2021
DOI: 10.3390/rs13122403
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Evaluation of the J-OFURO3 Sea Surface Net Radiation and Inconsistency Correction

Abstract: A new satellite-based product containing daily sea surface net radiation () values at a spatial resolution of 0.25° from 1988 to 2013, named the Japanese Ocean Flux Data Sets with Use of Remote Sensing Observations, version 3 (J-OFURO3), was recently generated and released. In this letter, the performance of the J-OFURO3 sea-surface product was fully evaluated by using observations from 55 global moored buoy sites. The overall accuracy was satisfactory, with root-mean-square difference (RMSD) of 24.05 and 10.7… Show more

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Cited by 3 publications
(5 citation statements)
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“…It indicates that most oceans underwent a significant change during 1983–2020 with mostly increasing at mid-high latitudes (red color) and only several increasing (e.g., the Indian Ocean and Tropical Center Pacific) and decreasing hot spots (e.g. the seas to northern Australia, western Africa and South America) over tropical seas, which were coincident with the results of previous studies 13 , 68 70 . The remarkable increased ocean surface R n over most oceans at high latitudes where the rate was even as large as 2 Wm −2 per year was speculated caused by the increased absorbed solar radiation because of the reduced ocean surface albedo due to the sea ice or glacier melting caused by global warming 71 , but the case was unexpected over the Norway sea (68°N – 80°N, 10°W – 45°E) where the ocean surface R n overly decreased at a rate of ~0.5 Wm −2 per year.…”
Section: Technical Validationsupporting
confidence: 88%
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“…It indicates that most oceans underwent a significant change during 1983–2020 with mostly increasing at mid-high latitudes (red color) and only several increasing (e.g., the Indian Ocean and Tropical Center Pacific) and decreasing hot spots (e.g. the seas to northern Australia, western Africa and South America) over tropical seas, which were coincident with the results of previous studies 13 , 68 70 . The remarkable increased ocean surface R n over most oceans at high latitudes where the rate was even as large as 2 Wm −2 per year was speculated caused by the increased absorbed solar radiation because of the reduced ocean surface albedo due to the sea ice or glacier melting caused by global warming 71 , but the case was unexpected over the Norway sea (68°N – 80°N, 10°W – 45°E) where the ocean surface R n overly decreased at a rate of ~0.5 Wm −2 per year.…”
Section: Technical Validationsupporting
confidence: 88%
“…Specifically, six products covering 1988–2016 were used for fusion including two remotely sensed products (CERES4 and ISCCP-FH) and four reanalysis products (JRA-55, MERRA2, NCEP R2, and ERA5), and five products were used for comparison including one remotely sensed product (GEWEX-SRB), three reconstructed products (TropFlux, OAFlux, and J-OFURO3), and one ship-based product (NOCS V2.0). Note that J-OFURO3 which was thought to be one of the best products in ocean surface R n 13 was mainly considered as a reference. Table 2 lists the characteristics of the 11 used ocean surface R n products.…”
Section: Methodsmentioning
confidence: 99%
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“…Fourth, Chen et al [36] evaluated the performance of the J-OFURO3 (the Japanese Ocean Flux Data Sets with Use of Remote Sensing Observations, version3) sea-surface net-radiation data set using buoy observations from 55 sites. The validation results showed that the overall accuracy of J-OFURO3 sea-surface net radiation was satisfactory, but an inconsistency issue occurred in long-term sea-surface net radiation variations.…”
Section: Overview Of Contributionsmentioning
confidence: 99%