Global warming is assumed to accelerate the global water cycle. However,
quantification of the acceleration and regional analyses remain open.
Accordingly, in this study we address the fundamental hydrological
question: Is the water cycle regionally accelerating/decelerating under
global warming? For our investigation we have implemented the
age-weighted regional water tagging approach into the Weather Research
and Forecasting WRF model, namely WRF-age, to follow the atmospheric
water pathways and to derive atmospheric water residence times
accordingly. Moreover, we have implemented the three-dimensional online
budget analysis of the total, tagged, and aged atmospheric water into
WRF-age to provide a prognostic equation of the atmospheric water
residence times. The newly developed, physics-based WRF-age model is
used to regionally downscale the reanalysis of ERA-Interim and the
MPI-ESM Representative Concentration Pathway 8.5 scenario (RCP8.5)
simulation exemplarily for an East Asian monsoon region, i.e., the
Poyang Lake basin (the tagged moisture source area), for two 10-year
slices of historical (1980-1989) and future (2040-2049) times. In
comparison to the historical simulation, the future 2-meter temperature
rises by +1.4 °C, evaporation increases by +6%, and precipitation
decreases by -38% under RCP8.5 on average. In this context, global
warming leads to regionally decreased residence times for the tagged
water vapor by 8 hours and the tagged condensed moisture by 12 hours in
the atmosphere, but increased transit times for the tagged precipitation
by 4 hours over the land surface that is partly attributed to a slower
fallout of precipitating moisture components in the atmosphere under
global warming.