Convection-permitting WRF simulation of extreme winds in Canada: Present and future scenarios

This study investigates extreme wind events across southern Canada using 4-km convection-permitting WRF simulations under present (CTRL) and future (PGW) climate scenarios. The high resolution allows explicit representation of convective processes and complex terrain, improving local-scale wind prediction. We analyze three distinct regions—the central Prairies, Rocky Mountains, and southern Ontario—and find strong spatial and seasonal contrasts. Under future conditions, summer wind extremes intensify notably in the Prairies and southern Ontario, while winter winds decrease in the Prairies but increase in Ontario, Quebec, and mountainous areas. A conditional probability analysis based on Convective Available Potential Energy (CAPE) reveals that the likelihood of destructive winds (>20 m/s) rises significantly in convectively unstable environments. In southern Ontario, the probability under strong instability (CAPE > 2500 J/kg) increases from nearly zero to 0.4. We also apply the Peaks-over-Threshold (POT) method to estimate 50-year return period wind speeds, which show substantial future increases, up to 6 m/s in some areas during summer. These changes indicate a rising threat from convectively driven wind extremes. This study highlights the value of convection-permitting models in resolving local wind features and emphasizes the need for region-specific adaptation strategies. The findings critically impact wind hazard assessment, infrastructure design, and climate resilience planning across southern Canada. • Identify regional and seasonal contrasts in Canadian extreme wind patterns • Use 4-km WRF to simulate convection and complex terrain effects • Project stronger summer winds in Prairies and Ontario under future climate • Link destructive wind events to high CAPE environments in southern Ontario