Reflectance spectra collected August 16, 2022, at Smith Creek Valley, Nevada, with an ASD FieldSpecⓇ 4 Hi-Res NG spectrometer for calibration/validation of imaging spectrometer data

A full description of all collection and processing steps is included in this data release as: ‘SmithCreekPlayaNV_16aug2022_ProcessingSteps.pdf’. Reflectance data were collected using Malvern Panalytical ASD FieldSpec® 4 Hi-Res NG Spectroradiometers with custom VNIR gratings (hereafter referred to a...

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Hauptverfasser: John M Meyer, Raymond Kokaly, Todd M Hoefen, Evan M Cox, Gregg A Swayze
Format: Dataset
Sprache:eng
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Zusammenfassung:A full description of all collection and processing steps is included in this data release as: ‘SmithCreekPlayaNV_16aug2022_ProcessingSteps.pdf’. Reflectance data were collected using Malvern Panalytical ASD FieldSpec® 4 Hi-Res NG Spectroradiometers with custom VNIR gratings (hereafter referred to as ASD spectrometers) on August 16, 2022, at a field site in Smith Creek Valley, Nevada, USA. The ASD spectrometers used have a spectral range of 0.35 to 2.5 micronswith 2151 channels of data reported (Malvern Panalytical, 2018). Reflected sunlight was measured with the bare fiber (no fore optic), having a field of view of ~22 degrees, while traversing the area of the field site. Additional measurements of reflected artificial light were made at discrete sample points within the field site using an ASD Hi-Brite Contact Probe. Averages of relative reflectance spectra for the field site were computed separately from the sunlight and artificial light measurements. These averages were converted from relative reflectance to absolute reflectance by compensating for the absorption properties of the reference panel, a National Institute of Standards and Technology traceable Labsphere Spectralon® 99% reflective panel. Parts of the averaged artificial light spectrum were merged with the averaged sunlight spectrum because atmospheric gases, e.g., water vapor, oxygen, and carbon dioxide, have strong absorption in parts of the measured wavelength region and the ASD spectrometers have low signal-to-noise ratio in parts of that wavelength range. To form the merged average absolute reflectance spectrum, segments of the averaged absolute reflectance from the artificial light measurements were scaled multiplicatively and merged with the averaged absolute reflectance from sunlight measurements. The merged spectrum is suitable for comparison with imaging spectrometer data across the full ASD wavelength range. At the field site, representative hand samples were collected. These samples were measured at the U.S. Geological Survey (USGS) laboratories in Denver, Colorado, using an ASD spectrometer. In this data release we provide the following data files in the specified formats; 1. Raw ASD spectrometer binary files recorded on the spectrometer in ASD Indico format (.asd files; Malvern Panalytical, 2018), 2. Latitude, longitude coordinates, date and UTC times of acquisition, and other metadata for all recorded field spectra in comma separated value (CSV) format (.csv extension) 3. Avera
DOI:10.5066/p9e2tsdf