Surface effects of bottom-generated turbulence in a shallow tidal sea
Surface effects of bottom-generated turbulence in a shallow tidal sea
Turbulence in shelf seas strongly affects the spread of pollution (such as oil spills) as well as the distribution of sediment and phytoplankton blooms. Turbulence is known to be generated intermittently close to the sea bed, but little is known of its evolution through the water column, or to what extent it affects the surface. Here we present observations of the surface effects of bottom-generated turbulence in a tidally influenced and well mixed region of the North Sea, as derived from acoustic and visual images. Although the sea bed in the area is flat, we find that at any one time, 20–30% of the water surface is affected by boils—circular regions of local upwelling—of diameter 0.90.2 times the water depth. The signature of individual boils persists for at least 7 minutes and, in accordance with laboratory and numerical studies, shows the appearance of eddies. The boils contribute to the replacement of surface waters from depth in unstratified waters, and may therefore enhance the fluxes of gases between atmosphere and ocean.
251-253
Nimmo Smith, W.A.M.
403f4fad-2ab0-4156-b6cb-4122a5e1af8c
Thorpe, S.A.
8a8f3888-cf5e-4b0f-b1e7-4882989212ab
Graham, A.
e6591a0a-c11d-4436-8f5a-aebb09c97279
15 July 1999
Nimmo Smith, W.A.M.
403f4fad-2ab0-4156-b6cb-4122a5e1af8c
Thorpe, S.A.
8a8f3888-cf5e-4b0f-b1e7-4882989212ab
Graham, A.
e6591a0a-c11d-4436-8f5a-aebb09c97279
Nimmo Smith, W.A.M., Thorpe, S.A. and Graham, A.
(1999)
Surface effects of bottom-generated turbulence in a shallow tidal sea.
Nature, 400 (6741), .
(doi:10.1038/22295).
Abstract
Turbulence in shelf seas strongly affects the spread of pollution (such as oil spills) as well as the distribution of sediment and phytoplankton blooms. Turbulence is known to be generated intermittently close to the sea bed, but little is known of its evolution through the water column, or to what extent it affects the surface. Here we present observations of the surface effects of bottom-generated turbulence in a tidally influenced and well mixed region of the North Sea, as derived from acoustic and visual images. Although the sea bed in the area is flat, we find that at any one time, 20–30% of the water surface is affected by boils—circular regions of local upwelling—of diameter 0.90.2 times the water depth. The signature of individual boils persists for at least 7 minutes and, in accordance with laboratory and numerical studies, shows the appearance of eddies. The boils contribute to the replacement of surface waters from depth in unstratified waters, and may therefore enhance the fluxes of gases between atmosphere and ocean.
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Published date: 15 July 1999
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Local EPrints ID: 50814
URI: http://eprints.soton.ac.uk/id/eprint/50814
ISSN: 0028-0836
PURE UUID: d90d68fd-6a40-4be9-9a7f-65e3862a8198
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Date deposited: 02 Apr 2008
Last modified: 15 Mar 2024 10:12
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Author:
W.A.M. Nimmo Smith
Author:
S.A. Thorpe
Author:
A. Graham
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