Initial Tropospheric Wind Observations by Sanya Incoherent Scatter Radar

被引:4
|
作者
Zhang, Ning [1 ,2 ]
Yue, Xinan [1 ,2 ,3 ]
Ding, Feng [1 ,2 ,3 ]
Ning, Baiqi [1 ,2 ]
Wang, Junyi [1 ,2 ,3 ]
Luo, Junhao [1 ,2 ]
Wang, Yonghui [1 ,2 ,3 ]
Li, Mingyuan [1 ,2 ,3 ]
Cai, Yihui [1 ,2 ,3 ]
机构
[1] Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing 100029, Peoples R China
[2] Chinese Acad Sci, Inst Geol & Geophys, Beijing Natl Observ Space Environm, Beijing 100029, Peoples R China
[3] Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
基金
中国国家自然科学基金;
关键词
tropospheric wind; atmospheric turbulence; SYISR; multibeam measurement; LOWER-STRATOSPHERIC WINDS; UPPER-ATMOSPHERE RADAR; DOPPLER RADAR; ARECIBO; MESOSPHERE; WAVES; TURBULENCE; PROFILER; VERSION; MIDDLE;
D O I
10.3390/rs14133138
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Sanya incoherent scatter radar (SYISR) is a newly developed phased array incoherent scatter radar in the low latitudes of China located at Sanya (18.3 degrees N, 109.6 degrees E), Hainan Province. The main objective of SYISR is to observe the ionosphere. Given its frequency and power, it should have the capability to observe the troposphere. In this study, we show several tropospheric wind experiments that may indicate radar function expansion and capability verification, although observing the troposphere will not be an operation mode in the future. Reliable radar echoes were detected by SYISR up to 20 km with a turbulence scale of 0.35 m and a frequency of 430 MHz. Generally, both the geometric (GEO) method and the velocity azimuth display (VAD) method give similar wind profiles. Above 10 km, the discrepancy between the two methods becomes nonnegligible. For the same method, the discrepancy above 15-20 km among winds derived from different zenith angle measurements is nonnegligible. The VAD methods give more reasonable results at higher altitudes. The standard deviation of the difference (SYISR radar minus the reanalysis data ERA5) for zonal wind and meridional wind was 1.1 m/s and 0.78 m/s, respectively. During rainfall, we can distinguish the spectrum of rainfall and atmospheric turbulence from the power spectrum according to the spectral widths and Doppler frequency shifts.
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页数:17
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