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Relation of Geomagnetic Disturbances to Circulation Changes at 30,000-Foot Level

Norman J. Macdonald and David D. Woodbridge
Science
New Series, Vol. 129, No. 3349 (Mar. 6, 1959), pp. 638-639
Stable URL: http://www.jstor.org/stable/1758194
Page Count: 2
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Abstract

From analyses of waves in the circulation pattern at the jet-stream level of the atmosphere during the winters of 1956-57 and 1957-58, it was found that, in comparison with other waves, those which appeared in the Alaska-Aleutian area about 3 days after a magnetic disturbance subsequently developed into large-amplitude disturbances.

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