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Diurnal sea breeze effects on inner-shelf cross-shore exchange
- Source :
-
Continental Shelf Research . Oct2009, Vol. 29 Issue 18, p2195-2206. 12p. - Publication Year :
- 2009
-
Abstract
- Abstract: Cross-shore exchange by strong (cross-shore wind stress, τsx >0.05Pa) diurnal (7–25h) sea breeze events are investigated using two years of continuous wind, wave, and ocean velocity profiles in 13m water depth on the inner-shelf in Marina, Monterey bay, California. The diurnal surface wind stress, waves, and currents have spectral peaks at 1, 2, and 3cpd and the diurnal variability represents about 50% of the total variability. During sea breeze relaxation (−0.05<τsx <0.05Pa), a background wave-driven inner-shelf Eulerian undertow profile exists, which is equal and opposite to the Lagrangian Stokes drift profile, resulting in a net zero Lagrangian transport at depth. In the presence of a sea breeze (τsx >0.05Pa), a uniform offshore profile develops that is different from the background undertow profile allowing cross-shore Lagrangian transport to develop, while including Lagrangian Stokes drift. The diurnal cross-shore current response is similar to subtidal (>25h) cross-shore current response, as found by . The seasonality of waves and winds modify the diurnal sea breeze impact. It is suggested that material is not transported cross-shore except during sea breeze events owing to near zero transport during relaxation periods. During sea breeze events, cross-shore exchange of material appears to occur onshore near the surface and offshore near the sea bed. Since sea breeze events last for a few hours, the long-term cross-shore transport is incremental each day. [Copyright &y& Elsevier]
Details
- Language :
- English
- ISSN :
- 02784343
- Volume :
- 29
- Issue :
- 18
- Database :
- Academic Search Index
- Journal :
- Continental Shelf Research
- Publication Type :
- Academic Journal
- Accession number :
- 44699162
- Full Text :
- https://doi.org/10.1016/j.csr.2009.08.011