4.7 Article

Heat Stress Indicators in CMIP6: Estimating Future Trends and Exceedances of Impact-Relevant Thresholds

Journal

EARTHS FUTURE
Volume 9, Issue 3, Pages -

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2020EF001885

Keywords

climate change; climate extremes; global climate modeling; heat stress; heat‐ related health impacts; thermal indices

Funding

  1. European Union's Horizon 2020 research and innovation program [820655]
  2. Belmont Forum Collaborative Research Action on Climate, Environment, and Health - Norwegian Research Council [310672]

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This study calculated trends of heat stress indicators in different climate models under global warming, finding significant increases in all regions globally. The research indicates that different heat stress indicators show substantial variations in exceeding impact-relevant thresholds, highlighting the importance of selecting appropriate indicators and thresholds for reliable assessments.
Global warming is leading to increased heat stress in many regions around the world. An extensive number of heat stress indicators (HSIs) has been developed to measure the associated impacts on human health. Here we calculate eight HSIs for global climate models participating in the Coupled Model Intercomparison Project Phase 6 (CMIP6). We compare their future trends as function of global mean temperature, with particular focus on highly populated regions. All analyzed HSIs increase significantly (p < 0.01) in all considered regions. Moreover, the different HSIs reveal a substantial spread ranging from trends close to the rate of global mean temperature up to an amplification of more than a factor of two. Trends change considerably when normalizing the HSIs by accounting for the different scales on which they are defined, but the large spread and strong trends remain. Consistently, exceedances of impact-relevant thresholds are strongly increasing globally, including in several densely populated regions, but also show substantial spread across the selected HSIs. The indicators with the highest exceedance rates vary for different threshold levels, suggesting that the large indicator spread is associated both to differences in trend magnitude and the definition of threshold levels. These results highlight the importance of choosing indicators and thresholds that are appropriate for the respective impact under consideration. Additionally, further validation of HSIs regarding their capability to quantify heat impacts on human health on regional-to-global scales would be of great value for assessing global impacts of future heat stress more reliably.

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