気象集誌. 第2輯
Online ISSN : 2186-9057
Print ISSN : 0026-1165
ISSN-L : 0026-1165

この記事には本公開記事があります。本公開記事を参照してください。
引用する場合も本公開記事を引用してください。

Feasibility Study for Future Spaceborne Coherent Doppler Wind Lidar, Part 2: Measurement Simulation Algorithms and Retrieval Error Characterization
BARON PhilippeISHII ShokenOKAMOTO KozoGAMO KyokaMIZUTANI KoheiTAKAHASHI ChikakoITABE ToshikazuIWASAKI ToshikiKUBOTA TakujiMAKI TakashiOKI RikoOCHIAI SatoshiSAKAIZAWA DaisukeSATOH MasakiSATOH YoheiTANAKA Taichu Y.YASUI Motoaki
著者情報
ジャーナル フリー 早期公開

論文ID: 2017-018

この記事には本公開記事があります。
詳細
抄録
 A feasibility study of tropospheric wind measurements by a coherent Doppler lidar aboard a super-low-altitude satellite is being conducted in Japan. The considered lidar uses a 2.05 μ m laser light source of 3.75 W. In order to assess the measurement performances, simulations of wind measurements were conducted. The mission definition is presented in a companion paper (Part 1) while, in this paper, we describe the measurement simulator and characterize the errors on the retrieved line-of-sight (LOS) winds. Winds are retrieved from the Doppler-shift of the noisy backscattered signal with a horizontal resolution of 100 km along the orbit track and a vertical resolution between 0.5 and 2 km. Cloud and wind fields are the pseudo-truth of an Observing System Simulation Experiment while aerosol data are from the Model-of-Aerosol-Species-IN-the-Global-AtmospheRe (MASINGAR) constrained with the pseudo-truth wind. We present the results of the analysis of a full month of data in summer time for a near-polar orbiting satellite and a LOS nadir angle of 35°. Below ≈ 8 km, the ratio of good retrievals is 30—55 % and the median LOS wind error is better than 0.6 m s-1 (1.04 m s-1 for the horizontal wind). In the upper troposphere, the ratio is less than 15 % in the southern hemisphere and high-latitudes. However the ratio is still 35 % in the northern Tropics and mid-latitudes where ice-clouds frequently occur. The upper-tropospheric median LOS-wind measurement error is between 1-2 m s-1 depending on the latitude (1.74-3.5 m s-1 for the horizontal wind). These errors are dominated by uncertainties induced by spatial atmospheric inhomogeneities.
著者関連情報
© 2017 by Meteorological Society of Japan
feedback
Top