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Atmospheric circulation during warm geologic periods: Is the equator-to-pole surface-temperature gradient the controlling factor?
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Atmospheric circulation during warm geologic periods: Is the equator-to-pole surface-temperature gradient the controlling factor?
Atmospheric circulation during warm geologic periods: Is the equator-to-pole surface-temperature gradient the controlling factor?
EB
E. J. Barren
E. J. Barren
WW
W. M. Washington
W. M. Washington
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1 January 1982
journal article
Published by
Geological Society of America
in
Geology
Vol. 10
(12)
https://doi.org/10.1130/0091-7613(1982)10<633:acdwgp>2.0.co;2
Abstract
No abstract available
Keywords
ATMOSPHERIC CIRCULATION
SURFACE TEMPERATURE
Cited by 51 articles