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Tides and long-term modulations in the Caribbean Sea

Tides and long-term modulations in the Caribbean Sea
Tides and long-term modulations in the Caribbean Sea
The tidal signal and its long-term variation in the Caribbean Sea is analyzed on the basis of hourly records from thirteen tide gauges five of which span more than 20 years. The seven larger tidal constituents are studied, namely the fortnightly term Mf, diurnal K1, O1, and P1, and semidiurnal M2, S2 and N2. The 18.61 year nodal modulation is clearly identifiable in almost all the examined constituents of lunar origin. However, its signal in M2 is less clear while it is almost imperceptible in N2, where the 8.85 year cycle caused by the eccentricity of the Moon's orbit and the orientation of its major axis variation dominates the long-term variability. The effect of the nodal variation in the amplitude and phase lag of the various tidal constituents is in agreement (within the 95% error limits) with the theoretical gravitational estimate, with the exception of the 8.85 year cycle in N2, where larger values are found. Overall, in the Caribbean the net effect of the low frequency cycles can change the maximum tidal range from 16.5% to 23.5% in a nodal cycle. Although the Caribbean is a micro-tidal environment this still results in changes of the range of up to 8.4 cm. Significant, spatially coherent trends are found for the amplitude of S2 (2.3 to 8.8 mm/cy.
0148-0227
C10022
Torres, R. Ricardo
d37085fe-b6e3-4d6f-a1a2-6daeb88c2fb4
Tsimplis, Michael N.
df6dd749-cda4-46ec-983c-bf022d737031
Torres, R. Ricardo
d37085fe-b6e3-4d6f-a1a2-6daeb88c2fb4
Tsimplis, Michael N.
df6dd749-cda4-46ec-983c-bf022d737031

Torres, R. Ricardo and Tsimplis, Michael N. (2011) Tides and long-term modulations in the Caribbean Sea. Journal of Geophysical Research, 116 (C10), C10022. (doi:10.1029/2011JC006973).

Record type: Article

Abstract

The tidal signal and its long-term variation in the Caribbean Sea is analyzed on the basis of hourly records from thirteen tide gauges five of which span more than 20 years. The seven larger tidal constituents are studied, namely the fortnightly term Mf, diurnal K1, O1, and P1, and semidiurnal M2, S2 and N2. The 18.61 year nodal modulation is clearly identifiable in almost all the examined constituents of lunar origin. However, its signal in M2 is less clear while it is almost imperceptible in N2, where the 8.85 year cycle caused by the eccentricity of the Moon's orbit and the orientation of its major axis variation dominates the long-term variability. The effect of the nodal variation in the amplitude and phase lag of the various tidal constituents is in agreement (within the 95% error limits) with the theoretical gravitational estimate, with the exception of the 8.85 year cycle in N2, where larger values are found. Overall, in the Caribbean the net effect of the low frequency cycles can change the maximum tidal range from 16.5% to 23.5% in a nodal cycle. Although the Caribbean is a micro-tidal environment this still results in changes of the range of up to 8.4 cm. Significant, spatially coherent trends are found for the amplitude of S2 (2.3 to 8.8 mm/cy.

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Published date: 2011
Organisations: Marine Physics and Ocean Climate

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Local EPrints ID: 203009
URI: http://eprints.soton.ac.uk/id/eprint/203009
ISSN: 0148-0227
PURE UUID: a23ee956-fa3b-4709-8a51-7d9e81cdf46b

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Date deposited: 10 Nov 2011 14:52
Last modified: 14 Mar 2024 04:26

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Contributors

Author: R. Ricardo Torres
Author: Michael N. Tsimplis

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