Preprints
https://doi.org/10.5194/egusphere-2026-5754
https://doi.org/10.5194/egusphere-2026-5754
25 Oct 2026
 | 25 Oct 2026
Status: this preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).

Explaining the rapid 2019–2024 increase in methane emissions from Colombia seen in satellite observations: a high-resolution inverse analysis

Sarah E. Hancock, Daniel J. Jacob, Nicholas Balasus, Carlos Andres Garzon, Ciniro Costa Junior, Matthew R. Johnson, Nikolai Calderón-Cangrejo, Scott Winton, Megan He, Lauren Potyk, Lucas A. Estrada, Rodrigo Jimenez, Andrés Ardila, Luis Morales-Rincon, and James L. France

Abstract. Colombia has been identified as a hotspot of increasing methane emissions over the 2019-2024 period by coarse-resolution global inversion of TROPOMI satellite observations. Here we reproduce this result with a high-resolution (25×25 km2) monthly analytical inversion of TROPOMI observations for the same period conducted within the Integrated Methane Inversion (IMI) framework and evaluated independently with GOSAT and GHGSat satellite observations. Prior estimates for the inversion include spatially-resolved national inventory reports and a measurement-based oil and gas sector inventory for anthropogenic emissions and high-resolution monthly CYGNSS satellite inundation data. We exploit the seasonality in the monthly inversion results to separate wetlands from anthropogenic sources. Total emissions from Colombia optimized by the inversion increase at a best estimated rate (and uncertainty) of 0.23 (0.025–0.46) Tg a-2 (2% a-1) during 2019–2024. Most of this increase is attributed to wetland emissions, peaking in 2021–2022 due to high precipitation driven by La Niña but reflecting interannual variability rather than a sustained trend. Anthropogenic sources account for 34% of the increase driven by cattle population growth, concentrated waste sources near Bogotá, increasing depth of surface coal mines, and fugitive emissions in oil and gas fields. The large seasonal and interannual variability of wetland emissions closely aligns with total water storage anomalies measured by the GRACE satellite instrument, consistent with the importance of water table dynamics in controlling emissions. This work demonstrates that satellite inversions can resolve sectoral drivers of national methane trends and monitor changes in emissions at policy-relevant scales.

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Sarah E. Hancock, Daniel J. Jacob, Nicholas Balasus, Carlos Andres Garzon, Ciniro Costa Junior, Matthew R. Johnson, Nikolai Calderón-Cangrejo, Scott Winton, Megan He, Lauren Potyk, Lucas A. Estrada, Rodrigo Jimenez, Andrés Ardila, Luis Morales-Rincon, and James L. France

Status: open (until 06 Dec 2026)

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Sarah E. Hancock, Daniel J. Jacob, Nicholas Balasus, Carlos Andres Garzon, Ciniro Costa Junior, Matthew R. Johnson, Nikolai Calderón-Cangrejo, Scott Winton, Megan He, Lauren Potyk, Lucas A. Estrada, Rodrigo Jimenez, Andrés Ardila, Luis Morales-Rincon, and James L. France
Sarah E. Hancock, Daniel J. Jacob, Nicholas Balasus, Carlos Andres Garzon, Ciniro Costa Junior, Matthew R. Johnson, Nikolai Calderón-Cangrejo, Scott Winton, Megan He, Lauren Potyk, Lucas A. Estrada, Rodrigo Jimenez, Andrés Ardila, Luis Morales-Rincon, and James L. France
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Latest update: 25 Oct 2026
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Short summary
Satellite observations reveal why methane emissions rose in Colombia during 2019–2024. Wetlands drove most of the increase, with emissions peaking during the wet La Niña years of 2021–2022. Human activities showed a steadier rise, led by livestock, waste, and fossil fuels. Wetland emissions tracked changes in water storage more closely than flooded area alone. These findings help distinguish natural variability from human sources when tracking progress on methane mitigation.
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