A discussion on the existence of the anomalous high and the anomalous low
The air flow in a three-way balance between the Coriolis force, the centrifugal force and the pressure gradient force, i.e., the gradient wind, is discussed. The author studies formation mechanisms and possible existence of four types of gradient wind (the normal high, the normal low, the anomal...
Main Author: | |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2015-10-01
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Series: | Annales Geophysicae |
Online Access: | https://www.ann-geophys.net/33/1253/2015/angeo-33-1253-2015.pdf |
Summary: | The air flow in a three-way balance between the Coriolis force, the
centrifugal force and the pressure gradient force, i.e., the gradient wind,
is discussed. The author studies formation mechanisms and possible
existence of four types of gradient wind (the normal high, the normal
low, the anomalous high and the anomalous low), and proposes
reasonable explanation of the evolution of the gradient wind, especially for the
anomalous high and the anomalous low, both of which are considered to be
pure mathematical solutions and are overlooked in classic literature. |
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ISSN: | 0992-7689 1432-0576 |