asymptotic direction of arrival
asymptotic direction of arrival
[ā‚sim′täd·ik di′rek·shən əv ə′rīv·əl] (geophysics)
The direction at infinity of a positively charged particle, with given rigidity, which impinges in a given direction at a given point on the surface of the earth, after passing through the geomagnetic field.
McGraw-Hill Dictionary of Scientific & Technical Terms, 6E, Copyright © 2003 by The McGraw-Hill Companies, Inc.
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