Instrumentation

LIDAR (LIght Detection And Ranging) is similar to RADAR, uses electromagnetic waves in the visible or near-visible spectrum to remotely investigate properties of a medium.

There are several types of Lidar:

  • DIAL Lidar (Differential Absorption Lidar)
  • Flourescence Lidar
  • Mie (Aerosol) Lidar
  • Raman Lidar
  • Rayleigh Lidar

The USU Na lidar is a narrowband resonance fluorescence Doppler lidar system operating at the Na D2 linewith a 120 MHz full-width half-maximum laser pulse bandwidth. The Na lidar is currently set up to probe the mesopause region simultaneously in three directions (north, east, and west) during the night and in two directions (north and east) during the daytime using a pair of Faraday filters [Chen et al., 1996] to obtain high-resolution temperature and horizontal wind profiles, along with Na density profile. It provides the critical atmospheric information throughout a full diurnal cycle of observations of the mesopause region, such as tidal and planetary wave variations [She et al., 2004; Yuan et al., 2013] of all the lidar measurements.

Xuguang Cai, JGR: Space Physics, August 2014

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Figure1. Block diagram of the USU Na Lidar.
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Figure1. Picture of the Receiver Room at the Science and Engineering Research Building.

  • CW Nd:YAG Laser
  • CW Ring Dye Laser
  • Pulsed Nd:YAG Laser
  • Pulsed Dye Amplifier
  • Doppler-Free Spectroscope
  • Acoustic Optic Modulator
  • Iodinefilter based Chirp Monitor
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Figure1. Picture of the Telescopes in the roof of the Science and Engineering Research Building.

Two 76 cm Newtonian Starsplitter II telescopes and one 35 cm Schmitt Cassegrain Celestron C-14 telescope used to collect backscattered light