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...
Main Author: | |
---|---|
Other Authors: | |
Format: | Others |
Language: | en |
Published: |
McGill University
1965
|
Subjects: | |
Online Access: | http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=118032 |
id |
ndltd-LACETR-oai-collectionscanada.gc.ca-QMM.118032 |
---|---|
record_format |
oai_dc |
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 |