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A study of severe convection over so...
~
Hopsch, Susanna Birgitta.
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A study of severe convection over southern New England.
紀錄類型:
書目-電子資源 : Monograph/item
正題名/作者:
A study of severe convection over southern New England./
作者:
Hopsch, Susanna Birgitta.
面頁冊數:
159 p.
附註:
Source: Masters Abstracts International, Volume: 41-02, page: 0554.
Contained By:
Masters Abstracts International41-02.
標題:
Physics, Atmospheric Science. -
電子資源:
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1410499
ISBN:
0493782125
A study of severe convection over southern New England.
Hopsch, Susanna Birgitta.
A study of severe convection over southern New England.
- 159 p.
Source: Masters Abstracts International, Volume: 41-02, page: 0554.
Thesis (M.S.)--University of Massachusetts Lowell, 2002.
Data from several days during which severe convection occurred over large parts of southern New England were collected during the summer of 2001 and two modes were identified—one mode where the convection propagates over the entire area and a second mode where the convection dissipates as it translates over the southeastern-most parts of New England. A mesoscale numerical weather prediction model was used to simulate the various events. The results of there model simulations were then used to find the involved physical processes responsible for the development of the two scenarios and the differences in various meteorological fields between the two identified modes of sustained convection and dissipating convection were identified. The integration area was divided into several topographically differing zones, and composites for the two scenarios were calculated to identify local differences. Also, a harmonic analysis was performed to gain further insight into which processes are of the biggest importance for the various developments. (Abstract shortened by UMI.)
ISBN: 0493782125Subjects--Topical Terms:
1019431
Physics, Atmospheric Science.
A study of severe convection over southern New England.
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Data from several days during which severe convection occurred over large parts of southern New England were collected during the summer of 2001 and two modes were identified—one mode where the convection propagates over the entire area and a second mode where the convection dissipates as it translates over the southeastern-most parts of New England. A mesoscale numerical weather prediction model was used to simulate the various events. The results of there model simulations were then used to find the involved physical processes responsible for the development of the two scenarios and the differences in various meteorological fields between the two identified modes of sustained convection and dissipating convection were identified. The integration area was divided into several topographically differing zones, and composites for the two scenarios were calculated to identify local differences. Also, a harmonic analysis was performed to gain further insight into which processes are of the biggest importance for the various developments. (Abstract shortened by UMI.)
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