Projected increase in compound dry and hot events over global land areas

Under global warming, dry and hot events have been increasing in recent decades and are projected to increase in the future across global land areas. The impacts of compound dry and hot events may lead to increased stress to the natural and human systems than separate dry or hot events. Thus, quantitative assessments of global land areas affected by these compound events are needed to understand their risks. This study focuses on the variation in global land and cropland areas affected by compound dry and hot events for both historical and future periods using observations from Climatic Research Unit (CRU) and simulations from Coupled Model Intercomparison Project Phase 5 (CMIP5) climate models. Based on historical observations and simulations, a substantial increase in the spatial extent of these compound events was detected, especially since the 1980s. Climate model projections under the Representative Concentration Pathway (RCP) 8.5 scenario reveal that both global land and cropland areas affected by compound dry and hot events will increase to approximately 1.7-1.8 times by the end of the 21st century. Based on different thresholds of compound events, the spatial extent of global land areas during the June-July-August (December-January-February) season will increase by 12.38-17.20% (7.83-11.19%) in 2050-2099 relative to that in 1950-1999, and the spatial extent of global cropland areas will increase by 14.69-19.63% (9.60-14.48%). The increase in areas affected by compound dry and hot events may lead to more losses in different sectors in the future and more efforts are needed to cope with their potential impacts.

Automated summary

Under global warming, the frequency of dry and hot events is increasing, leading to greater stress on natural and human systems. This study shows a significant increase in the spatial extent of compound dry and hot events since the 1980s, with projections indicating further expansion in the future. Efforts are needed to cope with potential impacts from the increasing areas affected by compound dry and hot events.