2019
DOI: 10.1016/j.rse.2019.05.015
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The ECOSTRESS spectral library version 1.0

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Cited by 253 publications
(162 citation statements)
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References 58 publications
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“…(a) spectra for gray/buff samples from 0.35 to 2.5 µm showing several features due to H 2 O, OH, NH 4 , and sulfate in these samples, (b) spectra from 1.3-2.5 µm including also NH 4 -bearing minerals. Vertical lines mark features due to minerals or species in these samples: dotted lines at 1.41 and 1.91 µm due to bound H 2 O in clays (Bishop et al, 1994) or zeolite (e.g., clinoptilolite, USGS spectral library, Clark et al, 1990), dashed lines at 1.45-1.48 and 1.94-1.97 µm due to H 2 O in hydrated sulfates such as hexahydrite (e.g., Bishop et al, 2009) or tschermigite (speclib.jpl.nasa.gov/library; Meerdink et al, 2019), solid lines at 1.56, 2.01 and 2.11 µm due to NH 4 + in minerals (e.g., Bishop et al, 2002;Berg et al, 2016), yellow solid lines at 1.47 and 2.26 µm due to Fe-OH in jarosite (Bishop and Murad, 2005), broken lines at 2.17 and 2.21 µm due to Al-OH in alunite (Bishop and Murad, 2005) and montmorillonite (e.g., Bishop et al, 2008), respectively. This is the peer-reviewed, final accepted version for American Mineralogist, published by the Mineralogical Society of America.…”
Section: Figure Captionsmentioning
confidence: 99%
“…(a) spectra for gray/buff samples from 0.35 to 2.5 µm showing several features due to H 2 O, OH, NH 4 , and sulfate in these samples, (b) spectra from 1.3-2.5 µm including also NH 4 -bearing minerals. Vertical lines mark features due to minerals or species in these samples: dotted lines at 1.41 and 1.91 µm due to bound H 2 O in clays (Bishop et al, 1994) or zeolite (e.g., clinoptilolite, USGS spectral library, Clark et al, 1990), dashed lines at 1.45-1.48 and 1.94-1.97 µm due to H 2 O in hydrated sulfates such as hexahydrite (e.g., Bishop et al, 2009) or tschermigite (speclib.jpl.nasa.gov/library; Meerdink et al, 2019), solid lines at 1.56, 2.01 and 2.11 µm due to NH 4 + in minerals (e.g., Bishop et al, 2002;Berg et al, 2016), yellow solid lines at 1.47 and 2.26 µm due to Fe-OH in jarosite (Bishop and Murad, 2005), broken lines at 2.17 and 2.21 µm due to Al-OH in alunite (Bishop and Murad, 2005) and montmorillonite (e.g., Bishop et al, 2008), respectively. This is the peer-reviewed, final accepted version for American Mineralogist, published by the Mineralogical Society of America.…”
Section: Figure Captionsmentioning
confidence: 99%
“…The surface reflectance for Sentinel-2 pixels classified as vegetation are scaled by a factor 0.82 in order to account for the generally lower reflectance by vegetation in the SWIR-2 window compared to Sentinel-2's band 12. 25 The scaling factor has been derived using spectral reflectance data from the ECOSTRESS spectral library (Baldridge et al, 2009;Meerdink et al). Figure 8b shows the gridded surface reflectance data for Indianapolis together with a corresponding RGB composite (Fig.…”
Section: Surface Albedo Data From Sentinel-2 15mentioning
confidence: 99%
“…We used the point value corresponding with the coordinates for the site (Table 1), the data is provided at 70 m spatial resolution. ESI is evapotranspiration/potential evapotranspiration and is a local short-term measure of water deficit for plants (Meerdink et al 2019), whereas aridity is a measure of overall climate.…”
Section: Site Descriptionmentioning
confidence: 99%