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Journal of Geophysical Research (Planets), vol. 108, No. E9, 5105, doi: 10.1029/2002JE001975, 2003
by Gregg A. Swayze, Roger N. Clark, Alexander F.H. Goetz, Thomas G. Chrien, and Noel S. Gorelick
Reference:
Estimates of spectrometer bandpass, sampling interval, and
signal-to-noise ratio required for identification of pure minerals and
plants were derived using reflectance spectra convolved to AVIRIS,
HYDICE, MIVIS, VIMS, and other imaging spectrometers. For each spectral
simulation, various levels of random noise were added to the reflectance
spectra after convolution and then each was analyzed with the
Tetracorder spectral identification algorithm (Clark et al., 2003).
The outcome of each identification attempt was tabulated to provide an
estimate of the signal-to-noise ratio at which a given percentage of the
noisy spectra were identified correctly. Results show that spectral
identification is most sensitive to the signal-to-noise ratio at
narrow sampling interval values but is more sensitive to the sampling
interval itself at broad sampling interval values because of spectral
aliasing a condition when absorption features of different materials
can resemble one another. The bandpass is less critical to spectral
identification than the sampling interval or signal-to-noise ratio
because broadening the bandpass does not induce spectral aliasing.
These conclusions are empirically corroborated by analysis of mineral
maps of AVIRIS data collected at Cuprite, Nevada between 1990 and 1995,
a period during which the sensor signal-to-noise ratio increased up to
sixfold. There are values of spectrometer sampling and bandpass beyond
which spectral identification of materials will require an abrupt
increase in sensor signal-to-noise ratio due to the effects of spectral
aliasing. Factors that control this threshold are the uniqueness of a
material's diagnostic absorptions in terms of shape and wavelength
isolation, and the spectral diversity of the materials found in nature
and in the spectral library used for comparison. Array spectrometers
provide the best data for identification when they critically sample
spectra. The sampling interval should not be broadened to increase the
signal-to-noise ratio in a photon-noise-limited system when high levels
of accuracy are desired. It is possible, using this simulation method,
to select optimum combinations of bandpass, sampling interval, and
signal-to-noise ratio values for a particular application that maximize
identification accuracy and minimize the volume of imaging data.
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U.S. Geological Survey,
a bureau of the U.S. Department of the Interior
Swayze,G. A., R. N. Clark, A. F. H. Goetz, T. G. Chrien,
and N. S. Gorelick, Effects of spectrometer band pass, sampling, and
signal-to-noise ratio on spectral identification using the Tetracorder
algorithm, J. Geoph. Research (Planets), vol. 108, No. E9, 5105,
doi: 10.1029/2002JE001975, 2003.
Abstract
Pre-print PDF Version:
Text and figures (6 Mbytes).
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This page is maintained by: Dr. Gregg A. Swayze gswayze@speclab.cr.usgs.gov
Last modified Jan. 18, 2008.