Free Content The effects of flow disturbance by an oceanic island

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Abstract:

We present CTD and ADCP surveys around the Indian Ocean coral atolls of Aldabra (46°20′E, 9°25′S) and Cosmoledo (47°30E, 9°45′S) during April–July 1987. These isolated, steep-sided islands situated in deep (4000 m) water in the South Equatorial Current provide examples of flow disturbance which are compared to laboratory studies of eddy generation by a circular cylinder in a channel.

For sufficiently strong and steady flows, a doming of the isopycnals is observed in the lee of the islands. The sea-surface temperature decreases and the salinity increases as cool, saline water is mixed from below. Just as in the case of islands in tidally dominated shelf seas, we observe an increase in the chlorophyll content of the water behind the island, indicative of enhanced phytoplankton productivity caused by the flow disturbance. This anomalous region may be associated with an eddy trapped downstream of the island. The incident flows were not strong enough to generate a vortex street of eddies spun off in a wake. When the incident flows are weak and fluctuating, no evidence for eddies is seen; and there is no doming of the isopycnals leading to low sea-surface temperature and high chlorophyll content.

Document Type: Research Article

DOI: http://dx.doi.org/10.1357/002224090784984623

Publication date: February 1, 1990

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  • The Journal of Marine Research publishes peer-reviewed research articles covering a broad array of topics in physical, biological and chemical oceanography. Articles that deal with processes, as well as those that report significant observations, are welcome. In the area of biology, studies involving coupling between ecological and physical processes are preferred over those that report systematics. Authors benefit from thorough reviews of their manuscripts, where an attempt is made to maximize clarity. The time between submission and publication is kept to a minimum; there is no page charge.
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