2006
DOI: 10.1016/s1001-6058(06)60046-2
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Application of a three-point explicit compact difference scheme to the incompressible navier-stokes equations

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“…The eddies are often observed as a long west-east band generated by shearing activity between the eastward-flowing Subtropical Countercurrent (STCC) and the westward-flowing North Equatorial Current (NEC) 24 . As a result of the beta planetary effect, the eddies move westward at a speed of approximately 0.1 m/s 2, 5, 6 . Seasonally, the eddies are more active in spring and summer than in other seasons 7 .…”
Section: Introductionmentioning
confidence: 99%
“…The eddies are often observed as a long west-east band generated by shearing activity between the eastward-flowing Subtropical Countercurrent (STCC) and the westward-flowing North Equatorial Current (NEC) 24 . As a result of the beta planetary effect, the eddies move westward at a speed of approximately 0.1 m/s 2, 5, 6 . Seasonally, the eddies are more active in spring and summer than in other seasons 7 .…”
Section: Introductionmentioning
confidence: 99%