Fig. 2: Contribution of different processes to the scaling of total moisture convergence.
From: Summer and winter precipitation in East Asia scale with global warming at different rates
a, c, e For JJA; b, d, f for DJF; unit is %/K. a, b Spatial thermodynamics. c, d Dynamics of the mean circulation. e, f Eddy moisture transport (unit: %/K). Stippling represents statistical significance at 5% level in student t test.
