EGU26-21165, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-21165
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Thursday, 07 May, 14:00–15:45 (CEST), Display time Thursday, 07 May, 14:00–18:00
 
Hall X5, X5.34
Towards robust global CH₄ emission inversions: Insights into the impact of parametric weighting of TROPOMI observations
Santiago Parraguez Cerda1, Johann Rasmus Nüß1, Nikos Daskalakis1, Arjo Segers2, Oliver Schneising1, Michael Buchwitz1, Mihalis Vrekoussis1,3,4, and Maria Kanakidou1,5,6
Santiago Parraguez Cerda et al.
  • 1Institute of Environmental Physics (IUP), University of Bremen, Bremen, Germany
  • 2Netherlands Organisation for Applied Scientific Research (TNO), Utrecht, The Netherlands
  • 3Center of Marine Environmental Sciences (MARUM), University of Bremen, Bremen, Germany
  • 4Climate and Atmosphere Research Center (CARE-C), The Cyprus Institute, Nicosia, Cyprus
  • 5Environmental Chemical Processes Laboratory (ECPL), University of Crete, Heraklion, Greece
  • 6Center for Studies of Air Quality and Climate Change (C-STACC), Foundation for Research and Technology Hellas (FORTH), Patras, Greece

Satellite observations are critical for global monitoring of trace gases like methane (CH₄), a potent greenhouse gas, but challenges remain in assimilating dense satellite data alongside sparser in situ measurements within inverse modelling systems. Here, we present a parametric regularisation method that computes observation-specific weights based on the spatial and temporal coverage of satellite data, enabling balanced assimilation across densely and sparsely observed regions. This approach is implemented as a preprocessing step, preserving computational efficiency by maintaining a fixed covariance matrix, and is adaptable for use with multiple satellite products in combined inversions.

Applied to global methane inversions using the TM5-MP/4DVAR system at 1° × 1° resolution for 2019 with TROPOMI observations, our method reduces grid cell weight variability by approximately 20% compared to a constant weighting approach. This adaptation effectively increases the influence of observations from regions with sparse satellite coverage, such as high latitudes and oceans, while reducing over-representation from densely sampled areas. The redistributed weights lead to localised but notable changes in optimised methane fluxes, especially in regions like Southeast Asia and South America, but the global posterior budget remains consistent with the latest Global Methane Budget estimates.

Comparison against independent TCCON and NOAA measurements confirms the robustness of the parametric weighting. Overall, the proposed methodology offers a robust, efficient, and easily generalizable framework for assimilating satellite observations, improving constraints on methane emissions globally, and providing a foundation for future multi-product inversions.

How to cite: Parraguez Cerda, S., Nüß, J. R., Daskalakis, N., Segers, A., Schneising, O., Buchwitz, M., Vrekoussis, M., and Kanakidou, M.: Towards robust global CH₄ emission inversions: Insights into the impact of parametric weighting of TROPOMI observations, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-21165, https://doi.org/10.5194/egusphere-egu26-21165, 2026.