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dc.contributor.authorBackeberg, Bjørn C.eng
dc.contributor.authorBertino, Laurenteng
dc.contributor.authorJohannessen, Johnny A.eng
dc.date.accessioned2009-06-04T07:51:19Z
dc.date.available2009-06-04T07:51:19Z
dc.date.issued2009-06-02eng
dc.Publishedhttp://www.ocean-sci.net/5/173/2009/os-5-173-2009.pdfen
dc.identifier.issn1812-0784en_US
dc.identifier.urihttps://hdl.handle.net/1956/3290
dc.description.abstractA 4th order advection scheme is applied in a nested eddy-resolving Hybrid Coordinate Ocean Model (HYCOM) of the greater Agulhas Current system for the purpose of testing advanced numerics as a means for improving the model simulation for eventual operational implementation. Model validation techniques comparing sea surface height variations, sea level skewness and variogram analyses to satellite altimetry measurements quantify that generally the 4th order advection scheme improves the realism of the model simulation. The most striking improvement over the standard 2nd order momentum advection scheme, is that the southern Agulhas Current is simulated as a well-defined meandering current, rather than a train of successive eddies. A better vertical structure and stronger poleward transports in the Agulhas Current core contribute toward a better southwestward penetration of the current, and its temperature field, implying a stronger Indo-Atlantic inter-ocean exchange. It is found that the transport, and hence this exchange, is sensitive to the occurrences of mesoscale features originating upstream in the Mozambique Channel and southern East Madagascar Current, and that the improved HYCOMsimulation is well suited for further studies of these inter-actions.en_US
dc.language.isoengeng
dc.publisherCopernicus Publications on behalf of the European Geosciences Unionen_US
dc.relation.ispartofseriesOcean Scienceen
dc.relation.ispartofseries5(2), p. 173–190en
dc.subjectOceanographyeng
dc.subjectOcean modellingeng
dc.titleEvaluating two numerical advection schemes in HYCOM for eddy-resolving modelling of the Agulhas Currenten_US
dc.typeJournal article
dc.subject.nsiVDP::Matematikk og Naturvitenskap: 400nob


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