Wind Observations in the MLT Region over Southern Japan, by Using Foil Chaff Technique, Yamagawa MF Radar and the MU Radar

Details Wind Observations in the MLT Region over Southern Japan, by Using Foil Chaff Technique, Yamagawa MF Radar and the MU Radar Wind Observations in the MLT Region over Southern Japan, by Using Foil Chaff Technique, Yamagawa MF Radar and the MU Radar

Jan 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999adspr..24..575m&link_type=abstract

Advances in Space Research, Volume 24, Issue 5, p. 575-578.

Computer Science

Scientific paper

Wind fields observed with foil chaff technique in the mesosphere and lower thermosphere (80-98 km in altitude) by means of two micro-rockets at 1200 and 1315 UT on 14 January 1997 from Uchinoura, Japan (31N, 131E) are compared with the winds simultaneously observed with the MU radar (MUR; 35N, 136E) and the Yamagawa MF radar (MFR; 31N, 131E). The chaff and MFR results showed good agreement at 80-88 km, and MFR data were missing at higher altitudes. A coherent structure was commonly detected in the chaff, MFR, and the MUR winds, likely caused by a large scale gravity wave

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