Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7808
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dc.contributor.authorallMilliff, R. F.en
dc.contributor.authorallBonazzi, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.authorallWikle, C. K.en
dc.contributor.authorallPinardi, N.en
dc.contributor.authorallBerliner, L. M.en
dc.date.accessioned2012-02-22T14:34:32Zen
dc.date.available2012-02-22T14:34:32Zen
dc.date.issued2011en
dc.identifier.urihttp://hdl.handle.net/2122/7808en
dc.description.abstractA Bayesian hierarchical model (BHM) is developed to estimate surface vector wind (SVW) fields and associated uncertainties over the Mediterranean Sea. The BHM–SVW incorporates data-stage inputs from analyses and forecasts of the European Centre for Medium-Range Weather Forecasts (ECMWF) and SVW retrievals from the QuikSCAT data record. The process-model stage of the BHM–SVW is based on a Rayleigh friction equation model for surface winds. Dynamical interpretations of posterior distributions of the BHM–SVW parameters are discussed. Ten realizations from the posterior distribution of the BHM–SVW are used to force the data-assimilation step of an experimental ensemble ocean forecast system for the Mediterranean Sea in order to create a set of ensemble initial conditions. The sequential data-assimilation method of the Mediterranean forecast system (MFS) is adapted to the ensemble implementation. Analyses of sample ensemble initial conditions for a single data-assimilation period in MFS are presented to demonstrate the multivariate impact of the BHM–SVW ensemble generation methodology. Ensemble initial-condition spread is quantified by computing standard deviations of ocean state variable fields over the ten ensemble members. The methodological findings in this article are of two kinds. From the perspective of statistical modelling, the process-model development is more closely related tophysicalbalances than inpreviousworkwithmodels for the SVW.Fromthe ocean forecast perspective, the generation of ocean ensemble initial conditions via BHM is shown to be practical for operational implementation in an ensemble ocean forecast system. Phenomenologically, ensemble spread generated via BHM–SVW occurs on ocean mesoscale time- and space-scales, in close association with strong synoptic-scale wind-forcing events. A companion article describes the impacts of the BHM–SVW ensemble method on the ocean forecast in comparisons with more traditional ensemble methods.en
dc.language.isoEnglishen
dc.publisher.nameWiley-Blackwellen
dc.relation.ispartofQuarterly Journal of the Royal Meteorological Societyen
dc.relation.ispartofseries/137 (2011)en
dc.subjectQuikSCAT surface windsen
dc.titleOcean ensemble forecasting. Part I: Ensemble Mediterranean winds from a Bayesian hierarchical modelen
dc.typearticleen
dc.description.statusPublisheden
dc.description.pagenumber858–878en
dc.subject.INGV03. Hydrosphere::03.01. General::03.01.05. Operational oceanographyen
dc.identifier.doi10.1002/qj.767en
dc.description.journalTypeJCR Journalen
dc.description.fulltextembargoed_20140501en
dc.relation.issn0035-9009en
dc.relation.eissn1477-870Xen
dc.contributor.authorMilliff, R. F.en
dc.contributor.authorBonazzi, A.en
dc.contributor.authorWikle, C. K.en
dc.contributor.authorPinardi, N.en
dc.contributor.authorBerliner, L. M.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.orcid0000-0003-4765-0775-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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