A complete view of the atmospheric hydrologic cycle

• Main Authors: Dey, Dipanjan, Aldama Campino, Aitor, Döös, Kristofer
• Format: Text
• Language: English
• Published: 2021
• Subjects: Canada; Greenland; Indian; Pacific
• Online Access: https://doi.org/10.5194/hess-2021-509; https://hess.copernicus.org/preprints/hess-2021-509/

The global atmospheric water transport from the evaporation to the precipitation regions has been traced using Lagrangian trajectories. A matrix has been constructed by selecting various group of trajectories based on their surface starting(evaporation) and ending (precipitation) positions to show the connectivity of the atmospheric water transport within and between the three major ocean basins and the global landmass. The analysis reveals that a major portion of the evaporated water precipitates back into the same region, namely 67 % for the Indian, 64 % for the Atlantic, 85 % for the Pacific Ocean and 72 % for the global landmass. The evaporation from the subtropical regions of the Indian, Atlantic and Pacific Oceans is found to be the primary source of atmospheric water for precipitation over the Intertropical Convergence Zone (ITCZ) in the corresponding basins. The evaporated waters from the subtropical and western Indian Ocean were traced as the source for precipitation over the South Asian and Eastern African landmass, while Atlantic Ocean waters are responsible for rainfall over North Asia and Western Africa. Atlantic storm tracks were identified as the carrier of atmospheric water that precipitates over Europe, while the Pacific storm tracks were responsible for North American, eastern Asian and Australian precipitation. The bulk of South and Central American precipitation is found to have its source in the tropical Atlantic Ocean. The recycling of evapotranspirated water from land is pronounced over the western coast of South America, Northeastern Asia, Canada and Greenland. The ocean-to-land and land-to-ocean water transport through the atmosphere was computed to be 2 × 10 9 kg/s and 1 × 10 9 kg/s, respectively. The difference between them (net ocean-to-land transport), i.e. 1 × 10 9 kg/s, is transported to land. This net transport is approximately the same as found in previous Eulerian estimates.