Changes of western European heat wave characteristics projected by the CMIP5 ensemble

We investigate heat waves defined as periods of at least 3 consecutive days of extremely high daily maximum temperature affecting at least 30 % of western Europe. This definition has been chosen to select heat waves that might impact western European electricity supply. Even though not all such heat waves threaten it, the definition allows to identify a sufficient number of events, the strongest being potentially harmful. The heat waves are characterised by their duration, spatial extent, intensity and severity. The heat wave characteristics are calculated for historical and future climate based on results of climate model simulations conducted during the 5th Phase of the Coupled Model Intercomparison Project (CMIP5). The uncertainty of future anthropogenic forcing is taken into account by analysing results for the Representative Concentration Pathway scenarios RCP2.6, RCP4.5 and RCP8.5. The historical simulations are evaluated against the EOBS gridded station data. The CMIP5 ensemble median captures well the observed mean heat wave characteristics. However, no model simulates a heat wave as severe as observed during August 2003. Under future climate conditions, the heat waves become more frequent and have higher mean duration, extent and intensity. The ensemble spread is larger than the scenario uncertainty. The shift of the temperature distribution is more important for the increase of the cumulative heat wave severity than the broadening of the temperature distribution. However, the broadening leads to an amplification of the cumulative heat wave severity by a factor of 1.7 for RCP4.5 and 1.5 for RCP8.5.

[1]  J. Barros,et al.  Applying neighbourhood classification systems to natural hazards: a case study of Mt Vesuvius , 2010, Natural Hazards.

[2]  Sonia I. Seneviratne,et al.  Observational evidence for soil-moisture impact on hot extremes in southeastern Europe , 2011 .

[3]  Constantine Photopoulos Evaluation and Response , 2008 .

[4]  Stefan Rahmstorf,et al.  A decade of weather extremes , 2012 .

[5]  A. Mariotti,et al.  Future Climate Projections , 2013 .

[6]  Andrés M. Alonso,et al.  Summarising changes in air temperature over Central Europe by quantile regression and clustering , 2011 .

[7]  H. Douville,et al.  Evaluation and response of winter cold spells over Western Europe in CMIP5 models , 2012, Climate Dynamics.

[8]  Pascal Yiou,et al.  Asymmetric European summer heat predictability from wet and dry southern winters and springs , 2012 .

[9]  G. Meehl,et al.  More Intense, More Frequent, and Longer Lasting Heat Waves in the 21st Century , 2004, Science.

[10]  Lisa V. Alexander,et al.  On the Measurement of Heat Waves , 2013 .

[11]  F. Zwiers,et al.  Changes in temperature and precipitation extremes in the CMIP5 ensemble , 2013, Climatic Change.

[12]  H. Douville,et al.  European temperatures in CMIP5: origins of present-day biases and future uncertainties , 2013, Climate Dynamics.

[13]  E. Fischer,et al.  Consistent geographical patterns of changes in high-impact European heatwaves , 2010 .

[14]  A. Thomson,et al.  The representative concentration pathways: an overview , 2011 .

[15]  Ricardo García-Herrera,et al.  The Hot Summer of 2010: Redrawing the Temperature Record Map of Europe , 2011, Science.

[16]  Ralf Koppmann,et al.  Joint modelling of obstacle induced and mesoscale changes—Current limits and challenges , 2011 .

[17]  S. Savić,et al.  Cold and warm air temperature spells during the winter and summer seasons and their impact on energy consumption in urban areas , 2014, Natural Hazards.

[18]  D. Lüthi,et al.  The role of increasing temperature variability in European summer heatwaves , 2004, Nature.

[19]  F. Ludwig,et al.  Vulnerability of US and European electricity supply to climate change , 2012 .

[20]  Milo E. Hoffman,et al.  Calculation of the thermal response of buildings by the total thermal time constant method , 1981 .

[21]  G. Hegerl,et al.  Influence of Modes of Climate Variability on Global Temperature Extremes , 2008 .

[22]  M. Rummukainen,et al.  Evaluating the performance and utility of regional climate models: the PRUDENCE project , 2007 .

[23]  S. Seneviratne,et al.  Land–atmosphere coupling and climate change in Europe , 2006, Nature.

[24]  P. Jones,et al.  A European daily high-resolution gridded data set of surface temperature and precipitation for 1950-2006 , 2008 .

[25]  A. Pezza,et al.  More Frequent, Longer, and Hotter Heat Waves for Australia in the Twenty-First Century , 2014 .

[26]  F. Zwiers,et al.  Climate extremes indices in the CMIP5 multimodel ensemble: Part 2. Future climate projections , 2013 .

[27]  Simon J. Brown,et al.  Do global warming targets limit heatwave risk? , 2010 .

[28]  H. Douville,et al.  The CNRM-CM5.1 global climate model: description and basic evaluation , 2013, Climate Dynamics.

[29]  D. Stephenson,et al.  Future extreme events in European climate: an exploration of regional climate model projections , 2007 .

[30]  Karl E. Taylor,et al.  An overview of CMIP5 and the experiment design , 2012 .

[31]  S. Seneviratne,et al.  Impact of soil moisture–atmosphere coupling on European climate extremes and trends in a regional climate model , 2011 .

[32]  Katherine A. Samolyk A regional perspective on the credit view , 1991 .

[33]  M. Beniston The 2003 heat wave in Europe: A shape of things to come? An analysis based on Swiss climatological data and model simulations , 2004 .

[34]  T. Palmer,et al.  Changing frequency of occurrence of extreme seasonal temperatures under global warming , 2005 .

[35]  S. Seneviratne,et al.  A regional perspective on trends in continental evaporation , 2009 .

[36]  Chris Hewitt,et al.  Ensembles-based predictions of climate changes and their impacts , 2004 .

[37]  Ngar-Cheung Lau,et al.  Model Simulation and Projection of European Heat Waves in Present-Day and Future Climates , 2014 .