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The Transition From Summer-to-Winter Temperatures Between 70 and ~115 km as Observed With the ALO-USU Rayleigh Lidar

Document Type

Poster

Publication Date

5-21-2024

Abstract

Rayleigh-Scatter Lidar Temperature Retrieval

  • Elastic scattering from N2, O2, Ar, and O.
  • Obtain a backscatter profile
  • Convert that profile to a relative density profile
  • From that profile derive an absolute temperature profile [1]. Use: Ideal gas law, Hydrostatic equilibrium, Top temperature

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