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Feasibility Study for Future Spaceborne Coherent Doppler Wind Lidar, Part 2: Measurement Simulation Algorithms and Retrieval Error Characterization
被引:15
|作者:
Baron, Philippe
[1
]
Ishii, Shoken
[1
]
Okamoto, Kozo
[2
]
Gamo, Kyoka
[3
]
Mizutani, Kohei
[1
]
Takahashi, Chikako
[3
]
Itabe, Toshikazu
[1
]
Iwasaki, Toshiki
[4
]
Kubota, Takuji
[5
]
Maki, Takashi
[2
]
Oki, Riko
[5
]
Ochiai, Satoshi
[1
]
Sakaizawa, Daisuke
[5
]
Satoh, Masaki
[6
]
Satoh, Yohei
[7
]
Tanaka, Taichu Y.
[2
]
Yasui, Motoaki
[8
]
机构:
[1] Natl Inst Informat & Commun Technol, Appl Electromagnet Res Inst, 4-2-1,Nukui Kitamachi, Koganei, Tokyo 1848795, Japan
[2] Japan Meteorol Agcy, Meteorol Res Inst, Tsukuba, Ibaraki, Japan
[3] Fujitsu FIP Corp, Tokyo, Japan
[4] Tohoku Univ, Grad Sch Sci, Sendai, Miyagi, Japan
[5] Japan Aerosp Explorat Agcy, Earth Observat Res Ctr, Tsukuba, Ibaraki, Japan
[6] Univ Tokyo, Kashiwa, Chiba, Japan
[7] Japan Aerosp Explorat Agcy, Satellite Technol Innovat Off, Tsukuba, Ibaraki, Japan
[8] Natl Inst Informat & Commun Technol, Social Innovat Unit, Strateg Program Produce Off, Koganei, Tokyo, Japan
关键词:
Doppler lidar;
satellite;
remote sensing;
wind;
aerosol;
simulation;
BACKSCATTER HETERODYNE LIDAR;
DIFFERENTIAL ABSORPTION;
AEROSOL OBSERVATIONS;
PERFORMANCE;
VELOCITY;
WEATHER;
ACCUMULATION;
OPTIMIZATION;
PREDICTION;
TURBULENCE;
D O I:
10.2151/jmsj.2017-018
中图分类号:
P4 [大气科学(气象学)];
学科分类号:
0706 ;
070601 ;
摘要:
A feasibility study of tropospheric wind measurements using a coherent Doppler lidar aboard a super low altitude satellite is being conducted in Japan. The considered lidar uses a 2.05 mu 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 degrees. Below approximate to 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.
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页码:319 / 342
页数:24
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