An integrated and homogenized global surface solar radiation dataset and its reconstruction based on a convolutional neural network approach

• Published in: Earth System Science Data
• Main Authors: Jiao B., Su Y., Li Q., Manara V., Wild M.
• Other Authors: B. Jiao, Y. Su, Q. Li, V. Manara, M. Wild
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2023
• Subjects: Settore FIS/06 - Fisica per il Sistema Terra e Il Mezzo Circumterrestre; Settore GEO/12 - Oceanografia e Fisica dell'Atmosfera; Antarc*; Antarctica
• Online Access: https://hdl.handle.net/2434/1021414; https://doi.org/10.5194/essd-15-4519-2023

Surface solar radiation (SSR) is an essential factor in the flow of surface energy, enabling accurate capturing of long-term climate change and understanding of the energy balance of Earth's atmosphere system. However, the long-term trend estimation of SSR is subject to significant uncertainties due to the temporal inhomogeneity and the uneven spatial distribution of in situ observations. This paper develops an observational integrated and homogenized global terrestrial (except for Antarctica) station SSR dataset (SSRIHstation) by integrating all available SSR observations, including the existing homogenized SSR results. The series is then interpolated in order to obtain a 5g g¯×g¯5g resolution gridded dataset (SSRIHgrid). On this basis, we further reconstruct a long-term (1955-2018) global land (except for Antarctica) SSR anomaly dataset with a 5g g¯×g¯2.5g resolution (SSRIH20CR) by training improved partial convolutional neural network deep-learning methods based on 20th Century Reanalysis version 3 (20CRv3). Based on this, we analysed the global land- (except for Antarctica) and regional-scale SSR trends and spatiotemporal variations. The reconstruction results reflect the distribution of SSR anomalies and have high reliability in filling and reconstructing the missing values. At the global land (except for Antarctica) scale, the decreasing trend of the SSRIH20CR (-1.276g¯±g¯0.205g¯Wg¯m-2 per decade) is smaller than the trend of the SSRIHgrid (-1.776g¯±g¯0.230g¯Wg¯m-2 per decade) from 1955 to 1991. The trend of the SSRIH20CR (0.697g¯±g¯0.359g¯Wg¯m-2 per decade) from 1991 to 2018 is also marginally lower than that of the SSRIHgrid (0.851g¯±g¯0.410g¯Wg¯m-2 per decade). At the regional scale, the difference between the SSRIH20CR and SSRIHgrid is more significant in years and areas with insufficient coverage. Asia, Africa, Europe and North America cause the global dimming of the SSRIH20CR, while Europe and North America drive the global brightening of the SSRIH20CR. Spatial sampling inadequacies have largely ...