Atmospheric kinetic energy at 500 mb as a function of zonal wave number.

Atmospheric kinetic energy at 500 mb as a function of zonal wave number.

An adequate portrayal of the global distribution of kinetic energy is fundamental to our understanding of the general circulation of the atmosphere. Since there are insufficient wind observations to carry out direct computations it is customary to supplement them with pressure or geopotential height...

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Bibliographic Details
Main Author: Luistro, Farnacio M.
Other Authors: Luistro, Farnacio M. (Supervisor)
Format: Others
Language:en
Published: McGill University 1965
Subjects:
Meteorology.
Aerodynamics.
Online Access:http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=118032
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spelling ndltd-LACETR-oai-collectionscanada.gc.ca-QMM.1180322014-02-13T04:11:26ZAtmospheric kinetic energy at 500 mb as a function of zonal wave number.Luistro, Farnacio M.Meteorology.Aerodynamics.An adequate portrayal of the global distribution of kinetic energy is fundamental to our understanding of the general circulation of the atmosphere. Since there are insufficient wind observations to carry out direct computations it is customary to supplement them with pressure or geopotential height data and to use space and time continuity to obtain analyzed weather maps. [...]McGill UniversityLuistro, Farnacio M. (Supervisor)1965Electronic Thesis or Dissertationapplication/pdfenalephsysno: NNNNNNNNNTheses scanned by McGill Library.All items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated.Master of Science. (Department of Meteorology.) http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=118032
collection NDLTD
language en
format Others
sources NDLTD
topic Meteorology.
Aerodynamics.
spellingShingle Meteorology.
Aerodynamics.
Luistro, Farnacio M.
Atmospheric kinetic energy at 500 mb as a function of zonal wave number.
description An adequate portrayal of the global distribution of kinetic energy is fundamental to our understanding of the general circulation of the atmosphere. Since there are insufficient wind observations to carry out direct computations it is customary to supplement them with pressure or geopotential height data and to use space and time continuity to obtain analyzed weather maps. [...]
author2 Luistro, Farnacio M. (Supervisor)
author_facet Luistro, Farnacio M. (Supervisor)
Luistro, Farnacio M.
author Luistro, Farnacio M.
author_sort Luistro, Farnacio M.
title Atmospheric kinetic energy at 500 mb as a function of zonal wave number.
title_short Atmospheric kinetic energy at 500 mb as a function of zonal wave number.
title_full Atmospheric kinetic energy at 500 mb as a function of zonal wave number.
title_fullStr Atmospheric kinetic energy at 500 mb as a function of zonal wave number.
title_full_unstemmed Atmospheric kinetic energy at 500 mb as a function of zonal wave number.
title_sort atmospheric kinetic energy at 500 mb as a function of zonal wave number.
publisher McGill University
publishDate 1965
url http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=118032
work_keys_str_mv AT luistrofarnaciom atmospherickineticenergyat500mbasafunctionofzonalwavenumber
_version_ 1716647070014636032

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