In this thesis we examine the possible causes of the model-to-model variability observed in the Comparison of Mesoscale Prediction and Research Experiments (COMPARE). A series of sensitivity experiments is performed involving changes to model initial conditions, physical parameterizations, and numerics. / Secondary cyclogenesis is most sensitive to latent heat release and moisture fluxes from the ocean surface. Initial differences are found to decay with time, and more rapidly so, in a 'dry' simulation. Sea-level pressures for the low center are lower in integrations with a longer time step, owing to greater rainrates and low-level diabatic heating at the storm center from 12 to 18 h. / Moisture fluxes in the first 12 h are crucial in creating grid-box saturation for initiation of precipitation, and the generation of a low-level potential vorticity maximum, with fluxes during the subsequent 24-h period of rapid deepening not as crucial. A westward storm track bias in COMPARE is related to a more robust low-level potential vorticity maximum along the coast, as compared to the maximum offshore.
Identifer | oai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.26664 |
Date | January 1996 |
Creators | Carrera, Marco. |
Contributors | Gyakum, John R. (advisor), Zhang, Da-Lin (advisor) |
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 Atmospheric and Oceanic Sciences.) |
Rights | All items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated. |
Relation | alephsysno: 001642599, proquestno: MQ37308, Theses scanned by UMI/ProQuest. |
Page generated in 0.0108 seconds