Research Article

A Short Surface Pathway of the Subsurface Indonesian Throughflow Water from the Java Coast Associated with Upwelling, Ekman Transport, and Subduction

Figure 7

(a) OGCM zonal current at a location close to the south Java coast and (b) corresponding observations from Sprintall et al. [18]. The shade shows the eastward current and the pattern shows the westward current. (c) The horizontal shelf velocity (shade) and vertical velocity (contour) resolved in OGCM. Positive shade, contour means an eastward, upward velocity, respectively.
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