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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.
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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| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 153 | 20 | 4 |
| PDF Downloads | 12 | 5 | 1 |
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