Fig. 10

a Time series of precipitation and other components of moisture budget over SE China (unit: mm day⁻¹). b is same as Fig. 7b, but for the linear trends in vertical velocity (unit:10^–2 Pa s⁻¹ decade⁻¹). c-d are same as Fig. 6a and 6c, respectively, but for the linear trend in horizontal wind (vectors; unit: m s⁻¹ decade⁻¹) and geopotential height (shading; unit: m decade⁻¹). The Tibetan Plateau region with elevations exceeding 3000 m is shaded gray