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The difluent upper trough

The difluent upper trough The difluent upper trough (with wind maximum behind the trough line) is shown to be an important part of the deepening mechanism of cyclones. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Meteorology and Atmospheric Physics Springer Journals

The difluent upper trough

Bjerknes, J.
Meteorology and Atmospheric Physics , Volume 7 (1) – Nov 24, 2005
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References (4)

Publisher
Springer Journals
Copyright
Copyright © 1954 by Springer-Verlag
Subject
Earth Sciences; Atmospheric Sciences; Meteorology; Math. Appl. in Environmental Science; Terrestrial Pollution; Waste Water Technology / Water Pollution Control / Water Management / Aquatic Pollution
ISSN
0177-7971
eISSN
1436-5065
DOI
10.1007/BF02277903
Publisher site
See Article on Publisher Site

Abstract

The difluent upper trough (with wind maximum behind the trough line) is shown to be an important part of the deepening mechanism of cyclones.

Journal

Meteorology and Atmospheric Physics – Springer Journals

Published: Nov 24, 2005

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