Journal of Tropical Oceanography ›› 2026, Vol. 45 ›› Issue (1): 17-26.doi: 10.11978/2025034CSTR: 32234.14.2025034
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LIANG Zhanlin1,2(
), WANG Weiqiang1,2(
)
Received:2025-01-28
Revised:2025-03-03
Online:2026-01-10
Published:2026-01-30
Contact:
WANG Weiqiang. email: Supported by:CLC Number:
LIANG Zhanlin, WANG Weiqiang. Research progress on the characteristics of deep-sea circulation and water masses in the deep Eastern Indian Ocean*[J].Journal of Tropical Oceanography, 2026, 45(1): 17-26.
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Fig. 5
Schematic pattern of horizontal circulation in a rectangular basin (representing the CIB) driven by upwelling at the top of the layer, as forced by a source S on the eastern boundary (Warren, 1982). Light lines with arrowheads denote streamlines of the interior flow. Heavy lines indicate the northern-, southern-, and western-boundary currents, with adjacent arrows showing flow direction. The bundle of streamlines represents the zonal jet flowing westward from the source. The left side shows the volume transport of the western-boundary current varying with latitude (positive values indicate northward flow), measured in units of source-strength S"
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