The effects of cumulus cloud ensembles on the dynamics of mid-latitude explosive cyclones are studied both from a diagnostic and from a theoretical point of view. / A diagnostic study of an explosive winter storm shows that significant residuals attributable to cumulus convection are present in the horizontal momentum, thermodynamic and vorticity budgets, but not in the divergence budget, and that the finite-amplitude wave is well described by linear dynamics. / A scale analysis appropriate for mid-latitude synoptic-scale waves with intense convection indicates the importance of three mechanisms by which cumulus clouds can influence these storms. These mechanisms are the thermodynamic and dynamical effects of clouds, and certain cloud-induced non-geostrophic effects. / A series of experiments with linear models of moist baroclinic instability using an idealized basic state shows the significant role of the ageostrophic terms and the important damping due to the dynamical effects of clouds. With a realistic wintertime basic state, we conclude that the different cloud forcings are necessary to account for the observed features of explosive storms.
| Identifer | oai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.72018 |
| Date | January 1985 |
| Creators | Mailhot, Jocelyn. |
| 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 | Doctor of Philosophy (Department of Meteorology.) |
| Rights | All items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated. |
| Relation | alephsysno: 000221112, proquestno: AAINL20887, Theses scanned by UMI/ProQuest. |
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