From an analysis of the flow over and around the Himalayas during the high summers of 1958 and 1959, it is deduced that the large-scale upper air patterns have significant effects on the surface circulation. The effect of the plateau (due to surface heating) is to induce a surface cyclonic circulation which is however often subdued by dynamic effeets. This result contradicts previous studies, in which it has always been maintained that anticyclonic circulation should result. [...]
| Identifer | oai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.116755 |
| Date | January 1965 |
| Creators | Anand, Harbhajan S. |
| 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 Meteorology. ) |
| 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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