As the atmosphere's primary base and one of the main reactive nitrogen compounds, ammonia (NH 3 ) plays a key role in our atmosphere and the global nitrogen cycle (Fowler et al., 2013). Emitted in excess, NH 3 can lead to a dramatic loss of biodiversity and deterioration of water, soil and air quality (Bauer et al., 2016;Bobbink et al., 2010;Sutton, Bleeker, et al., 2013). Unlike other primary gaseous pollutants, such as the acidifying NO x and SO 2 (Aas et al., 2019;Georgoulias et al., 2019), concentrations of NH 3 are steadily increasing in large parts of the world (Sutton et al., 2020;Van Damme et al., 2021). NH 3 has stayed under the radar for long, partially as a result of the historic dearth of measurements. Fortunately, thanks to the availability of new and cheaper techniques, large measurement networks of ground-based stations are gradually put in place (Nair & Yu, 2020;Viatte et al., 2021). In addition, since over a decade, satellites equipped with high-resolution infrared spectrometers offer an unprecedented temporal and spatial sampling of the global NH 3 distributions, which has led to important progress in our understanding of its local to global emission and deposition fluxes and how these are evolving over time (e.g.,