de siltLEDBETTER, M. T.Nature (London). 1986, Vol 321, Num 6068, pp 423-425, issn 0028-0836Article

Pouzitie radioindikatorov k stanoveniu prudenia na hydraulickych modeloch = Le contrôle des courants dans les modèles hydrauliques par les traceurs radio-actifsMAYER, J; BRACHTL, I; DEMSKY, L et al.Vodní hospodářství (1990). 1990, Vol 40, Num 6, pp 234-237, issn 0862-5549, 4 p.Article

On the tectonic evolution and paleocanographic significance of the Fram Strait gatewayKRISTOFFERSEN, Y.NATO advanced research workshop on geological history of the Polar Oceans : Arctic versus Antarctic. 1990, pp 63-76, 14 p.Conference Paper

A lee wave model for deep-sea mudwave activity = Un modèle d'onde se formant à l'aval d'une ride pour représenter l'activité des ondes de boue en milieu marin profondFLOOD, R. D.Deep-sea research. Part A. Oceanographic research papers. 1988, Vol 35, Num 6, pp 973-983, issn 0198-0149Article

CORRELATION BETWEEN SURFACE GULF-STREAM AND BOTTOM FLOW NEAR 5000 METERS DEPTHKELLEY EA; WEATHERLY GL; EVANS JC et al.1982; JOURNAL OF PHYSICAL OCEANOGRAPHY; ISSN 0022-3670; USA; DA. 1982; VOL. 12; NO 10; PP. 1150-1153; BIBL. 14 REF.Article

Issledovanie i primenenie avtomodel'nykh svojstv pridonnogo stratifitsirovannogo potokaSAMOLYUBOV, B. I.Meteorologiâ i gidrologiâ. 1986, Num 1, pp 83-93, issn 0130-2906Article

NEAR-BOTTOM CURRENT MEASURED BY ACOUSTIC SENSORSSELANGER KA; CARSTENS T.1980; VASSDRAGS-OG HAVNELAB. MEDD.; NOR; DA. 1980; NO 19; PP. 181-200; BIBL. 3 REF.Article

ON DENSE BOTTOM CURRENTS IN THE BALTIC DEEP WATER.PEDERSEN FB.1977; NORD. HYDROL.; DANM.; DA. 1977; VOL. 8; NO 5; PP. 297-316; BIBL. 1 P. 1/2Article

Strömungen im Bodensee = Les courants dans le Lac de Constance = Current measurement in Lake ConstanceHOLLAN, E.Wasserwirtschaft. 1984, Vol 74, Num 7-8, pp 366-373, issn 0043-0978Article

The concept of deep-sea contourites. Discussion. Author's replyFRIEDMAN, G. M; HOLLISTER, C. D.Sedimentary geology. 1994, Vol 88, Num 3-4, pp 301-306, issn 0037-0738Article

A BOOMERANG TYPE BUOY FOR MEASUREMENT OF NEAR BOTTOM CURRENTS IN THE DEEP OCEAN.CLOSSER DR.1975; IN: OCEAN 75. IEEE CONF. ENG. OCEAN ENVIRON. MAR. TECHNOL. SOC. ANNU. MEET. 11; SAN DIEGO, CALIF.; 1975; NEW YORK; IEEE; DA. 1975; PP. 39-43Conference Paper

Erosion and slope instability on Horizon Guyot, Mid-Pacific Mountains = Erosion et instabilité des versants du guyot Horizon, Monts du Pacifique CentralSCHWAB, W. C; LEE, H. J; KAYEN, R. E et al.Geo-marine letters. 1988, Vol 8, Num 1, pp 1-10, issn 0276-0460Article

Dynamics of bottom currents in a small lake = Dynamique des courants de fond dans un petit lacLEMMIN, U; IMBODEN, D. M.Limnology and oceanography. 1987, Vol 32, Num 1, pp 62-75, issn 0024-3590Article

Side-scan targets in lake Superior ― evidence for bedforms and sediment transport = Signaux de vision latérale dans le lac Supérieur ― mise en évidence de configuration du fond du lac et du transport de sédimentFLOOD, R. D; JOHNSON, T. C.Sedimentology. 1984, Vol 31, Num 3, pp 311-333, issn 0037-0746Article

The TiO2/Al2O3 ratio in the Cenozoic Bengal Abyssal Fan sediments and its use as a paleostream energy indicator = Rapport TiO2/Al2O3 dans les sédiments cénozoïques du cône abyssal du Bengale et son utilisation en tant qu'indicateur d'énergie de paléorivièreSCHMITZ, B.Marine geology. 1987, Vol 76, Num 3-4, pp 195-206, issn 0025-3227Article

Facies distribution and textural variation in Faro Drift contourites: velocity fluctuation and drift growth = Répartition de faciès et variation de texture dans les contourites Faro Drift: fluctuation de la vitesse et croissance de la dériveSTOW, D. A. V; FAUGERES, J.-C; GONTHIER, E et al.Marine geology. 1986, Vol 72, Num 1-2, pp 71-100, issn 0025-3227Article

Long-term photographic, current, and nephelometer observations of manganese nodule environments in the Pacific = Observations photographiques du courant et à l'aide d'un néphélomètre sur une longue période des milieux à nodules de manganèse dans le PacifiqueGARDNER, W. D; SULLIVAN, L. G; THORNDIKE, E. M et al.Earth and planetary science letters. 1984, Vol 70, Num 1, pp 95-109, issn 0012-821XArticle

Observations of bottom intensification of temperature and velocity fluctuations induced by oblique tidal interactions with a slopeANTENUCCI, Jason P; IVEY, Gregory N.Marine and freshwater research. 2006, Vol 57, Num 3, pp 255-263, issn 1323-1650, 9 p.Article

L'évolution de l'hydrologie de la mer d'Alboran et ces courants de contour (veine d'eau méditerranéenne) dans le golfe de Cadix au Quaternaire récent : Apports des modèles physiquesPOUTIERS, J; FAUGERES, J.-C.Bulletin de la Société géologique de France. 1987, Vol 3, Num 5, pp 899-911, issn 0037-9409Conference Paper

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