Surface Solar Radiation Compositions Observed from Himawari-8/9 and Fengyun-4 Series

Author:

Letu Husi1,Ma Run2,Nakajima Takashi Y.3,Shi Chong1,Hashimoto Makiko4,Nagao Takashi M.5,Baran Anthony J.6,Nakajima Teruyuki7,Xu Jian8,Wang Tianxing9,Tana Gegen8,Bilige Sude10,Shang Huazhe1,Chen Liangfu1,Ji Dabin1,Lei Yonghui1,Wei Lesi1,Zhang Peng11,Li Jun12,Li Lei13,Zheng Yu13,Khatri Pradeep14,Shi Jiancheng8

Affiliation:

1. State Key Laboratory of Remote Sensing Science, Aerospace Information Research Institute, Chinese Academy of Sciences, Beijing, China;

2. State Key Laboratory of Remote Sensing Science, Aerospace Information Research Institute, Chinese Academy of Sciences, and University of Chinese Academy of Sciences, Beijing, China;

3. Research and Information Center (TRIC), Tokai University, Hiratsuka, Kanagawa, Japan;

4. Earth Observation Research Center, Japan Aerospace Exploration Agency, Tsukuba, Japan;

5. Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa, Japan;

6. Met Office, Exeter, and School of Physics, Astronomy, and Mathematics, University of Hertfordshire, Hatfield, Hertfordshire, United Kingdom;

7. Center for Global Environmental Research, National Institute for Environmental Studies, Tsukuba, Japan;

8. National Space Science Center, Chinese Academy of Sciences, Beijing, China;

9. School of Geospatial Engineering and Science, Sun Yat-sen University, and Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, China;

10. Information Center, Inner Mongolia Normal University, Hohhot, China;

11. National Satellite Meteorological Center, China Meteorological Administration, Beijing, China;

12. Key Laboratory of Radiometric Calibration and Validation for Environmental Satellite, China Meteorological Administration, Beijing, China;

13. State Key Laboratory of Severe Weather (LASW), and Key Laboratory of Atmospheric Chemistry, Chinese Academy of Meteorological Sciences, CMA, Beijing, China;

14. Center for Atmospheric and Oceanic Studies, Tohoku University, Sendai, Japan

Abstract

Abstract Surface downward solar radiation compositions (SSRC), including photosynthetically active radiation (PAR), ultraviolet-A (UVA), ultraviolet-B (UVB), and shortwave radiation (SWR), with high spatial–temporal resolutions and precision are essential for applications including solar power, vegetation photosynthesis, and environmental health. In this study, an optimal algorithm was developed to calculate SSRC, including their direct and diffuse components. Key features of the algorithm include combining the radiative transfer model with machine learning techniques, including full consideration of the effects of aerosol types, cloud phases, and gas components. A near-real-time monitoring system was developed based on this algorithm, with SSRC products generated from Himawari-8/9 and Fengyun-4 series data. Validation with ground-based data shows that the accuracy of the SWR and PAR compositions (daily mean RMSEs of 19.7 and 9.2 W m−2, respectively) are significantly better than those of state-of-the-art products from CERES, ERA5, and GLASS. The accuracy of UVA and UVB measurements is comparable with CERES. Characteristics of aerosols, clouds, gases, and their impacts on SSRC are investigated before, during, and post COVID-19; in particular, significant SSRC variations due to the reduction of aerosols and increase of ozone are identified in the Chinese central and eastern areas during that period. The spatial–temporal resolution of data products [up to 0.05° (10 min)−1 for the full-disk region] is one of the most important advantages. Data for the East Asia–Pacific region during 2016–20 is available from the CARE home page (www.slrss.cn/care/sp/pc/).

Publisher

American Meteorological Society

Subject

Atmospheric Science

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