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.
| Identifer | oai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.113727 |
| Date | January 1962 |
| Creators | Million, Herbert. A. |
| Contributors | Boville, B. (Supervisor) |
| Publisher | McGill University |
| Source Sets | Library and Archives Canada ETDs Repository / Centre d'archives des thèses électroniques de Bibliothèque et Archives Canada |
| Language | English |
| Detected Language | English |
| Type | Electronic Thesis or Dissertation |
| Format | application/pdf |
| Coverage | Master of Science. (Department of Earth Sciences.) |
| Rights | All items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated. |
| Relation | alephsysno: NNNNNNNNN, Theses scanned by McGill Library. |
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