Effects of sloping bottom on the deep cross-equatorial boundary current

Wu De-xing; Lü Hong-min; Guo Qun; Lu Zhen

doi:10.1007/BF02850585

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Effects of sloping bottom on the deep cross-equatorial boundary current

OriginalPaper | Updated：2023-05-16

- Effects of sloping bottom on the deep cross-equatorial boundary current
- Effects of sloping bottom on the deep cross-equatorial boundary current
- 海洋湖沼学报（英文） 1997年15卷第1期页码：65-69
- Affiliations：
  
  Institute of Physical Oceanography
- Author bio：
- Funds：
  
  This research was supported by the NSFC and State Oceanic Administration (No. 49276267).
- DOI：10.1007/BF02850585
  中图分类号：
- 纸质出版：1997
- Accepted：
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Effects of sloping bottom on the deep cross-equatorial boundary current[J]. 海洋湖沼学报（英文）, 1997,15(1):65-69.

De-xing, W., Hong-min, L., Qun, G. et al. Effects of sloping bottom on the deep cross-equatorial boundary current., Chin. J. Ocean. Limnol. 15, 65–69 (1997). https://doi.org/10.1007/BF02850585
Effects of sloping bottom on the deep cross-equatorial boundary current[J]. 海洋湖沼学报（英文）, 1997,15(1):65-69. DOI： 10.1007/BF02850585.

De-xing, W., Hong-min, L., Qun, G. et al. Effects of sloping bottom on the deep cross-equatorial boundary current., Chin. J. Ocean. Limnol. 15, 65–69 (1997). https://doi.org/10.1007/BF02850585 DOI：

摘要

Abstract

This paper reports study focusing on the effects of sloping bottom on the deep cross-equatorial boundary current

and discusses model and laboratory experiment results showing that the southward intrusion distance and flow speed of the western boundary current depend on the bottom slope variation rate

the difference between {ie65-1} and {ie65-2} ({ie65-3} and {ie65-4} are the current thickness at eastward edge and westward edge

respectively)

and the net mass transport.

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references

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Kawase, M., Straub, D. N., 1991. Spin up of source-driven circulation in an abyssal basin in the presence of bottom topography.J. Phys. Oceanogr. 21: 1501–1541.

Killworth, P. D., 1991. Cross-equatorial geostrophic adjustment.J. Phys. Oceanogr.21: 1581–1601.

McCartney, M. S., 1993. Crossing of the equator by the deep western boundary current in the Western Atlantic Ocean.J. Phys. Oceanogr. 23: 1953–1974.

Nof, D., 1990. Why are some boundary currents blocked by the equator?Deep Sea Res. 37: 853–873.

Richardson, P. L., Schmitz, Jr. W. J., 1993. Deep cross-equatorial flow in the Atlantic measured with SOFAR flcats.J. Geophys. Res. 98: 8371–8387.

Straub, D. N., Rhines, P. B., 1990. Effects of large scale topography on abyssal circulation.J. Mar. Res. 48: 223–253.

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