Improving low-quality satellite remote sensing reflectance at blue bands over coastal and inland waters
The satellite remote sensing reflectance (Rrs(λ)) at two short blue bands (410 or 412 nm and 443 nm) are prone to large uncertainties in coastal and inland waters, prohibiting algorithms from generating reliable ocean color products associated with these bands. In this study, we developed an algorit...
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| Published in | Remote sensing of environment Vol. 250; p. 112029 |
|---|---|
| Main Authors | , , , , |
| Format | Journal Article |
| Language | English |
| Published |
New York
Elsevier Inc
01.12.2020
Elsevier BV |
| Subjects | |
| Online Access | Get full text |
| ISSN | 0034-4257 1879-0704 |
| DOI | 10.1016/j.rse.2020.112029 |
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| Abstract | The satellite remote sensing reflectance (Rrs(λ)) at two short blue bands (410 or 412 nm and 443 nm) are prone to large uncertainties in coastal and inland waters, prohibiting algorithms from generating reliable ocean color products associated with these bands. In this study, we developed an algorithm to estimate Rrs(41×) and Rrs(443) when the satellite Rrs(λ) in blue bands suffer from large uncertainties. The algorithm first determines the Rrs(λ) spectral shape from the satellite-measured Rrs(λ) values at three wavelengths of 48× (486, 488, or 490), 55× (547, 551, or 555), and 67× (667, 670, or 671) nm. The algorithm then derives Rrs(41×) and Rrs(443) from the estimated Rrs(λ) spectral shape with algebraic formulations. We assessed the algorithm performance with satellite (SeaWiFS, MODISA, and VIIRS-SNPP) and in situ Rrs(λ) matchups from global waters. It is shown that the uncertainties of estimated Rrs(41×) and Rrs(443) are substantially smaller than the original satellite products when applicable. Besides, implementation of the algorithm contributes to a significant increase in the number of utilizable Rrs(41×) and Rrs(443) values. The algorithm is relatively stable and is best applicable to the satellite Rrs(λ) spectra for which the Rrs(48×) and Rrs(55×) measurements are subject to small uncertainties. The demonstrations support the application of the blue-band estimation algorithm to a wide range of coastal waters.
•A spectral shape based algorithm is developed to estimate Rrs(41×) and Rrs(443).•The algorithm can greatly increase the satellite Rrs data quality and quantity.•It allows for more accurate and increased number of valid ocean color retrievals. |
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| AbstractList | The satellite remote sensing reflectance (Rrs(λ)) at two short blue bands (410 or 412 nm and 443 nm) are prone to large uncertainties in coastal and inland waters, prohibiting algorithms from generating reliable ocean color products associated with these bands. In this study, we developed an algorithm to estimate Rrs(41×) and Rrs(443) when the satellite Rrs(λ) in blue bands suffer from large uncertainties. The algorithm first determines the Rrs(λ) spectral shape from the satellite-measured Rrs(λ) values at three wavelengths of 48× (486, 488, or 490), 55× (547, 551, or 555), and 67× (667, 670, or 671) nm. The algorithm then derives Rrs(41×) and Rrs(443) from the estimated Rrs(λ) spectral shape with algebraic formulations. We assessed the algorithm performance with satellite (SeaWiFS, MODISA, and VIIRS-SNPP) and in situ Rrs(λ) matchups from global waters. It is shown that the uncertainties of estimated Rrs(41×) and Rrs(443) are substantially smaller than the original satellite products when applicable. Besides, implementation of the algorithm contributes to a significant increase in the number of utilizable Rrs(41×) and Rrs(443) values. The algorithm is relatively stable and is best applicable to the satellite Rrs(λ) spectra for which the Rrs(48×) and Rrs(55×) measurements are subject to small uncertainties. The demonstrations support the application of the blue-band estimation algorithm to a wide range of coastal waters.
