资源环境科技发展态势分析平台

Projected precipitation changes in a warming climate vary considerably, spatially and between intensities. The changes can be greater or less than the ~7% K^‐1 Clausius‐‐Clapeyron (CC) prediction, owing to dynamic effects. Using two global‐climate‐model large ensembles, we quantify the dynamically‐induced changes to precipitation extremes from the present (1996‐‐2005) to late‐21st‐Century (2071‐‐2080) climates, as a function of recurrence interval, focusing on the subtropics. We separate non‐CC changes into a term proportional to the present‐day vertical‐velocity spatial pattern (i.e., an amplification or damping thereof by a constant factor) and a residual. The amplitude term varies with recurrence interval, approximately canceling (doubling) CC for moderate (large) extremes, increasing precipitation variability. Contrastingly, the residual is quasi‐uniform across recurrence intervals but spatially heterogeneous, weakening extremes over dry zones. This residual may be related to Hadley Cell expansion, although this explanation is insufficient to explain many features, and other possible mechanisms are discussed.