Quantification of atmospheric carbon dioxide from the Geostationary Operational Environmental Satellite (GOES East)

arXiv:2605.23991 · physics.ao-ph, astro-ph.EP, cs.LG · Submitted 2026-05-17 · Read on arXiv

Aaron Sonabend-W, Sean Campbell, John Platt, Christopher Van Arsdale, Anna M. Michalak

physics.ao-ph, astro-ph.EP, cs.LG

Submitted: 2026-05-17

Comments: 28 pages, 9 figures, 1 table

License: http://creativecommons.org/licenses/by/4.0/

The gist: There is a growing urgency to track greenhouse gasses with the resolution, precision and accuracy needed to support independent verification of CO 2 fluxes at local to global scales.

Terminology

Abstract

There is a growing urgency to track greenhouse gasses with the resolution, precision and accuracy needed to support independent verification of CO 2 fluxes at local to global scales. The current generation of space-based sensors, however, only provides sparse observations in space and time. This challenge has fueled interest in the potential use of data from existing missions originally developed for other applications to infer global greenhouse gas variability. The Advanced Baseline Imager (ABI) onboard the Geostationary Operational Environmental Satellite (GOES-East), operational since 2017, provides full coverage of much of the western hemisphere at 10-minute intervals from geostationary orbit across 16 spectral channels at an approximately 2 km squared spatial resolution. Here, we leverage this high spatial coverage and temporal revisit to develop Deep XCO 2, a single-pixel, physics-guided neural network to estimate dry-air column CO 2 mole fraction (XCO 2). Deep XCO 2 employs a time series of GOES-East's 16 spectral bands, ECMWF ERA5 lower tropospheric meteorology, MODIS surface reflectance, solar and satellite viewing geometry, and day of year. The network was trained on collocated GOES-East and OCO-2/OCO-3 observations. Deep XCO 2 is able to capture realistic XCO 2 variability when compared against a held-out year of OCO-2 and OCO-3 observations, and against observations from the TCCON network. We also present case studies illustrating the use of Deep XCO 2 to observe XCO 2 enhancements over urban areas and drawdown over agricultural regions. Overall, while the precision of GOES-East derived XCO 2 can never rival that of dedicated instruments, the unprecedented combination of contiguous geographic coverage, 10-minute temporal frequency, and multi-year record offers the potential to observe aspects of atmospheric CO 2 variability currently unseen from space.

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