Thursday, 1 February 2024: 9:00 AM
339 (The Baltimore Convention Center)
Wetlands are the largest natural source of methane (CH4) emissions globally. Northern wetlands CH4 emissions may accelerate under intensified warming in the Arctic and subsequent permafrost thaw. Although top-down atmospheric inversions of wetland CH4 emissions differ from bottom-up estimates of process models, the two estimates are not completely independent as atmospheric inversions would take process-based estimation as priors in the model. Data-driven upscaling instead provides independent estimates of large-scale methane fluxes. To upscale wetland CH4 fluxes at high latitudes (>45° N), we developed a machine learning framework (WetCH4) based on eddy covariance observations, reanalysis, and remote sensing constraints from Soil Moisture Active Passive (SMAP) soil moisture and MODIS reflectance. Our results modeled from 155 site-years across 26 sites of wetland EC data with accuracies of a mean R2 of 0.46 and 0.62 and the mean absolute error (MAE) of 19.4 nmol m-2 s-1 and 21 nmol m-2 s-1, for daily and monthly fluxes, respectively. With a dynamic wetland inundation dataset, WetCH4 estimated average annual CH4 emissions of 22.3 ± 2.5 Tg CH4 yr-1 from Arctic and boreal wetlands for 2016-2022, with 86% emitted during the May-October period. The estimated magnitude and seasonal cycle of CH4 emissions aligned with estimates of process-based models. Furthermore, a comparison of our estimated fluxes with inversions of aircraft-observed concentration data in the North Slope area underscores the significance of accurately delineating wet-emitting surfaces in this region to reduce estimation uncertainty. In summary, WetCH4 provides daily wetland CH4 fluxes from 2016 to 2022, facilitating investigations into the global CH4 budget and wetland responses to climate change through a robust, data-driven perspective.

