2021
DOI: 10.1016/j.rse.2021.112574
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Impact of scene-specific enhancement spectra on matched filter greenhouse gas retrievals from imaging spectroscopy

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Cited by 23 publications
(12 citation statements)
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“…The other spectral region spans from 2100 to 2500 nm, exhibiting a stronger CH4 absorption signal. The 𝒌 spectrum can be generated by MODerate resolution atmospheric TRANsmission (MODTRAN; Berk et al, 2014) radiative transfer model (Foote et al, 2021). Moreover, spectral features vary from satellites due to different spectral response functions (SRF).…”
Section: Mf Methodsmentioning
confidence: 99%
“…The other spectral region spans from 2100 to 2500 nm, exhibiting a stronger CH4 absorption signal. The 𝒌 spectrum can be generated by MODerate resolution atmospheric TRANsmission (MODTRAN; Berk et al, 2014) radiative transfer model (Foote et al, 2021). Moreover, spectral features vary from satellites due to different spectral response functions (SRF).…”
Section: Mf Methodsmentioning
confidence: 99%
“…First, it uses wavelength bands within the range 1,928–2,200 nm where CO 2 has strong absorption effects on the radiance. Second, it simulates CO 2 concentration enhancements above background, starting at 0 ppm‐m and incrementally doubling up from 20,000 to 1,280,000 ppm‐m (Foote et al., 2021). Finally, it applies an independent matched filter to a group of 50 adjacent columns of the image to improve the covariance estimate by suppressing artifacts from non‐uniformity among detector elements (Ayasse et al., 2019).…”
Section: Methodsmentioning
confidence: 99%
“…They estimated emissions from 17 coal and gas fired power plants in the U.S. with robust correlation with simultaneous in situ measured data. Foote et al (2021) also quantified seven CO 2 emissions examples, concluding that generating the scene-specific unit enhancement spectra could achieve quantification improvement. However, these studies have primarily focused on power plants, as they are often high-volume point sources of CO 2 emissions equipped with continuous emissions monitoring systems (CEMS) that provide in situ measured data for calibration purposes (U.S. EPA, 2023).…”
mentioning
confidence: 99%
“…where i ∈ [0,n] are the pixels selected through manual plume segmentation, S is the area of a pixel, and αi is the concentration path length enhancement within each pixel. The constant k represents the conversion factor from concentration-path length (in ppm-m) to mass of CH4 (typically in kilograms); it is derived by dividing the molecular mass of the gas and the volume of one mole of an ideal gas at standard pressure and temperature with appropriate unit conversions (Duren et al 2019;Foote et al 2021). To minimize the variability of IME with respect to rc, IME is calculated for the entire range of radii (rc) then its standard deviation (σIME/rc), representing the uncertainty in IME/rc estimates, is calculated.…”
Section: Plume Detection and Emission Flux Estimationmentioning
confidence: 99%