Abstract

A mobile Rayleigh Doppler lidar based on the molecular double-edge technique is developed for measuring wind velocity in the middle atmosphere up to 60 km. The lidar uses three lasers with a mean power of 17.5 W at 355 nm each and three 1 m diameter telescopes to receive the backscattered echo: one points to zenith for vertical wind component and temperature measurement; the two others pointing toward east and north are titled at 30° from the zenith for zonal and meridional wind component, respectively. The Doppler shift of the backscattered echo is measured by inter-comparing the signal detected through each of the double-edge channels of a triple Fabry-Perot interferometer (FPI) tuned to either side of the emitted laser line. The third channel of FPI is used for frequency locking and a locking accuracy of 1.8 MHz RMS (root-mean-square) at 355 nm over 2 hours is realized, corresponding to a systematic error of 0.32 m/s. In this paper, we present detailed technical evolutions on system calibration. To validate the performance of the lidar, comparison experiments was carried out in December 2013, which showed good agreement with radiosondes but notable biases with ECMWF (European Centre for Medium range Weather Forecasts) in the height range of overlapping data. Wind observation over one month performed in Delhi (37.371° N, 97.374° E), northwest of China, demonstrated the stability and robustness of the system.

Highlights

  • Wind and temperature measurement are fundamental for a comprehensive understanding of atmospheric dynamics on small (

  • In the Atmospheric Dynamics Mission Aeolus (ADM-Aeolus) payload Atmospheric Laser Doppler Instrument (ALADIN), which has been demonstrated by airborne validation and scheduled to be launched in the near future, observation of stratospheric wind profiles is merely expected to be 30 km altitude [4,5,6,7,8]

  • The Rayleigh/Mie/Raman lidar implemented in ALOMAR conceived and demonstrated an effective solution which uses a Doppler Rayleigh Iodine Spectrometer (DoRIS) with two branches of intensity cascaded channels to cover the dynamic range from

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Summary

Introduction

Wind and temperature measurement are fundamental for a comprehensive understanding of atmospheric dynamics on small (

Description of the method
Instrumental setup
Characterization of the system calibration
Frequency locking of emitted laser
Null Doppler shift reference
Calibration of instrumental drift
Wind and temperature observations
Findings
Conclusion and future research

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