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E. Palmén
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Dorothy L. Bradbury
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E. Palmén

Specific cases are cited which show the existence of a clear-cut frontal zone at the 500-mb level. The relationship of this frontal zone to the location of the jet stream and to the formation of surface disturbances can be used as a valuable tool for forecasting. The value of the data received from weather reconnaissance flights is emphasized and recommendations for improving these flights are given.

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