Dynamical seasonal climate prediction using an ocean-atmosphere coupled climate model developed in partnership between South Africa and the IRI

dc.contributor.authorBeraki, Asmerom Fissehatsion
dc.contributor.authorDeWitt, David G.
dc.contributor.authorLandman, Willem Adolf
dc.contributor.authorOlivier, Cobus
dc.date.accessioned2014-05-06T06:40:24Z
dc.date.available2014-05-06T06:40:24Z
dc.date.issued2014-02
dc.description.abstractThe recent increase in availability of high-performance computing (HPC) resources in South Africa allowed the development of an ocean–atmosphere coupled general circulation model (OAGCM). The ECHAM4.5-South African Weather Service (SAWS) Modular Oceanic Model version 3 (MOM3-SA) is the first OAGCM to be developed in Africa for seasonal climate prediction. This model employs an initialization strategy that is different from previous versions of the model that coupled the same atmosphere and ocean models. Evaluation of hindcasts performed with the model revealed that the OAGCM is successful in capturing the development and maturity of El Niño and La Niña episodes up to 8 months ahead. A model intercomparison also indicated that the ECHAM4.5-MOM3-SA has skill levels for the Niño-3.4 region SST comparable with other coupled models administered by international centers. Further analysis of the coupled model revealed that La Niña events are more skillfully discriminated than El Niño events. However, as is typical for OAGCM, the model skill was generally found to decay faster during the spring barrier. The analysis also showed that the coupled model has useful skill up to several-months lead time when predicting the equatorial Indian Ocean dipole (IOD) during the period spanning between the middle of austral spring and the start of the summer seasons, which reaches its peak in November. The weakness of the model in other seasons was mainly caused by the western segment of the dipole, which eventually contaminates the dipole mode index (DMI). The model is also able to forecast the anomalous upper air circulations, particularly in the equatorial belt, and surface air temperature in the Southern African region as opposed to precipitation.en_US
dc.description.librarianhb2014en_US
dc.description.sponsorshipThe Water Research Commission (WRC) and Applied Centre for Climate & Earth Systems Science (ACCESS).en_US
dc.description.urihttp://journals.ametsoc.org/en_US
dc.identifier.citationBeraki, AF, DeWitt, DG, Landman, WA & Olivier, C 2014, 'Dynamical seasonal climate prediction using an ocean-atmosphere coupled climate model developed in partnership between South Africa and the IRI', Journal of Climate, vol. 27, no. 4, pp. 1719-1741.en_US
dc.identifier.issn0894-8755 (print)
dc.identifier.issn1520-0442 (online)
dc.identifier.other10.1175/JCLI-D-13-00275.1
dc.identifier.urihttp://hdl.handle.net/2263/39708
dc.language.isoenen_US
dc.publisherAmerican Meteorological Societyen_US
dc.rights© 2014 American Meteorological Societyen_US
dc.subjectSeasonal forecastingen_US
dc.subjectCoupled modelsen_US
dc.subjectEnsemblesen_US
dc.subjectInterannual variabilityen_US
dc.subjectModel evaluationen_US
dc.subjectPerformanceen_US
dc.subjectNumerical weather predictionen_US
dc.subjectForecastingen_US
dc.titleDynamical seasonal climate prediction using an ocean-atmosphere coupled climate model developed in partnership between South Africa and the IRIen_US
dc.typePostprint Articleen_US

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