Please use this identifier to cite or link to this item: http://hdl.handle.net/10125/11308

Some computations of surface air trajectories over the oceanic tropics and accompanying weather

File Description SizeFormat 
uhm_phd_6910607_uh.pdfVersion for UH users4.04 MBAdobe PDFView/Open
uhm_phd_6910607_r.pdfVersion for non-UH users. Copying/Printing is not permitted4.09 MBAdobe PDFView/Open

Item Summary

Title: Some computations of surface air trajectories over the oceanic tropics and accompanying weather
Authors: Taylor, Ronald Charles
Keywords: Meteorology -- Pacific Ocean
Atmospheric pressure
Weather
Issue Date: 1968
Publisher: [Honolulu]
Abstract: An attempt is made to compute some near surface air trajectories from an initial specification of the (steady) pressure field over selected regions of the oceanic tropics: Friction is assumed to oppose the motion and is proportional to the speed, while the percentage change of horizontal areas is computed to obtain the horizontal velocity divergence along the parcel paths. The latter results are related to observed distributions of low-level cloudiness and rainfall in the Indian Ocean and selected regions of the Pacific. Further interpretative comment is offered through an analysis of the divergence equation; the latter indicates that both the divergence of the pressure-gradient force and Coriolis forces are significant in determining the temporal change of horizontal velocity divergence along a trajectory.
Description: Typescript.
Bibliographical references included in "Notes and references" (leaves [147]-162)
xiv, 162 l illus., tables
URI/DOI: http://hdl.handle.net/10125/11308
Rights: All UHM dissertations and theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission from the copyright owner.
Appears in Collections:Ph.D. - Geosciences (Meteorology)



Items in ScholarSpace are protected by copyright, with all rights reserved, unless otherwise indicated.