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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

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A FINITE-ELEMENT SOLUTION PROCEDURE FOR THE INTERPOLATION OF CURRENT DATA IN COMPLEX REGIONSGALT JA.1980; J. PHYS. OCEANOGR.; ISSN 0022-3670; USA; DA. 1980; VOL. 10; NO 12; PP. 1984-1997; BIBL. 19 REF.Article

DENSITY-DIFFUSIVE MODEL OF THE NINETYEAST RIDGE CURRENTJOHNSON ES; WARREN BA.1979; J. PHYS. OCEANOGR.; USA; DA. 1979; VOL. 9; NO 6; PP. 1288-1293; BIBL. 3 REF.Article

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VOLUME TRANSPORT OF THE WESTERN BOUNDARY CURRENT PENETRATING INTO A MARGINAL SEAMINATO S; KIMURA R.1980; NIPPON KAIYO GAKKAI-SHI; ISSN 0029-8131; JPN; DA. 1980; VOL. 36; NO 4; PP. 185-195; ABS. JAP; BIBL. 6 REF.Article

THE EFFECT OF A LOCALIZED TOPOGRAPHIC IRREGULARITY ON THE FLOW OF A BOUNDARY CURRENT ALONG THE CONTINENTAL MARGINSHENN YU CHAO; JANOWITZ GS.1979; J. PHYS. OCEANOGR.; USA; DA. 1979; VOL. 9; NO 5; PP. 900-910; BIBL. 14 REF.Article

EFFECT OF A WESTERN BOUNDARY EDDY FIELD ON MID-OCEAN CIRCULATIONNIILER PP.1980; DYN. ATMOS. OCEANS; ISSN 0377-0265; NLD; DA. 1980; VOL. 5; NO 2; PP. 73-82; BIBL. 8 REF.Article

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