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dc.contributor.authorHarr, Patrick A.
dc.contributor.authorAnwender, Doris
dc.contributor.authorJones, Sarah
dc.date.accessioned2015-08-13T22:30:05Z
dc.date.available2015-08-13T22:30:05Z
dc.date.issued2006
dc.identifier.urihttp://hdl.handle.net/10945/46045
dc.descriptionP6.7en_US
dc.description.abstractThe poleward movement of a decaying tropical cyclone (TC) often results in a rapidly-moving, explosively-deepening midlatitude cyclone. The re-intensification of the remnant TC as an extratropical cyclone depends on the phasing between the decaying TC and a midlatitude environment that is favorable for midlatitude cyclogenesis.en_US
dc.description.sponsorshipThis research has been sponsored by the Office of Naval Research, Marine Meteorology Program.en_US
dc.rightsThis publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States.en_US
dc.titlePredictability Associated with the Downstream Impacts of the Extratropical Transition (ET) of Tropical Cyclonesen_US
dc.typeArticleen_US
dc.contributor.departmentMeteorologyen_US


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