1993
DOI: 10.1080/01431169308904363
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Remote sensing of submerged vegetation canopies for biomass estimation

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Cited by 119 publications
(74 citation statements)
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“…The model is limited to wavelengths from 400 nm to 700 nm and to sun zenith angles from 25 • to 65 • . Due to strong absorption of water in the near-infrared wavelengths the characteristic spectral features normally are superimposed by water absorption [41]. Hence, several surface models of reflectance intensities could be processed for each sun zenith angle.…”
Section: Reflectance Modelmentioning
confidence: 99%
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“…The model is limited to wavelengths from 400 nm to 700 nm and to sun zenith angles from 25 • to 65 • . Due to strong absorption of water in the near-infrared wavelengths the characteristic spectral features normally are superimposed by water absorption [41]. Hence, several surface models of reflectance intensities could be processed for each sun zenith angle.…”
Section: Reflectance Modelmentioning
confidence: 99%
“…At the beginning of the growing season, the spectral response, even of sparsely vegetated areas, is sediment-dominated. Organic material on the lake bottom such as epiphytes and detritus may alter the spectral response of bare sediment [6,13,[39][40][41]. During the growing season, changes in macrophyte/sediment coverage ratio, leaf size and orientation, leaf pigment concentrations and cellular structure specifically influence intensity and shape of spectral signatures [6,13,40].…”
Section: Introductionmentioning
confidence: 99%
“…Due to strong attenuation of water in near-infrared wavelengths ( Figure 2) this feature is normally superimposed by water absorption [23]. To minimize the influence of water absorption, ( ) was included in the index calculation.…”
Section: Differentiation Of Littoral Bottom Coveragementioning
confidence: 99%
“…In particular, Y 3,4 covered a characteristic vegetation feature, the red edge, i.e., the passage where reflectance strongly increases between visible red and near infrared wavelengths. Due to strong attenuation of water in near-infrared wavelengths ( Figure 2) this feature is normally superimposed by water absorption [23]. To minimize the influence of water absorption, K d (λ) was included in the index calculation.…”
Section: Differentiation Of Littoral Bottom Coveragementioning
confidence: 99%
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