Estimation of chromophoric dissolved organic matter in the Mississippi and Atchafalaya river plume regions using above-surface hyperspectral remote sensing
A method for the inversion of hyperspectral remote sensing was developed to determine the absorption coefficient for chromophoric dissolved organic matter (CDOM) in the Mississippi and Atchafalaya river plume regions and the northern Gulf of Mexico, where water types vary from Case 1 to turbid Case...
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Published in | Journal of Geophysical Research Vol. 116; no. C2 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
Published |
Washington
Blackwell Publishing Ltd
01.02.2011
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Subjects | |
Online Access | Get full text |
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Summary: | A method for the inversion of hyperspectral remote sensing was developed to determine the absorption coefficient for chromophoric dissolved organic matter (CDOM) in the Mississippi and Atchafalaya river plume regions and the northern Gulf of Mexico, where water types vary from Case 1 to turbid Case 2. Above‐surface hyperspectral remote sensing data were measured by a ship‐mounted spectroradiometer and then used to estimate CDOM. Simultaneously, water absorption and attenuation coefficients, CDOM and chlorophyll fluorescence, turbidities, and other related water properties were also measured at very high resolution (0.5–2 m) using in situ, underwater, and flow‐through (shipboard, pumped) optical sensors. We separate ag, the absorption coefficient a of CDOM, from adg (a of CDOM and nonalgal particles) based on two absorption‐backscattering relationships. The first is between ad (a of nonalgal particles) and bbp (total particulate backscattering coefficient), and the second is between ap (a of total particles) and bbp. These two relationships are referred as ad‐based and ap‐based methods, respectively. Consequently, based on Lee's quasi‐analytical algorithm (QAA), we developed the so‐called Extended Quasi‐Analytical Algorithm (QAA‐E) to decompose adg, using both ad‐based and ap‐based methods. The absorption‐backscattering relationships and the QAA‐E were tested using synthetic and in situ data from the International Ocean‐Colour Coordinating Group (IOCCG) as well as our own field data. The results indicate the ad‐based method is relatively better than the ap‐based method. The accuracy of CDOM estimation is significantly improved by separating ag from adg (R2 = 0.81 and 0.65 for synthetic and in situ data, respectively). The sensitivities of the newly introduced coefficients were also analyzed to ensure QAA‐E is robust. |
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Bibliography: | ark:/67375/WNG-F41S5VMR-S ArticleID:2010JC006523 Tab-delimited Table 1.Tab-delimited Table 2.Tab-delimited Table A1.Tab-delimited Table A2. istex:5D5C4C9CC1FEB35A83160C7C05ACD031F0E28A80 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0148-0227 2169-9275 2156-2202 2169-9291 |
DOI: | 10.1029/2010JC006523 |