High-resolution global atmospheric moisture connections from evaporation to precipitation
High-resolution global atmospheric moisture connections from evaporation to precipitation
O. Tuinenburg,J. Theeuwen,A. Staal
2020 · DOI: 10.5194/essd-2020-89
Earth System Science Data · 125 Citations
Abstract
Abstract. A key Earth system process is the circulation of evaporated
moisture through the atmosphere. Spatial connections between evaporation andprecipitation affect the global and regional climates by redistributingwater and latent heat. Through this atmospheric moisture recycling,land cover changes influence regional precipitation patterns, withpotentially far-reaching effects on human livelihoods and biomedistributions across the globe. However, a globally complete dataset ofatmospheric moisture flows from evaporation to precipitation has beenlacking so far. Here we present a dataset of global atmospheric moisturerecycling on both 0.5∘ and 1.0∘ spatial resolution. Wesimulated the moisture flows between each pair of cells across all land andoceans for 2008–2017 and present their monthly climatological means. Weapplied the Lagrangian moisture tracking model UTrack, which is forced withERA5 reanalysis data on 25 atmospheric layers and hourly wind speeds anddirections. Due to the global coverage of the simulations, a completepicture of both the upwind source areas of precipitation and downwind targetareas of evaporation can be obtained. We show a number of statistics ofglobal atmospheric moisture flows: land recycling, basin recycling, meanlatitudinal and longitudinal flows, absolute latitudinal and longitudinalflows, and basin recycling for the 26 largest river basins. We find that, onaverage, 70 % of global land evaporation rains down over land, varyingbetween 62 % and 74 % across the year; 51 % of global landprecipitation has evaporated from land, varying between 36 % and 57 %across the year. The highest basin recycling occurs in the Amazon and Congobasins, with evaporation and precipitation recycling of 63 % and 36 %for the Amazon basin and 60 % and 47 % for the Congo basin. Thesestatistics are examples of the potential usage of the dataset, which allowsusers to identify and quantify the moisture flows from and to any area onEarth, from local to global scales. The dataset is available at https://doi.org/10.1594/PANGAEA.912710 (Tuinenburg etal., 2020).