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A case study of gravity wave dissipation in the polar MLT region using sodium LIDAR and radar data

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Academic year: 2017

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Figure 1. (a) The neutral temperature variation from 16:30 UT on 29 October to 00:30 UT on 30 October 2010
Figure 3. The eastward (a) and northward (b) wind velocity ob- ob-tained by meteor radar from 80 to 100 km from 16:30 to 24:30 UT on 29 October 2010
Figure 4. Eight hourly hodographs associated with the fitted eclipses are shown. Crosses denote data values associated with corresponding height values (in km)
Figure 5. The local time maximum (a), phase difference between temperature and wind oscillation (b), and amplitude profile of the temperature and wind (c)
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