2007
DOI: 10.1080/01431160600887698
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Monitoring Sahelian floodplains using Fourier analysis of MODIS time‐series data and artificial neural networks

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Cited by 28 publications
(12 citation statements)
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“…Wetland areas (CLC41 and CLC42) showed a bimodal pattern (more clearly distinguishable for CLC42) with an early peak in February-March and a long period of high values between June-July to October-November with two sub-peaks for this second half year. Westra and De Wulf [25] also observed this typical pattern of a bimodal temporal distribution for flooded land, resulting in relatively high amplitude values for the second and third harmonic terms. For wetland areas, significant phase variations are expected due to the start and end of the flooding cycle and the density of the flooded vegetation [25].…”
Section: Fourier Transform Parametermentioning
confidence: 95%
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“…Wetland areas (CLC41 and CLC42) showed a bimodal pattern (more clearly distinguishable for CLC42) with an early peak in February-March and a long period of high values between June-July to October-November with two sub-peaks for this second half year. Westra and De Wulf [25] also observed this typical pattern of a bimodal temporal distribution for flooded land, resulting in relatively high amplitude values for the second and third harmonic terms. For wetland areas, significant phase variations are expected due to the start and end of the flooding cycle and the density of the flooded vegetation [25].…”
Section: Fourier Transform Parametermentioning
confidence: 95%
“…Westra and De Wulf [25] also observed this typical pattern of a bimodal temporal distribution for flooded land, resulting in relatively high amplitude values for the second and third harmonic terms. For wetland areas, significant phase variations are expected due to the start and end of the flooding cycle and the density of the flooded vegetation [25]. This phenomenon provides an explanation for the different behaviors (vegetation re-growth after winter) of wetland areas.…”
Section: Fourier Transform Parametermentioning
confidence: 95%
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“…Each individual wave is called a harmonic term and is characterized by its amplitude (height of the maximum), frequency (number of cycles), and phase (delay from time zero). Previous studies have used this method successfully to characterize seasonal changes in natural land-cover and land-use types (Jakubauskas, Legates, and Kastens 2001;Jakubauskas, Legates, and Kastens 2002;Canisius, Turral, and Molden 2007;Westra and De Wulf 2007). Jung and Chang (2015) assessed land-cover change using harmonic analysis.…”
Section: Introductionmentioning
confidence: 99%