30 September 1994 Validation of winds from the High-Resolution Doppler Imager on the Upper Atmosphere Research Satellite (UARS)
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Horizontal winds in the mesosphere and lower thermosphere are obtained with the high resolution Doppler imager (HRDI) on the Upper Atmosphere Research Satellite (UARS) by observing the Doppler shifts of emission lines in the O2 atmospheric band. The validity of the measurements depends on an accurate knowledge of the positions on the detector of the observed lines in the absence of a wind induced Doppler shift. These positions have been determined to an accuracy of better than 5 ms-1 from the comparison of winds measured by HRDI with those obtained by MF radars and rockets. In addition, the degrees of horizontal and vertical smoothing of the recovered wind profiles have been optimized by examining the effect both on the amplitude of the HRDI derived diurnal tidal amplitude and the variance of the wind differences with correlative data.
© (1994) COPYRIGHT Society of Photo-Optical Instrumentation Engineers (SPIE). Downloading of the abstract is permitted for personal use only.
Mark D. Burrage, Mark D. Burrage, Wilbert R. Skinner, Wilbert R. Skinner, Alan R. Marshall, Alan R. Marshall, Paul B. Hays, Paul B. Hays, R. S. Lieberman, R. S. Lieberman, S. J. Franke, S. J. Franke, David A. Gell, David A. Gell, David A. Ortland, David A. Ortland, F. J. Schmidlin, F. J. Schmidlin, Robert A. Vincent, Robert A. Vincent, D. L. Wu, D. L. Wu, "Validation of winds from the High-Resolution Doppler Imager on the Upper Atmosphere Research Satellite (UARS)", Proc. SPIE 2266, Optical Spectroscopic Techniques and Instrumentation for Atmospheric and Space Research, (30 September 1994); doi: 10.1117/12.187566; https://doi.org/10.1117/12.187566


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