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  • Author or Editor: W. L. Somervell Jr. x
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J. J. George
,
P. M. Wolff
, and
W. L. Somervell Jr.

Abstract

An empirically derived method is presented for objectively predicting the 24-hr movement and change in intensity of maritime cyclones. The technique developed requires only measurement of the 500-mb height and temperature gradients above the current sea-level center, and determination of the type of 500-mb flow within which the surface system is embedded.

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