Generating a High-Resolution Time-Series Ocean Surface Net Radiation Product by Downscaling J-OFURO3
Autor: | Shaopeng Li, Xiuxia Li, Shunlin Liang, Jianglei Xu, Yezhe Wang, Bo Jiang, Hongkai Chen, Jianghai Peng, Hui Liang |
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Rok vydání: | 2021 |
Předmět: | |
Zdroj: | IEEE Transactions on Geoscience and Remote Sensing. 59:2794-2809 |
ISSN: | 1558-0644 0196-2892 |
DOI: | 10.1109/tgrs.2020.3021585 |
Popis: | The ocean surface net radiation ( $R_{n}$ ) characterizing ocean surface radiation budget is a key variable in ocean climate modeling and analysis. In this study, a downscaling scheme was developed to generate a high-resolution (0.05°) time-series (2002–2013) daily ocean surface $R_{n}$ from the third-generation Japanese Ocean Flux Data Sets with Use of Remote-Sensing Observations (J-OFURO3) at 0.25° based on the Advanced Very-High-Resolution Radiometer (AVHRR) top-of-atmosphere (TOA) observations (AVH021C) and other ancillary information (Clearness Index and cloud mask). This downscaling scheme includes the statistical downscaling models and the residual correction post-processing. A series of angle-dependent downscaling statistical models were established between the daily ocean surface $R_{n}$ in J-OFURO3 and the AVHRR TOA data, and then, the residual correction was conducted to the model estimates $R_{n}$ _AVHRR_est to obtain the final downscaled data set $R_{n}$ _AVHRR. Validation against the measurements from 57 moored buoy sites in six ocean observing networks shows the high accuracy of the downscaled estimates $R_{n}$ _AVHRR_est with a $R^{2}$ of 0.88, RMSE of 23.44 $\text{W}\cdot \text{m}^{-2}$ , and bias of $-0.14\,\,\text{W}\cdot \text{m}^{-2}$ under all-sky condition. The results of the spatio-temporal analysis in $R_{n}$ _AVHRR and intercomparison with Cloud and the Earth’s Radiant Energy System (CERES) and the European Centre for Medium-Range Weather Forecasts (ECMWF) Interim Re-Analysis (ERA-Interim) products also indicated that the superior of the $R_{n}$ _AVHRR with more detailed information especially in the hot spot regions, such as central tropical Pacific (warming pool), Atlantic and Equatorial Eastern Indian Ocean (EIO). |
Databáze: | OpenAIRE |
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