Atmospheric moisture plays a vital role in the hydrological cycle, connecting evaporation sources to precipitationsinks. While high-resolution moisture-tracking models offer valuable insight, discrepancies to atmospheric re-analysis dataemerge. In this study, we reconcile tracked atmospheric water flows with reanalysis data, using the Iterative ProportionalFitting procedure (IPF). We apply IPF to the atmospheric moisture flows from the UTrack dataset (averaged over 2008-2017),aggregated within countries and ocean boundaries. This reconciled dataset ensures that the total tracked atmospheric moisture5equals the total precipitation at the sink and evaporation at the source on an annual basis. Country-scale discrepancies of upto 275% in precipitation and 225% in evaporation are amended, correcting fluxes by∼0.07%, on average. We find 45% ofthe total terrestrial precipitation (∼1.5·105km3yr−1) originates from land evaporation (9.8·104km3yr−1). Our reconciledcountry-scale dataset offers new ground to investigate transboundary atmospheric water flows which connect us globally.