2016
DOI: 10.1007/s12524-015-0531-8
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Comparison of in-Situ Hyperspectral and Landsat ETM+ Data for Chlorophyll-a Mapping in Case-II Water (Krishnarajapuram Lake, Bangalore)

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Cited by 15 publications
(7 citation statements)
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“…Studies indicate that the spectral response obtained in the field is the collective response of Chl-a and other components/minerals of lake water. Because minerals and other components vary from lake to lake, the spectral bands suitable for Chl-a estimation also vary and should be selected for a model by comparing the estimated values with the measured values obtained from laboratory analysis [22,23].…”
Section: Introductionmentioning
confidence: 99%
“…Studies indicate that the spectral response obtained in the field is the collective response of Chl-a and other components/minerals of lake water. Because minerals and other components vary from lake to lake, the spectral bands suitable for Chl-a estimation also vary and should be selected for a model by comparing the estimated values with the measured values obtained from laboratory analysis [22,23].…”
Section: Introductionmentioning
confidence: 99%
“…Gitelson (1992) argumenta que a magnitude e a posição desses picos podem ser usadas como indicadores precisos do conteúdo de fitoplâncton, e por conseguinte, da concentração de clorofila-a. Ainda assim, a presença desse pico, para Guimarães et al (2017), está associado à baixa absorção pelo pigmento, bem como ao alto espalhamento pela matéria particulada (Murugan et al 2016), de modo que, associando a feição às concentrações da Tabela 1, observa-se que o ponto 3 apresenta menor concentração de clorofila-a e maior reflectância nesse pico. Portanto, o deslocamento do pico para 580 nm, bem como sua magnitude nos espectros, está associado à baixa concentração do pigmento nos pontos amostrais.…”
Section: Ponto Amostralunclassified
“…Substances in the atmosphere such as water vapor, aerosol and cloud particles are bound to exert a certain influence on the reflectance spectrum of ground objects, resulting in a difference between the spectrum received by the sensor and the spectral information of the ground objects themselves [6,42]. Therefore, atmospheric correction should be carried out on the images to remove the effects of the atmosphere, so as to obtain real physical parameters such as reflectance of ground objects and surface temperature.…”
Section: (B) Flaash Atmospheric Correctionmentioning
confidence: 99%