dc.creatorDotto, T S
dc.creatorKerr, R
dc.creatorMata, M M
dc.creatorAzaneu, M
dc.creatorWainer, Ilana Elazari Klein Coaracy
dc.creatorFahrbach, E
dc.creatorRohardt, G
dc.date.accessioned2014-10-23T21:35:12Z
dc.date.accessioned2018-07-04T16:54:52Z
dc.date.available2014-10-23T21:35:12Z
dc.date.available2018-07-04T16:54:52Z
dc.date.created2014-10-23T21:35:12Z
dc.date.issued2014
dc.identifierhttp://www.producao.usp.br/handle/BDPI/46437
dc.identifierdoi:10.5194/os-10-523-2014
dc.identifierwww.ocean-sci.net/10/523/2014/
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/1642100
dc.description.abstractWe assessed and evaluated the performance of five ocean reanalysis products in reproducing essential hydrographic properties and their associated temporal variability for the Weddell Sea, Antarctica. The products used in this assessment were ECMWF ORAS4 (European Centre for Medium-Range Weather Forecasts Ocean Reanalysis System 4), CFSR (Climate Forecast System Reanalysis), My- Ocean UR025.4 (University of Reading), ECCO2 (Estimating the Circulation and Climate of the Ocean, Phase II) and SODA (Simple Ocean Data Assimilation). The present study focuses on the Weddell Sea deep layer, which is composed of the following three main water masses: Warm Deep Water (WDW),Weddell Sea DeepWater (WSDW) andWeddell Sea Bottom Water (WSBW). The MyOcean UR025.4 product provided the most accurate representation of the structure and thermohaline properties of theWeddell Sea water masses when compared with observations. All the ocean reanalysis products analyzed exhibited limited capabilities in representing the surface water masses in the Weddell Sea. The CFSR and ECCO2 products were not able to represent deep water masses with a neutral density_28.40 kgm−3, which was considered the WSBW’s upper limit throughout the simulation period. The expected WDW warming was only reproduced by the SODA product, whereas the ECCO2 product was able to represent the trends in the WSDW’s hydrographic properties. All the assessed ocean reanalyses were able to represent the decrease in the WSBW’s density, except the SODA product in the inner Weddell Sea. Improvements in parameterization may have as much impact on the reanalyses assessed as improvements in horizontal resolution primarily because the Southern Ocean lacks in situ data, and the data that are currently available are summer-biased. The choice of the reanalysis product should be made carefully, taking into account the performance, the parameters of interest, and the type of physical processes to be evaluated
dc.languageeng
dc.relationOcean Science, 10, 523–546, 2014
dc.rightsrestrictedAccess
dc.subjectSea water
dc.subjectAntarctica
dc.subjectwater masses
dc.subjectWeddell Sea
dc.titleAssessment of the structure and variability ofWeddell Sea water masses in distinct ocean reanalysis products
dc.typeArtículos de revistas


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