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Cited by 267

The DOI matches its Crossref record; 13 of the 13 references it cites were found in a registry or an index.

Observations of the flow in the Mozambique Channel

Open access
de Ruijter, Wilhelmus P. M., Ridderinkhof, Herman, Lutjeharms, Johann R. E., Schouten, Mathijs W., Veth, Cornelis·2002·Geophysical Research Letters

Abstract

During a recent research cruise to investigate the nature and continuity of the Mozambique Current, we observed that the flow in the Mozambique Channel is dominated by a train of large anti‐cyclonic eddies (diameters >300 km) that reach to the channel bottom and propagate southward. At a frequency of 4 per year they cause a net poleward transport of about 15 Sv (1 Sv = 10 6 m 3/s). In the deep sea, a Mozambique Undercurrent flows equatorward along the continental slope. Using a lowered acoustic Doppler current profiler maximum observed velocities are about 0.2 m/s around 2400 m with another current core around 1000 m. It carries about 5 Sv of intermediate (AAIW) and deep waters (NADW) of Atlantic origin into the Channel. Subsequently, the equatorward flowing AAIW is largely entrained by the eddies and, while mixing with intermediate water from the North Indian Ocean in the eddy core, returned to the Agulhas Retroflection region.

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Crossref · 10.1029/2001gl013714

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Metadata

Authors
de Ruijter, W. P. M., Ridderinkhof, H., Lutjeharms, J. R. E., Schouten, M. W., & Veth, C.
Venue
Geophysical Research Letters
Published
2002-05-15
Volume
29
Issue
10
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W1593094915
Cited by
267
References
13
FWCI
8.31
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: Observations of the flow in the Mozambique Channel. https://app.cochat.ai/papers/10.1029/2001gl013714
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de Ruijter, W. P. M., Ridderinkhof, H., Lutjeharms, J. R. E., Schouten, M. W., & Veth, C. (2002). Observations of the flow in the Mozambique Channel. Geophysical Research Letters. https://doi.org/10.1029/2001gl013714

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