Fig. 7: Spatial distribution of the whole layer water vapor flux and its components and water vapor flux divergence in REF and their differences between three levels (I, II, III) and REF.
From: Mechanisms and quantification: How anthropogenic aerosols weaken the East Asian summer monsoon

a REF; b I–REF; c II–REF; d III–REF. The four columns are the whole layer water vapor flux (unit: 100 kg/(m·s)), latitudinal water vapor flux (unit: 100 kg/(m·s)), meridional water vapor flux (unit: 100 kg/(m·s)), and water vapor flux divergence (unit: 10-5kg/(m2·s)).