Mixing height and Cloud Convection in the Canadian PrairiesReportar como inadecuado




Mixing height and Cloud Convection in the Canadian Prairies - Descarga este documento en PDF. Documentación en PDF para descargar gratis. Disponible también para leer online.

Mixing height and Convection

Stachowiak, Olga I

Supervisor and department: Reuter, Gerhard Earth and Atmospheric Science Wilson, John Earth and Atmospheric Science

Examining committee member and department: Wilson, John Earth and Atmospheric Science Gan,Thian Civil and Environmental Engineering Reuter, Gerhard Earth and Atmospheric Science

Department: Department of Earth and Atmospheric Sciences

Specialization:

Date accepted: 2010-01-29T18:51:06Z

Graduation date: 2010-06

Degree: Master of Science

Degree level: Master's

Abstract: The Mixing Height MH, Convective Condensation Level CCL, and Convective Available Potential Energy CAPE are computed with different methods and we examined whether these parameters can help to discriminate between weak and strong convection. The observational data set contains soundings released from Stony Plain in Alberta and The Pas in Manitoba for the summers of 2006 and 2007. The major findings were: 1 The Mixing Height values computed with the Heffter method were reliable provided the critical inversion criterion was adjusted for Prairie conditions.2 The Mixing Height values computed with the Moist Mixed layer method were in good agreement with Mixing Heights computed with the Heffter method.3 The Mixing Height values computed with the Holzworth parcel method were less useful in that often the potential temperature did not decrease with height above the ground.4 Observed convective cloud base heights tended to be lower than the CCL computed using the surface parcel method, the 50 mb mixed parcel method, and the moist mixed parcel method.5 The MH, the sounding-based CCL, and the CAPE did not differentiate between weak and strong convection.6 We derived a new parameter: the difference between the convective cloud base and the Moist Air Mixing Height. This parameter did discriminate between the likely occurrence of strong and weak convection.

Language: English

DOI: doi:10.7939-R32S4X

Rights: Permission is hereby granted to the University of Alberta Libraries to reproduce single copies of this thesis and to lend or sell such copies for private, scholarly or scientific research purposes only. Where the thesis is converted to, or otherwise made available in digital form, the University of Alberta will advise potential users of the thesis of these terms. The author reserves all other publication and other rights in association with the copyright in the thesis and, except as herein before provided, neither the thesis nor any substantial portion thereof may be printed or otherwise reproduced in any material form whatsoever without the author's prior written permission.





Autor: Stachowiak, Olga I

Fuente: https://era.library.ualberta.ca/



DESCARGAR PDF




Documentos relacionados