An intercomparison of internal solitary waves in the Bay of Biscay and resulting from Korteweg-de Vries-Type theory
An intercomparison of internal solitary waves in the Bay of Biscay and resulting from Korteweg-de Vries-Type theory
A recently developed Korteweg-de Vries (KdV)-type theory is used to study the formation of internal ‘solitary’ waves from internal tides in the Bay of Biscay, and detailed comparisons are made with observations. The theory is for a continuously-stratified fluid, and includes both first order non-linearity and dispersion, as well as the earth's rotation without restriction at the lowest order. We investigate and compare the detailed structure of the waves, paying particular attention to the horizontal and vertical velocity fields, as well as to the more usual characteristics, since it appears this has not been undertaken before. The comparison shows that the simplified but often-used ‘KdV physics’ is able to reproduce almost all features of the observed solitary waves, such as wavelengths, amplitudes, phase speeds, and horizontal velocity structure, with reasonable success. The magnitude of the vertical velocities, however, is significantly underestimated by the theory, although their qualitative structure is reproduced. The comparison also indicates that the internal solitary waves in nature are likely to produce significant mixing of the seasonal thermocline.
BISCAY BAY, INTERNAL WAVES, SOLITARY WAVES, INTERNAL TIDES, MATHEMATICAL MODELS
1-38
New, A.L.
69c2be8b-c6c2-408f-9612-6980b1a25802
Pingree, R.D.
ca54a28e-f3b8-4846-86eb-eafb37527e5f
2000
New, A.L.
69c2be8b-c6c2-408f-9612-6980b1a25802
Pingree, R.D.
ca54a28e-f3b8-4846-86eb-eafb37527e5f
New, A.L. and Pingree, R.D.
(2000)
An intercomparison of internal solitary waves in the Bay of Biscay and resulting from Korteweg-de Vries-Type theory.
Progress in Oceanography, 45 (1), .
(doi:10.1016/S0079-6611(99)00049-X).
Abstract
A recently developed Korteweg-de Vries (KdV)-type theory is used to study the formation of internal ‘solitary’ waves from internal tides in the Bay of Biscay, and detailed comparisons are made with observations. The theory is for a continuously-stratified fluid, and includes both first order non-linearity and dispersion, as well as the earth's rotation without restriction at the lowest order. We investigate and compare the detailed structure of the waves, paying particular attention to the horizontal and vertical velocity fields, as well as to the more usual characteristics, since it appears this has not been undertaken before. The comparison shows that the simplified but often-used ‘KdV physics’ is able to reproduce almost all features of the observed solitary waves, such as wavelengths, amplitudes, phase speeds, and horizontal velocity structure, with reasonable success. The magnitude of the vertical velocities, however, is significantly underestimated by the theory, although their qualitative structure is reproduced. The comparison also indicates that the internal solitary waves in nature are likely to produce significant mixing of the seasonal thermocline.
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Published date: 2000
Keywords:
BISCAY BAY, INTERNAL WAVES, SOLITARY WAVES, INTERNAL TIDES, MATHEMATICAL MODELS
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Local EPrints ID: 8787
URI: http://eprints.soton.ac.uk/id/eprint/8787
ISSN: 0079-6611
PURE UUID: f7999a4c-aae6-4103-8c83-a80dee6a13e2
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Date deposited: 13 Sep 2004
Last modified: 15 Mar 2024 04:52
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Author:
A.L. New
Author:
R.D. Pingree
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