The geostrophic kinetic energy 30N to 8ON at 1000 mb, 500 mb, 100 mb and 25 mb is computed on a daily basis for January, 1959, employing Fourier analysis. The general characteristics of the energy spectra are presented as means for the month. The daily variations reveal that tropospheric "shore" wave kinetic energy is a good indicator of surface cyclonic activity, and that the effect of tropospheric synoptic scale disturbances is strongly damped in the lower stratosphere. Four levels proved inadequate to define the vertical structure of the ultra-long waves. [...]
| Identifer | oai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.117847 |
| Date | January 1965 |
| Creators | Klump, Leo John. |
| 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. |
Page generated in 0.0016 seconds