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dc.contributor.advisorKerry Emanuel.en_US
dc.contributor.authorGombos, Daniel (Daniel Lawrence)en_US
dc.contributor.otherMassachusetts Institute of Technology. Dept. of Earth, Atmospheric, and Planetary Sciences.en_US
dc.date.accessioned2009-10-01T15:50:48Z
dc.date.available2009-10-01T15:50:48Z
dc.date.copyright2009en_US
dc.date.issued2009en_US
dc.identifier.urihttp://hdl.handle.net/1721.1/47844
dc.descriptionThesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2009.en_US
dc.descriptionIncludes bibliographical references (p. 183-190).en_US
dc.description.abstractEnsemble regression (ER) is a linear inversion technique that uses ensemble statistics from atmospheric model output to make dynamical inferences and forecasts. ER defines a multivariate regression operator using ensemble forecasts and analyses to determine the most probable predict and perturbation associated with the prescribed predictor perturbation resolved by linear combinations of the predictor ensemble anomalies. Because it employs flow-dependent ensemble data, as opposed to the stationary time series data typically used to make statistical forecasts, ER is capable of modeling synoptic scale processes with rapidly evolving covariances. This characteristic is applied in several ways. Firstly, it is shown that the classical dynamical piecewise potential vorticity (PV) inversion of the PV perturbation effectively resolved by the ER operator yields nearly identical geopotential heights to those deduced from an ER performed in the subspace of the leading PV singular vectors. Secondly, using the example of the lagged sensitivity of tropical cyclone tracks to preexisting midtropospheric heights, ER is used to infer dynamical relationships from statistical sensitivities, to identify, in real-time, the dynamical processes that are particularly relevant to specific forecast decisions, and to make preemptive forecasts. Thirdly, it is shown that singular vectors deduced from the ER operator approximate those from the analysis error covariance normed tangent linear model operator, suggesting a simple alternative method for computing singular vectors. Given that ER results are a function of forecast ensemble reliability, theory and applications of a multivariate ensemble reliability verification technique called the minimum spanning tree rank histogram are presented.en_US
dc.description.abstract(cont.) Experiments using Euclidean, variance, and Mahalanobis norms for defining minimum spanning tree distances imply that, unless the number of ensemble members is less than or equal to the number of dimensions being verified, the Mahalanobis norm transforms a spanning tree into a space where model imperfections are most readily identified.en_US
dc.description.statementofresponsibilityby Daniel Gombos.en_US
dc.format.extent190 p.en_US
dc.language.isoengen_US
dc.publisherMassachusetts Institute of Technologyen_US
dc.rightsM.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission.en_US
dc.rights.urihttp://dspace.mit.edu/handle/1721.1/7582en_US
dc.subjectEarth, Atmospheric, and Planetary Sciences.en_US
dc.titleEnsemble regression : using ensemble model output for atmospheric dynamics and predictionen_US
dc.title.alternativeUsing ensemble model output for atmospheric dynamics and predictionen_US
dc.typeThesisen_US
dc.description.degreePh.D.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
dc.identifier.oclc430043035en_US


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