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dc.contributor.authorTokmakian, R.
dc.date.accessioned2014-08-27T16:18:25Z
dc.date.available2014-08-27T16:18:25Z
dc.date.issued2005
dc.identifier.citationOcean Modeling, Volume 9, pp. 89-103, 2005.
dc.identifier.urihttp://hdl.handle.net/10945/43117
dc.descriptionThe article of record as published may be located at http://dx.doi.org/10.1016/j.ocemod.2004.04.005en_US
dc.description.abstractTwo simulations of the North Atlantic have been run using the POP ocean model for approximately two and one half years each. One simulation used the 1.25 wind product from ECMWF and the other used the JPL Quikscat 0.25 gridded product. The resulting sea level anomaly fields from the simulations are quantified by using tide gauge and altimetric sea level anomaly data. In addition, upper ocean quantities were compared, such as the mix layer depths, to understand the difference in the ocean’s response when using the different wind products. The analysis found that significant improvements were made in the representation at the surface, and in particular areas where comparison data exists such as the Labrador Sea. There was also improvement in the scatterometer forced run with more realistic depths of the mixed layer.en_US
dc.rightsThis publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States.en_US
dc.titleAn ocean model’s response to scatterometer windsen_US
dc.typeArticleen_US
dc.contributor.departmentOceanography
dc.subject.authorNorth Atlanticen_US
dc.subject.authorModelingen_US
dc.subject.authorScatterometryen_US
dc.subject.authorAltimetryen_US
dc.subject.authorSea levelen_US
dc.subject.authorUpper ocean processesen_US


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