•A spectral shape based algorithm is developed to estimate Rrs(41×) and Rrs(443).•The algorithm can greatly increase the satellite Rrs data quality and quantity.•It allows for more accurate and increased number of valid ocean color retrievals. The satellite remote sensing reflectance (Rᵣₛ(λ)) at two short blue bands (410 or 412 nm and 443 nm) are prone to large uncertainties in coastal and inland waters, prohibiting algorithms from generating reliable ocean color products associated with these bands. In this study, we developed an algorithm to estimate Rᵣₛ(41×) and Rᵣₛ(443) when the satellite Rᵣₛ(λ) in blue bands suffer from large uncertainties. The algorithm first determines the Rᵣₛ(λ) spectral shape from the satellite-measured Rᵣₛ(λ) values at three wavelengths of 48× (486, 488, or 490), 55× (547, 551, or 555), and 67× (667, 670, or 671) nm. The algorithm then derives Rᵣₛ(41×) and Rᵣₛ(443) from the estimated Rᵣₛ(λ) spectral shape with algebraic formulations. We assessed the algorithm performance with satellite (SeaWiFS, MODISA, and VIIRS-SNPP) and in situ Rᵣₛ(λ) matchups from global waters. It is shown that the uncertainties of estimated Rᵣₛ(41×) and Rᵣₛ(443) are substantially smaller than the original satellite products when applicable. Besides, implementation of the algorithm contributes to a significant increase in the number of utilizable Rᵣₛ(41×) and Rᵣₛ(443) values. The algorithm is relatively stable and is best applicable to the satellite Rᵣₛ(λ) spectra for which the Rᵣₛ(48×) and Rᵣₛ(55×) measurements are subject to small uncertainties. The demonstrations support the application of the blue-band estimation algorithm to a wide range of coastal waters. The satellite remote sensing reflectance (Rrs(λ)) at two short blue bands (410 or 412 nm and 443 nm) are prone to large uncertainties in coastal and inland waters, prohibiting algorithms from generating reliable ocean color products associated with these bands. In this study, we developed an algorithm to estimate Rrs(41×) and Rrs(443) when the satellite Rrs(λ) in blue bands suffer from large uncertainties. The algorithm first determines the Rrs(λ) spectral shape from the satellite-measured Rrs(λ) values at three wavelengths of 48× (486, 488, or 490), 55× (547, 551, or 555), and 67× (667, 670, or 671) nm. The algorithm then derives Rrs(41×) and Rrs(443) from the estimated Rrs(λ) spectral shape with algebraic formulations. We assessed the algorithm performance with satellite (SeaWiFS, MODISA, and VIIRS-SNPP) and in situ Rrs(λ) matchups from global waters. It is shown that the uncertainties of estimated Rrs(41×) and Rrs(443) are substantially smaller than the original satellite products when applicable. Besides, implementation of the algorithm contributes to a significant increase in the number of utilizable Rrs(41×) and Rrs(443) values. The algorithm is relatively stable and is best applicable to the satellite Rrs(λ) spectra for which the Rrs(48×) and Rrs(55×) measurements are subject to small uncertainties. The demonstrations support the application of the blue-band estimation algorithm to a wide range of coastal waters. |
| ArticleNumber | 112029 |
| Author | Lee, Zhongping Yu, Xiaolong Wang, Menghua Jiang, Lide Wei, Jianwei |
| Author_xml | – sequence: 1 givenname: Jianwei orcidid: 0000-0002-6872-3534 surname: Wei fullname: Wei, Jianwei email: jianwei.wei@noaa.gov organization: NOAA Center for Satellite Applications and Research, College Park, MD 20740, USA – sequence: 2 givenname: Xiaolong orcidid: 0000-0003-2813-0854 surname: Yu fullname: Yu, Xiaolong organization: State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen 361102, China – sequence: 3 givenname: Zhongping surname: Lee fullname: Lee, Zhongping organization: School for the Environment, University of Massachusetts Boston, Boston, MA 02125, USA – sequence: 4 givenname: Menghua orcidid: 0000-0001-7019-3125 surname: Wang fullname: Wang, Menghua organization: NOAA Center for Satellite Applications and Research, College Park, MD 20740, USA – sequence: 5 givenname: Lide orcidid: 0000-0002-9883-4411 surname: Jiang fullname: Jiang, Lide organization: NOAA Center for Satellite Applications and Research, College Park, MD 20740, USA |
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| Snippet | The satellite remote sensing reflectance (Rrs(λ)) at two short blue bands (410 or 412 nm and 443 nm) are prone to large uncertainties in coastal and inland... The satellite remote sensing reflectance (Rrs(λ)) at two short blue bands (410 or 412 nm and 443 nm) are prone to large uncertainties in coastal and inland... The satellite remote sensing reflectance (Rᵣₛ(λ)) at two short blue bands (410 or 412 nm and 443 nm) are prone to large uncertainties in coastal and inland... |
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| SubjectTerms | Algorithms Atmospheric correction Blue bands Coastal waters color environment Inland waters MODIS Ocean color Reflectance Remote sensing Remote sensing reflectance Satellites SeaWiFS Spectra Spectral shape Uncertainty VIIRS Wavelengths |
| Title | Improving low-quality satellite remote sensing reflectance at blue bands over coastal and inland waters |
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