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Tao Yuan, C. Fish, J. Sojka, D. Rice, M. J. Taylor and N. J. Mitchell Coordinated investigation of summer time mid-latitude descending E layer (Es) perturbations using Na lidar, ionosonde, and meteor wind radar observations over Logan, Utah (41.7°N, 111.8°W) Journal of Geophysical Research: Atmospheres 118

Article first published online: 28 FEB 2013 | DOI: 10.1029/2012JD017845

Key Points

  • Es induces large perturbations of Na abundance in lower thermosphere
  • Es weakening is coincident with weakening of zonal wind tides
  • The damping of tidal amplitude is the result of interaction between PW and Tide

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