2012
DOI: 10.14358/pers.78.2.119
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An Empirical Model-based Method for Signal Restoration of SWIR in ASD Field Spectroradiometry

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Cited by 15 publications
(21 citation statements)
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“…Third, the significant water absorption valleys could be seen at the spectral regions centered at 1450 and 1910 nm. The depth and the area of the absorption valley are negatively closely related to leaf RWC (Lin et al, 2012). Finally, a water-stressed leaf reflectance peaked at around 2000 nm as the RWC was less than or equal to 16 %.…”
Section: Reflectance Spectra Of Fresh and Water-stressed Leafmentioning
confidence: 95%
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“…Third, the significant water absorption valleys could be seen at the spectral regions centered at 1450 and 1910 nm. The depth and the area of the absorption valley are negatively closely related to leaf RWC (Lin et al, 2012). Finally, a water-stressed leaf reflectance peaked at around 2000 nm as the RWC was less than or equal to 16 %.…”
Section: Reflectance Spectra Of Fresh and Water-stressed Leafmentioning
confidence: 95%
“…Typical reflectance of vegetation in the visible-infrared region will increase as water deficit occurs (Knipling, 1970;Gausman and Allen, 1973;Gausman et al, 1982;Hunt and Rock, 1989;Carter, 1991 and1993;Ceccato et al, 2001;Zygielbaum et al, 2009;Lin et al, 2012). As leaves dehydrate or vegetation suffers water stress, leaf water potential becomes increasingly negative and the rate of photosynthesis is reduced (Nilsen and Orcutt, 1996;Montagu and Woo, 1999;Keenan et al, 2009;Lavoir et al, 2009) because water deficit can cause chlorophyll degradation and thus significantly decreases foliar chlorophyll concentration (Kirnak et al, 2001;Pirzad et al, 2011;Desotgiu et al, 2012;Ghorbanli et al, 2013).…”
Section: Indexmentioning
confidence: 99%
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“…This problem is particularly pronounced in 1350-1410 nm and 1700-1900 nm because of the broad absorption of atmospheric water vapor [15], thus these spectra are rarely used in practical sensing [16][17][18][19][20]. Even though the low signal-to-noise ratio (SNR) is considered as troublesome, the absorption feature centered at 1450 nm and 1940 nm has been demonstrated as quite valuable for estimating the water content of plants [21][22][23][24] and nitrogen content [25][26][27]. In general, a degraded hyperspectral is represented as a combination of a true signal and additive noise and a denoising method is designed to estimate the original signal by penalized least squares optimization [28].…”
Section: Introductionmentioning
confidence: 99%