Kinematic divergence and large scale energy conversions.
Experimental evidence is presented in support of the hypothesis that real, large-scale divergence and energy conversion processes can be analysed from the winds and temperatures reported by the present North American rawinsonde network. The Bellamy triangle method has been used to produce divergence...
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McGill University
1963
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ndltd-LACETR-oai-collectionscanada.gc.ca-QMM.1150912014-02-13T04:10:01ZKinematic divergence and large scale energy conversions.Eddy, George. A.Meteorology.Experimental evidence is presented in support of the hypothesis that real, large-scale divergence and energy conversion processes can be analysed from the winds and temperatures reported by the present North American rawinsonde network. The Bellamy triangle method has been used to produce divergence and this divergence is shown to have continuity in the horizontal, the vertical and in time. A discussion of the scale on which this parameter can be analysed objectively and the errors involved are presented. Energy conversion processes associated with an individual weather system are displayed in map form for comparison with other synoptic features.McGill UniversityBoville, B. (Supervisor)1963Electronic 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.Doctor of Philosophy. (Department of Earth Sciences.) http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=115091 |
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en |
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Meteorology. |
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Meteorology. Eddy, George. A. Kinematic divergence and large scale energy conversions. |
description |
Experimental evidence is presented in support of the hypothesis that real, large-scale divergence and energy conversion processes can be analysed from the winds and temperatures reported by the present North American rawinsonde network. The Bellamy triangle method has been used to produce divergence and this divergence is shown to have continuity in the horizontal, the vertical and in time. A discussion of the scale on which this parameter can be analysed objectively and the errors involved are presented. Energy conversion processes associated with an individual weather system are displayed in map form for comparison with other synoptic features. |
author2 |
Boville, B. (Supervisor) |
author_facet |
Boville, B. (Supervisor) Eddy, George. A. |
author |
Eddy, George. A. |
author_sort |
Eddy, George. A. |
title |
Kinematic divergence and large scale energy conversions. |
title_short |
Kinematic divergence and large scale energy conversions. |
title_full |
Kinematic divergence and large scale energy conversions. |
title_fullStr |
Kinematic divergence and large scale energy conversions. |
title_full_unstemmed |
Kinematic divergence and large scale energy conversions. |
title_sort |
kinematic divergence and large scale energy conversions. |
publisher |
McGill University |
publishDate |
1963 |
url |
http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=115091 |
work_keys_str_mv |
AT eddygeorgea kinematicdivergenceandlargescaleenergyconversions |
_version_ |
1716646579442548736 |