N Equator Air starts moving toward a zone of low pressure and veers off course to right -Core of tropical cyclone rotating to the left, counter- clockwise Figure 8.28 The dynamics of a tropical cyclone, showing the influence of the Coriolis effect. Note that the storm turns the "wrong" way (that is, counterclockwise) in the Northern Hemisphere, but for the "right" reasons. Air starts moving toward a zone of low pressure and veers off course to right © Cengage Learning
N Equator Air starts moving toward a zone of low pressure and veers off course to right -Core of tropical cyclone rotating to the left, counter- clockwise Figure 8.28 The dynamics of a tropical cyclone, showing the influence of the Coriolis effect. Note that the storm turns the "wrong" way (that is, counterclockwise) in the Northern Hemisphere, but for the "right" reasons. Air starts moving toward a zone of low pressure and veers off course to right © Cengage Learning
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
Related questions
Question
Which way do tropical cyclones spin in the Southern Hemisphere?

Transcribed Image Text:N
Equator
Air starts moving
toward a zone of
low pressure and
veers off course
to right
-Core of tropical
cyclone rotating
to the left, counter-
clockwise
Figure 8.28 The dynamics of a tropical cyclone, showing the influence
of the Coriolis effect. Note that the storm turns the "wrong" way (that
is, counterclockwise) in the Northern Hemisphere, but for the "right"
reasons.
Air starts moving
toward a zone of low
pressure and veers
off course to right
© Cengage Learning
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