2017
DOI: 10.1016/j.jqsrt.2017.05.033
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Predicting the diurnal blue-sky albedo of soils using their laboratory reflectance spectra and roughness indices

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Cited by 18 publications
(13 citation statements)
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“…The state of cell structures, photosynthetically active pigments, water, lignin and cellulose content determines the spectral reflectance curve in different parts of the electromagnetic spectrum [7]. In addition, the relationship between absorbed and scattered photons allows an exploration of the stress resistance mechanism(s) according to species properties [8][9][10]. main source of information, ASD FieldSpec 3/4 hyperspectral measurements were used to analyze interactions between the electromagnetic spectrum and the morphology and physiology of plants.…”
Section: Introductionmentioning
confidence: 99%
“…The state of cell structures, photosynthetically active pigments, water, lignin and cellulose content determines the spectral reflectance curve in different parts of the electromagnetic spectrum [7]. In addition, the relationship between absorbed and scattered photons allows an exploration of the stress resistance mechanism(s) according to species properties [8][9][10]. main source of information, ASD FieldSpec 3/4 hyperspectral measurements were used to analyze interactions between the electromagnetic spectrum and the morphology and physiology of plants.…”
Section: Introductionmentioning
confidence: 99%
“…Quantitative studies of vegetation are related to plant indices [24]; they require calibration with biophysical variables [25]. Currently, they are used to assess crops, e.g., soil property modeling [26,27], irrigation efficiency [28], adaptation to stress factors [29], and the identification of dominant types of meadows [30] or forests [31,32]. Narrowband indices acquired from spectrometric measurements are applicable for assessing vegetation vigor, e.g., chlorophyll concentration or change in pigment concentration during the growing season [33].…”
Section: Introductionmentioning
confidence: 99%
“…The surface roughness is a parameter that can reflect the geometric structure of the underlying surface. High surface roughness increases the reflections of solar radiation, resulting in a decrease in surface albedo [42,43]. The roughness of semi-fixed and fixed dunes is higher than that of shifting and semishifting dunes.…”
Section: Spatial and Temporal Differences In Surface Albedo Over Different Underlying Surfacesmentioning
confidence: 99%