Large wind shears and stabilities in the mesopause region observed by Na wind-temperature lidar at midlatitude

Details Large wind shears and stabilities in the mesopause region observed by Na wind-temperature lidar at midlatitude Large wind shears and stabilities in the mesopause region observed by Na wind-temperature lidar at midlatitude

Oct 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010jgra..11510307y&link_type=abstract

Journal of Geophysical Research, Volume 115, Issue A10, CiteID A10307

Computer Science

Sound

3

Atmospheric Processes: Middle Atmosphere Dynamics (0341, 0342), Atmospheric Processes: Mesospheric Dynamics, Ionosphere: Wave Propagation (0689, 3285, 4275, 4455, 6934), Atmospheric Processes: Tides And Planetary Waves, Planetary Sciences: Comets And Small Bodies: Instruments And Techniques

Scientific paper

Unexpected large horizontal winds and wind shears in the lower thermosphere have been observed by rocket soundings and lidars for decades. From 4 years of the Colorado State University sodium wind-temperature lidar data set (2002-2005 total of ˜1600 nocturnal h), we observed an altitude distribution of high wind velocity and wind shears between 80 and 105 km, similar to the results of chemical release experiments. Our lidar data show conclusively that when the observed wind shears are plotted as a function of the squared Brunt-Vaisala frequency, N2, they are below the value corresponding to the Richardson number of 1/4, which is a necessary condition of the onset of dynamic instability. This suggests that large wind shears can be sustained in the region of high static stability, for example, in the lower thermosphere, where large wind shears are often observed by rocket sounding. The full-diurnal-cycle lidar data enable the extraction of tidal wave components with periods of 24, 12, 8, and 6 h, therefore allowing us to reveal the strong correlation of 60% between large wind shears (>50 m s-1 km-1) and tidal waves. The lidar-measured seasonal variation in N2 and tidal amplitudes in the mesosphere and lower thermosphere are found to be consistent with the difference in altitude distribution of strong wind shears between winter and summer.

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