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A diagnostic study of the thermodynamic equation in rain/snow boundaries /

A diagnostic study using the CASP (Canadian Atlantic Storm Program) dataset and available precipitation data is performed to examine the thermodynamics of melting-induced mesoscale circulations. Various terms of the thermodynamic equation were evaluated. The horizontal and vertical advection terms were calculated using the rawinsonde data while the diabatic term due to melting was parameterized using surface precipitation observations. The effects of evaporation and dissipation were neglected in the calculation of the diabatic terms. The importance of the melting term was clearly shown although direct evidence of a melting-induced circulation was not found due to the relatively low resolution of the datasets used.

Identiferoai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.59593
Date January 1988
CreatorsJarrett, Philip Lionel
PublisherMcGill University
Source SetsLibrary and Archives Canada ETDs Repository / Centre d'archives des thèses électroniques de Bibliothèque et Archives Canada
LanguageEnglish
Detected LanguageEnglish
TypeElectronic Thesis or Dissertation
Formatapplication/pdf
CoverageMaster of Science (Department of Meteorology.)
RightsAll items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated.
Relationalephsysno: 001071653, proquestno: AAIMM63754, Theses scanned by UMI/ProQuest.

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