A simple model for testing the effects of gravity-wave-produced vertical-oscillations of scattering irregularities on spaced-antenna, horizontal drift measurements

Date

1984

Authors

Meek, C.
Reid, I.

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Conference paper

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Middle Atmosphere Program. Volume 14, Papers presented at the URSI/SCOSTEP Workshop on Technical Aspects of MST Radar, May 22-25, 1984 / S.A. Bowhill, B. Edwards (eds.):pp.131-133

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C. E. Meek and I. M. Reid

Conference Name

URSI/SCOSTEP Workshop on Technical Aspects of MST Radar (2nd : 1984 : Urbana, IL, USA)

Abstract

It has been suggested that the velocities produced by the spaced antenna partial-reflection drift experiment may constitute a measure of the vertical oscillations due to short-period gravity waves rather than the mean horizontal flow. The contention is that the interference between say two scatterers, one of which is traveling upuard, and the other down, will create a pattern which sweeps across the ground in the direction (or anti-parallel) of the wave propagation. Since the expected result, viz. spurious drift directions, is seldom, if ever, seen in spaced antenna drift velocities, this speculation is tested in the following model.

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Also cited as: Handbook for MAP, 1984; 14: pp.131-133

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