2009
DOI: 10.1016/j.rse.2009.06.016
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A sun glint correction method for hyperspectral imagery containing areas with non-negligible water leaving NIR signal

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Cited by 102 publications
(86 citation statements)
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“…The method could not be used at all on the IKONOS data, which has only one NIR band. However, the results presented in [43] suggest that this approach has advantages over other methods in cases where the water-leaving signal is strong, e.g., where vegetation is close to the water surface or the water is less than 2 m deep. shows four wavebands for pixels along the line shown in (a)(i) and (iii) shows a spectral analysis for pixels at each end of the line (i.e., in the glint and no-glint regions).…”
Section: Comments On the Methodsmentioning
confidence: 94%
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“…The method could not be used at all on the IKONOS data, which has only one NIR band. However, the results presented in [43] suggest that this approach has advantages over other methods in cases where the water-leaving signal is strong, e.g., where vegetation is close to the water surface or the water is less than 2 m deep. shows four wavebands for pixels along the line shown in (a)(i) and (iii) shows a spectral analysis for pixels at each end of the line (i.e., in the glint and no-glint regions).…”
Section: Comments On the Methodsmentioning
confidence: 94%
“…Kutser, Vahtmäe and Praks [43] suggest a variant on these methods, which uses information in the oxygen absorption band at 760 nm to assess the size of the glint. They assume that the amount of glint is proportional to the depth of the oxygen absorption feature, D: …”
Section: The Methods Of Kutser Et Almentioning
confidence: 99%
“…Furthermore, classification errors primarily occur at pixels with insufficient sunglint removal. Conventional sunglint removal methods may be suitable to reduce the sunglint and thus also the classification errors [80][81][82]. However, a first attempt to correct the sunglint with the method introduced by Kutser et al, (2009) showed unsatisfactory results.…”
Section: Kelp Detection Results Validated With Diving Transectsmentioning
confidence: 99%
“…Modeling of optical water properties for the littoral zone is more complicated due to rapidly changing water depth and/or substrate and higher amounts of Colored Dissolved Organic Matter (CDOM) and/or suspended particles (phytoplankton, seston, and inorganic particles) compared to the deeper portions of oceans. In addition, bottom backscattering in the shallow areas is more significant, which makes the NIR signals more important, especially in areas that contain substantial amount of seagrasses, benthic algae, or phytoplankton (Kutser et al, 2009) and that the conventional Beer-Lambert's exponential light attenuation with depth is not applicable (Holden & LeDrew, 2002).…”
Section: Dilemmas In Remote Sensing Of Shallow Aquatic System and Savmentioning
confidence: 99%