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Article: Assessment of three satellite-estimated land surface downwelling shortwave irradiance data sets

TitleAssessment of three satellite-estimated land surface downwelling shortwave irradiance data sets
Authors
KeywordsData sets
downwelling shortwave irradiance
satellite-estimated
technology assessment
Issue Date2010
Citation
IEEE Geoscience and Remote Sensing Letters, 2010, v. 7, n. 4, p. 776-780 How to Cite?
AbstractThis letter assesses three satellite-estimated surface downwelling shortwave irradiance data sets: 1) GEWEX-SRB; 2) ISCCP-FD; and 3) CERES-FSW, using ground measurements collected at 36 globally distributed sites from 20002002. SRB and FD solar irradiance are available at three hourly intervals during daytime and FSW hourly solar irradiance is available at late morning. The data are compared to ground measurements at the temporal resolutions of the satellite measurements. Results indicate that the downwelling solar irradiances of the three products show good overall agreement with ground measurements. FSW has an overall coefficient of determination of R2 = 0.69, a bias of 29.7 Wm-2 (6.0% in relative value), and a standard deviation (STD) of 123.2 Wm-2 (25.1% in relative value). The values are 0.83, -5.5Wm-2 (- 1.9%), 101.3 Wm-2 (35.0%) for SRB, and 0.83, 2.8 Wm-2 (0.3%), 101.7 Wm-2 (35.0%) for FD. However, there are substantial uncertainties in these products in some regions. For example, large biases ranging from -90.2 Wm-2 to 45.8 Wm-2 are found in SRB in Southeast Asia. FD has large biases in Southeast Asia (58.9 Wm-2) and Greenland (-33.2)Wm-2. FSW has substantial biases in Southeast Asia (72.6 Wm-2) and Japan (66.5 Wm-2) Wm-2 is 0.35 in Tibetan Plateau and 0.47 in Southeast Asia. © 2006 IEEE.
Persistent Identifierhttp://hdl.handle.net/10722/321423
ISSN
2023 Impact Factor: 4.0
2023 SCImago Journal Rankings: 1.248
ISI Accession Number ID

 

DC FieldValueLanguage
dc.contributor.authorGui, Sheng-
dc.contributor.authorLiang, Shunlin-
dc.contributor.authorWang, Kaicun-
dc.contributor.authorLi, Lin-
dc.contributor.authorZhang, And Xiaotong-
dc.date.accessioned2022-11-03T02:18:49Z-
dc.date.available2022-11-03T02:18:49Z-
dc.date.issued2010-
dc.identifier.citationIEEE Geoscience and Remote Sensing Letters, 2010, v. 7, n. 4, p. 776-780-
dc.identifier.issn1545-598X-
dc.identifier.urihttp://hdl.handle.net/10722/321423-
dc.description.abstractThis letter assesses three satellite-estimated surface downwelling shortwave irradiance data sets: 1) GEWEX-SRB; 2) ISCCP-FD; and 3) CERES-FSW, using ground measurements collected at 36 globally distributed sites from 20002002. SRB and FD solar irradiance are available at three hourly intervals during daytime and FSW hourly solar irradiance is available at late morning. The data are compared to ground measurements at the temporal resolutions of the satellite measurements. Results indicate that the downwelling solar irradiances of the three products show good overall agreement with ground measurements. FSW has an overall coefficient of determination of R2 = 0.69, a bias of 29.7 Wm-2 (6.0% in relative value), and a standard deviation (STD) of 123.2 Wm-2 (25.1% in relative value). The values are 0.83, -5.5Wm-2 (- 1.9%), 101.3 Wm-2 (35.0%) for SRB, and 0.83, 2.8 Wm-2 (0.3%), 101.7 Wm-2 (35.0%) for FD. However, there are substantial uncertainties in these products in some regions. For example, large biases ranging from -90.2 Wm-2 to 45.8 Wm-2 are found in SRB in Southeast Asia. FD has large biases in Southeast Asia (58.9 Wm-2) and Greenland (-33.2)Wm-2. FSW has substantial biases in Southeast Asia (72.6 Wm-2) and Japan (66.5 Wm-2) Wm-2 is 0.35 in Tibetan Plateau and 0.47 in Southeast Asia. © 2006 IEEE.-
dc.languageeng-
dc.relation.ispartofIEEE Geoscience and Remote Sensing Letters-
dc.subjectData sets-
dc.subjectdownwelling shortwave irradiance-
dc.subjectsatellite-estimated-
dc.subjecttechnology assessment-
dc.titleAssessment of three satellite-estimated land surface downwelling shortwave irradiance data sets-
dc.typeArticle-
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.1109/LGRS.2010.2048196-
dc.identifier.scopuseid_2-s2.0-77958016343-
dc.identifier.volume7-
dc.identifier.issue4-
dc.identifier.spage776-
dc.identifier.epage780-
dc.identifier.isiWOS:000283446700033-

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