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A study of the thermal structure of jet stream wind maxima.

A synoptic and dynamic investigation of the jet stream reveals that in a transverse profile the maximum wind tends to lie along a pseudo-parabolic rather than a horizontal surface. The upwardfacing parabola is identified by a band of warm temperatures on the cyclonic side of the jet core and a band of cold temperatures on the anticyclonic side. The model is shown to be compatible with the thermal wind relationship.

Identiferoai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.113727
Date January 1962
CreatorsMillion, Herbert. A.
ContributorsBoville, B. (Supervisor)
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 Earth Sciences.)
RightsAll items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated.
Relationalephsysno: NNNNNNNNN, Theses scanned by McGill Library.

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