2019
DOI: 10.1002/lom3.10320
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A blended inherent optical property algorithm for global satellite ocean color observations

Abstract: Water inherent optical properties (IOPs) can be derived from satellite‐measured normalized water‐leaving radiance (nLw(λ)) spectra. In this study, we evaluate the performance of the quasi‐analytical algorithm (QAA) and the near‐infrared (NIR)‐based IOP algorithm using a Hydrolight simulation data set covering a wide range of water types that span from clear open ocean to turbid coastal/inland waters. The NIR‐based algorithm produces significantly improved IOP retrievals over turbid coastal and inland waters, w… Show more

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Cited by 27 publications
(12 citation statements)
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“…For these models, in-situ measurements are usually required for training and validating the RS models [27], [28]. The latter has a bio-geo-optical basis in which the relationship between WLR, inherent optical properties, and biochemical constituents are defined through the Radiative Transfer (RT) models [29], [31].…”
Section: Optical Rsmentioning
confidence: 99%
“…For these models, in-situ measurements are usually required for training and validating the RS models [27], [28]. The latter has a bio-geo-optical basis in which the relationship between WLR, inherent optical properties, and biochemical constituents are defined through the Radiative Transfer (RT) models [29], [31].…”
Section: Optical Rsmentioning
confidence: 99%
“…Segregation criteria helped us select the appropriate algorithm to produce accurate IOP products for both open-ocean and turbid coastal waters. It is to be noted that (Shi and Wang, 2019) used nL w (745) based classification criteria for open ocean and coastal waters. However, their discrimination approach resulted in high data noise for moderate coastal turbid waters and did not blend our region's coastal and estuarine optical properties.…”
Section: Conceptual Algorithm Developmentmentioning
confidence: 99%
“…The band-integrated above-water remote-sensing reflectance R rs (L,0 + ) from both datasets was then converted to underwater (just below the surface) remote sensing reflectance r rs (L, 0 -) following (Lee et al, 2002) as described in section 1 of Supplementary Information. r rs (L, 0 -) were processed using a blended QAA algorithm (Shi and Wang, 2019) to estimate total absorption a t (l) and backscattering coefficients b b (l) as the next step of the algorithm development (see Supplementary Information Section 2). The adopted blended algorithm uses a near-infrared (NIR)-based quasi-analytical IOP derivation for turbid coastal/inland waters and Lee's quasi-analytical algorithm (QAA-v6) (IOCCG, 2006) for the open-ocean and less turbid coastal waters.…”
Section: Conceptual Algorithm Developmentmentioning
confidence: 99%
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“…Recent studies [42][43][44] show that the semi-analytical radiance model [20] can be simplified for the nL w (λ) at the NIR wavelengths because the sea water absorption a w (λ) is normally~1-2 orders higher than the other IOP components at the NIR wavelengths. Consequently, the b bp (λ) spectra for all wavelengths between the short blue and NIR can be computed analytically from b bp (λ) values at the two NIR bands (745 and 862 nm) in coastal and inland turbid waters [42].…”
Section: Introductionmentioning
confidence: 99%