Abstract

AbstractHeat 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 highest possible temperature levels is challenging given the lack of long homogeneous time series and methodological framework to assess them. Here, we address this challenge by analysing summer temperatures in a nearly 5000-year pre-industrial 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 re-initialized extreme heat waves in the long climate simulation.All methods provide consistent temperature estimates, suggesting that historical exceptional heat waves as in Chicago 1995, Europe 2003 and Russia 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 socio-economic systems to increase resilience to extreme climate stressors.

Highlights

  • Over recent decades, several outstanding heat waves have been recorded across densely populated regions of the world, including Chicago in 1995 (Changnon et al 1996), western Europe in 2003 (García-Herrera et al 2010), Russia in 2010 (Dole et al 2011), and Australia in 2013 (Lewis and Karoly 2013)

  • We argue that the difference in the short-term temperature development between members is largely influenced by differences in circulation anomalies, because the 2-month mean anomalies of surface solar radiation (SSR) and soil moisture (SOIL) hardly change in the boosted ensembles (Fig. S16)

  • In light of recent exceptional heat waves across the world, this study addresses the questions of how much more extreme the recent extreme events could have been relative to the corresponding climatology and what are their driving mechanisms

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Summary

Introduction

Several outstanding heat waves have been recorded across densely populated regions of the world, including Chicago in 1995 (Changnon et al 1996), western Europe in 2003 (García-Herrera et al 2010), Russia in 2010 (Dole et al 2011), and Australia in 2013 (Lewis and Karoly 2013). With increasing atmospheric greenhouse gas concentrations and continuing warming, heat wave frequency, duration, and intensity are projected to strongly increase

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