4.7 Article

Very Rare Heat Extremes: Quantifying and Understanding Using Ensemble Reinitialization

Journal

JOURNAL OF CLIMATE
Volume 34, Issue 16, Pages 6619-6634

Publisher

AMER METEOROLOGICAL SOC
DOI: 10.1175/JCLI-D-20-0916.1

Keywords

Atmosphere-land interaction; Atmospheric circulation; Extreme events; Summer; warm season; Surface temperature; Regression analysis; Statistical techniques; Ensembles

Funding

  1. Swiss National Science Foundation SNSF [200020_178778]
  2. Swiss National Science Foundation (SNF) [200020_178778] Funding Source: Swiss National Science Foundation (SNF)

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This study investigates the potential for unseen extreme heat waves by analyzing preindustrial climate model simulations. The findings suggest that historical heat waves in Chicago, Europe, and Russia could have been substantially exceeded even without further global warming. The study highlights the importance of combining different approaches to assess extreme heat wave scenarios beyond observational records for adaptation and resilience building.
Heat waves such as the one in Europe 2003 have severe consequences for the economy, society, and ecosystems. It is unclear whether temperatures could have exceeded these anomalies even without further climate change. Developing storylines and quantifying the highest possible temperature levels is challenging given the lack of a long homogeneous time series and methodological framework to assess them. Here, we address this challenge by analyzing summer temperatures in a nearly 5000-yr preindustrial climate model simulation, performed with the Community Earth System Model CESM1. To assess how anomalous temperatures could get, we compare storylines generated by three different methods: 1) a return-level estimate, deduced from a generalized extreme value distribution; 2) a regression model, based on dynamic and thermodynamic heat wave drivers; and 3) a novel ensemble boosting method, generating large samples of reinitialized extreme heat waves in the long climate simulation. All methods provide consistent temperature estimates, suggesting that historical exceptional heat waves such as those in Chicago in 1995, Europe in 2003, and Russia in 2010 could have been substantially exceeded even in the absence of further global warming. These estimated unseen heat waves are caused by the same drivers as moderate observed events, but with more anomalous patterns. Moreover, altered contributions of circulation and soil moisture to temperature anomalies include amplified feedbacks in the surface energy budget. The methodological framework of combining different storyline approaches of heat waves with magnitudes beyond the observational record may ultimately contribute to adaptation and to the stress testing of ecosystems or socioeconomic systems to increase resilience to extreme climate stressors.

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