The Greenhouse Gases Observing Satellite-2 (GOSAT-2), launched in October 2018, is equipped with the Cloud and Aerosol Imager-2 (CAI-2), which is used to estimate aerosol properties. In this study, the error characteristics of the estimated products were investigated through comparison with ground-based observations. Worldwide AERONET data from all available sites were primarily used to evaluate the optical properties of aerosol for the period March 2019 to December 2024. The comparison results for each year were similar, and most error statistics showed little or no trend. Consequently, the results from 2019 were considered to be representative and are presented here.
Comparing the satellite data with the AERONET data and calculating the correlation coefficients between them, the correlation for aerosol optical depth (AOD) was generally moderate, but the correlations for other parameters (Ångström exponent (AE_ext), absorption AOD (AOD_abs), absorption AE (AE_abs), single scattering albedo (SSA), PM2.5, and BC amount) were either absent or weak. For example, in a comparison between AOD at 550 nm with AERONET_AOD (all) (i.e., over land and ocean areas), the bias (BIAS), standard deviation (SD), and root mean squared error (RMSE), were 0.090, 0.149, and 0.174, respectively, and the correlation coefficient (R) was 0.593, indicating a moderate correlation. The satellite estimates tended to be overestimated when AOD was low and underestimated when AOD was high. In the comparison with AERONET_AOD (ocean) (i.e., over ocean areas), the BIAS, SD, and RMSE were 0.138, 0.071, and 0.155, respectively, and R was 0.880, indicating a strong correlation. Both the BIAS and R were higher than the values observed over land.
The results of the comparisons varied by dataset, region, target area, and time period. For ground-based AOD values below approximately 0.2, the satellite-derived AOD estimates were insensitive to changes in AOD, suggesting that low AOD values may not be reliably estimated. The estimated AE_ext and AE_abs values were limited to a narrow range, and the SSA values tended to cluster around specific values.
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