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dc.contributor.authorRamp, Steven R.
dc.contributor.authorLermusiaux, Pierre F. J.
dc.contributor.authorShulman, Igor
dc.contributor.authorChao, Yi
dc.contributor.authorWolf, Rebecca E.
dc.contributor.authorBahr, Frederick L.
dc.date.accessioned2014-01-30T00:11:25Z
dc.date.available2014-01-30T00:11:25Z
dc.date.issued2011
dc.identifier.citationDynamics of Atmospheres and Oceans, 52, (2011), pp. 192-223
dc.identifier.urihttp://hdl.handle.net/10945/38647
dc.descriptiondx.doi.org/10.1016/dynatmoce.2011.04.005en_US
dc.description.abstractA comprehensive data set from the ocean and atmosphere was obtained just north of the Monterey Bay as part of the Monterey Bay 2006 (MB2006) field experiment. The wind stress, heat fluxes and sea surface temperature were sampled by the Naval Postgraduate's TWIN OTTER research aircraft. In situ data were collected using ships, moorings, gliders and AUVs. Four data-assimilating numerical models wre additinally run, including the Coupled Ocean/Atmosphere Mesoscale Prediction System (COAMPS) model for the atmosphere and the Harvard Ocean Prediction System (HOPS), the Regional Ocean Modeling System (ROMS) and the Navy Coastal Ocean Model(NCOM) for the ocean. The wcientific focus of the Adaptive Sampling and Prediction Experiment (ASAP) was on the upwelling/relaxation cycle and the resulting three-dimensinal coastal circulation near a coastal promontory, in this case Point Ano Nuevo, CA. The emphasis of this study is on the circulation over the continental shelf as estimated from the wind forcing, two ADCP moorings, and model outputs. The wind stress during August 2006 consisted of 3-10 day upwelling favorable events separated by brief 1-3 day relaxations. During the first two weeks there was some correlation between local winds and currents and the three models' capability to reproduce the events. During the last two weeks, largely equatorward surface wind stress forced ythe sea surface and barotropic poleward flow occurred over the shelf, reducing model skill at predicting the circulation. The poleward flow was apparently remotely forced by mesoscale eddies and alongshore pressure gradients, which were not well simulated by the models. The small, high-resolution model domains were highly reliant on correct open boundary conditions to drive these larger-scale poleward flows. Multiply-nested models were no more effective than well-initialized local models in this respect.en_US
dc.publisherElsevieren_US
dc.rightsThis publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. As such, it is in the public domain, and under the provisions of Title 17, United States Code, Section 105, may not be copyrighted.en_US
dc.titleOceanographic and atmospheric conditions on the continental shelf north of the Monterey Bay during August 2006en_US
dc.typeArticleen_US
dc.contributor.corporateNaval Postgraduate School
dc.subject.authorcoastal circulationen_US
dc.subject.authorair/sea interactionen_US
dc.subject.authorupwellingen_US
dc.subject.authorocean modeling and predictionen_US
dc.subject.authorUSA/West Coast/California/Monterey Bayen_US


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