Mesoscale frontal evolution of the ERICA IOP-5A cyclone

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Naval Postgraduate School, Available from National Technical Information Service , Monterey, Calif, Springfield, Va About the Edition

A synoptic investigation was conducted of the rapid coastal cyclogenesis that occurred during Intensive Observation Period (IOP) 5A of the Experiment on Rapidly Intensifying Cyclones over the Atlantic (ERICA). Navy Operational Regional Analysis and Prediction System (NORAPS) forecasts were examined in order to study the mesoscale frontal evolution associated with this rapidly deepening coastal cyclone. The ability of the NORAPS forecasts to accurately depict the frontal positions and intensity was also investigated. The frontal evolution showed characteristics of a classical occlusion, similar to the Norwegian cyclone model and of marine frontal structure as discussed by Shapiro and Keyser (1990). The frontal evolution was highly influenced by the prior existanse of strong arctic and coastal fronts. These fronts intensified during the course of the storm development and did not develop as a result of the cyclogenesis.

StatementSteven R. Cameron
The Physical Object
Pagination74 p. ;
ID Numbers
Open LibraryOL25474646M

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Mesoscale frontal evolution of the ERICA IOP-5A Cyclone. Erica Iop 5A: Mesoscale Structure and Frontal Evolution [Timothy G.

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Thesis advisor(s): Carlyle H. Wash ; Paul A. Hirschberg. This banner text can have markup. The frontal evolution showed characteristics of a classical occlusion, similar to the Norwegian cyclone model and of marine frontal structure as discussed by Shapiro and Keyser ().

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In a numerical simulation of the ERICA (Experiment on Rapidly Intensifying Storms over the Atlantic) IOP 5A storm, the E-∈ parameterization provides an improved forecast of cyclone central pressure.

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