Abstract Extreme weather events that occur concurrently are especially damaging to society, agriculture, the economy, and ecosystems. Here, we investigate the spatial distribution, trends, persistence properties, and temporal shifts of concurrent heatwaves and droughts (CHWDs) across Canada from 1979 to 2018. Our results indicate that the regions of British Columbia and the Prairies are more susceptible to a high number of CHWDs and the Arctic region is affected by less frequent but more intense CHWDs (on average 44 and 25 events respectively). The Arctic regions also have the highest increasing trend of CHWDs due to the higher trends of temperature as compared to other regions. We also explore the relationship of CHWDs with large‐scale climate drivers. The North Atlantic Oscillation has the most influence on the CHWDs affecting the coastal regions and the Arctic. EP‐NP and WP also show a correlation with the CHWD events occurring in central Canada. A relatively high persistence in northeast Canada, coupled with the increasing trend of the total duration of CHWDs, highlights the increasing risk of CHWDs. We note that the timing of CHWDs shifts toward early summer in parts of the Yukon and Northwest Territories and toward late summer in the Canadian Arctic Archipelago. The changes in the number of concurrent events, their total duration, and temporal shifts of occurrence should be incorporated into adaptation and mitigation policies. The rapid variability and inconsistency of CHWDs across Canada emphasize the critical need for region‐specific hazard assessments that incorporate these concurrent extreme events.
Sinha et al. (2025) studied this question.