Analysis of rain effects on China-France oceanography satellite scatterometer backscatter measurements

被引:0
|
作者
Quan, Meixuan [1 ]
Yan, Qiushuang [1 ]
Fan, Chenqing [2 ,3 ]
Meng, Junmin [2 ,3 ]
Zhang, Jie [1 ,2 ,3 ]
机构
[1] China Univ Petr, Coll Oceanog & Space Informat, Qingdao, Peoples R China
[2] Minist Nat Resources, Inst Oceanog 1, Qingdao, Peoples R China
[3] Minist Nat Resources, Technol Innovat Ctr Ocean Telemetry, Qingdao, Peoples R China
基金
中国国家自然科学基金;
关键词
Backscatter coefficient; CFOSAT scatterometer; rain effect; ocean surface wind; BAND; SCATTERING; OCEAN;
D O I
10.1080/2150704X.2024.2399328
中图分类号
TP7 [遥感技术];
学科分类号
081102 ; 0816 ; 081602 ; 083002 ; 1404 ;
摘要
The rotating fan beam scanning observation mechanism of China-France oceanography satellite (CFOSAT) scatterometer provides more comprehensive ocean measurements. However, its data quality is often impacted by rain contamination. In this study, we analysed the effect of rain on CFOSAT SCATterometer (CSCAT) backscatter measurements by collocating CSCAT data, the Integrated Multi-satellitE Retrievals (IMERG) rain data, and the wind reanalysis from European Centre for Medium-Range Weather Forecasts (ECMWF). The research findings indicate that, rain exhibits an intensification effect on backscatter at low wind speeds, but this effect gradually diminishes with increasing wind speeds, eventually transitioning to an attenuation effect at a wind speed between 10-20 m<middle dot>s(-1). At extremely high wind speeds above 20 m<middle dot>s(-1), the rain initially increases and then decreases CSCAT normalized radar cross section (sigma(0)) as the rain rate increases. The sensitivity of CSCAT sigma(0) to rain rate decreases as the incidence angle increases. Its sensitivity to wind speed decreases as the rain rate increases. The azimuthal modulation becomes more pronounced with higher wind speeds and smaller incidence angles. However, rain weakens the asymmetry and anisotropy. Furthermore, the HH polarization exhibits a more pronounced susceptibility to rain compared to the VV polarization.
引用
收藏
页码:1011 / 1022
页数:12
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