Estimation of shortwave solar radiation using the artificial neural network from Himawari-8 satellite imagery over China

被引:35
作者
Peng, Zhong [1 ]
Letu, Husi [1 ]
Wang, Tianxing [1 ]
Shi, Chong [2 ]
Zhao, Chuanfeng [3 ,4 ]
Tana, Gegen [3 ,4 ]
Zhao, Naizhuo [5 ]
Dai, Tie [6 ]
Tang, Ronglin [7 ]
Shang, Huazhe [1 ]
Shi, Jiancheng [1 ]
Chen, Liangfu [1 ]
机构
[1] Chinese Acad Sci, Inst Remote Sensing & Digital Earth, State Key Lab Remote Sensing Sci, Beijing, Peoples R China
[2] Japan Aerosp Explorat Agcy, Earth Observat Res Ctr, 2-1-1 Sengen, Tsukuba, Ibaraki, Japan
[3] Beijing Normal Univ, Coll Global Change & Earth Syst Sci, Beijing, Peoples R China
[4] Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource Ecol, Beijing, Peoples R China
[5] Northeastern Univ, Sch Humanities & Law, Inst Land Resource Management, Shenyang, Liaoning, Peoples R China
[6] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, Beijing, Peoples R China
[7] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, State Key Lab Resources & Environm Informat Syst, Beijing, Peoples R China
基金
中国国家自然科学基金;
关键词
Surface shortwave radiation; Artificial neural network; Geostationary satellite; Empirical orthogonal function; LAND-SURFACE SHORTWAVE; DOUBLING-ADDING METHOD; ICE-CLOUD PROPERTIES; REANALYSIS PRODUCTS; RECENT DECADES; AEROSOLS; ALGORITHM; TREND; FLUX; APPROXIMATION;
D O I
10.1016/j.jqsrt.2019.106672
中图分类号
O43 [光学];
学科分类号
070207 ; 0803 ;
摘要
In this study, we use an artificial neural network (ANN) method to estimate the downward surface shortwave radiation (DSSR) over China from Himawari-8 geostationary satellite data. As the training data of the DSSR estimation algorithm, ground-observed DSSR (GOS) data is compiled to complete the ANN method. GOS data from 89 stations over mainland China in 2016 are divided into training, testing and validation samples with a proportion of 3:1:1, in order to perform the DSSR estimation and accuracy validation. As a result, estimated DSSR from Himawari-8 data in 2016 shows good consistency with validation samples of ground observed DSSR, holding the determination coefficient and root mean square error of 0.90 and 88.86W m(-2) for the hourly mean DSSR, and 0.96 and 24.46W m(-2) for the daily mean DSSR, respectively. To investigate the spatio-temporal variation of daily DSSR in China, we performed the first empirical orthogonal function (EOF) analysis based on the ANN-derived DSSR estimates. The spatial pattern of the first EOF mode reveals a larger DSSR variation in northeast and northwest China, in contrast to the smallest variation appeared in the southwest. The hourly ANN-derived DSSR analysis shows a peak point at noon (local time) in each region, particularly in the Tibetan Plateau. In terms of the monthly and annual DSSR spatial distribution, the regions with higher elevations, such as Northwest, Tibetan Plateau and Inner Mongolia Plateau in China, have larger DSSR than other regions. In contrast, relatively low DSSR appears in the southwest and the northeast of China through the year. (C) 2019 Elsevier Ltd. All rights reserved.
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页数:8
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