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Climate change : a global science update Valrie Masson-Delmotte @valmasdel Introduction Current global warming in context Human influence on extreme events Implications of warming targets Sea level A tremendous scientific


  1. Climate change : a global science update Valérie Masson-Delmotte @valmasdel

  2. • Introduction • Current global warming in context • Human influence on extreme events • Implications of warming targets • Sea level

  3. A tremendous scientific endeavour Quantitative paleoclimate Fluid physics Supercomputers Thermodynamics Satellites Radiative transfers 17 th Century 19 th Century Late 20 th Century Antiquity Middle Age Meteorological Networks Key concepts instruments Ice ages Climate modelling Greenhouse effect Statistical analyses  A vast scientific community  Curiosity-driven research  Societal and policy relevance

  4. From knowledge production… 20000 Number of peer-review papers with « climate change » keyword 15000 10000 5000 0 1970 1975 1980 1985 1990 1995 2000 2005 2010 2015

  5. Climate projections : IPCC AR5 Emission pathways Radiative perturbation (W/m 2 ) carbon volcanoe s Assessing risks Simulated climate response (°C) clouds regional sea level extremes

  6. Von Schuckmann et al, Nature Climate Change, 2016

  7. • Introduction • Current global warming in context • Human influence on extreme events • Implications of warming targets • Sea level

  8. Where do we stand now for global mean temperature? Z. Hausfather

  9. Where do we stand now with respect to pre-industrial levels? Hawkins et al, BAMS, 2017

  10. Where do we stand now with respect to the current and last interglacial periods ? Current interglacial period (Holocene) Last interglacial period (Eemian) Hansen et al, ESD, 2017

  11. Where do we stand now with respect to earlier climate projections? Z. Hausfather

  12. What are the drivers of climate change? Sunshade effect Heat – trapping gases

  13. What are the cumulative contributions to the carbon budget?

  14. What is the best estimate of human influence on global warming? IPCC, 2013

  15. • Introduction • Current global warming in context • Human influence on extreme events • Implications of warming targets • New developments for projections

  16. How are extreme events affected by human influence? NAS, 2016

  17. How are extreme events affected by human influence? Example of a heavy rainfall event : Seine and Loire river basins, May 29-31, 2016  3 day precipitation extremes in April-June : the probability of a 3-day spring extreme rainfall has increased by 80-90% due to human influence on the climate system wwa.climatecentral.org  30-40% reduced common wheat yield due to the wet spring Source : Agritel WWA Agritel

  18. How are extreme events affected by human influence? Recent major drought events :  California : rainfall deficit linked to natural variability, water stress enhanced by warming trend Griffin et al, GRL, 2014 ; Williams et al, GRL 2015 ; Diffenbaugh et al, PNAS, 2015 ; Cheng et al.,2016, J Clim  Levant region : drought twice more likely due to human influence on drying and warming trends Bergaoui et al., 2015, BAMS ; Cook et al, JGR, 2016, Kelley et al, PNAS, 2015

  19. How are extreme events affected by human influence? Arctic, autumn 2016 2016 1958-2002 DMI

  20. How are extreme events affected by human influence? Arctic, autumn 2016 2016  Highly unlikely event in a pre- industrial climate  In 2050, business as usual scenario : about one year out of two Reference : 1979-2004 Simulations with natural and all forcings (1901-2026) Reanalyses year by year since 1979 wwa.climatecentral.org

  21. • Introduction • Current global warming in context • Human influence on extreme events • Implications of warming targets • New developments for projections

  22. What are the implications of 1.5, 2 ° C warming or more? Hot days Knutti et al, Nat. Geo., 2015

  23. What are the implications of 1.5 or 2 ° C warming for potential impacts? Schleussner et al, Nature Climate Change, 2016

  24. Which projection methods are fit for purpose? Example of European Alps Global climate models Regional climate models Simulated summer precipitation change  European Alps summer precipitation : regional models simulate a robust increase in convective precipitation at high elevations Giorgi et al, Nature Geoscience, 2016

  25. What are the implications of 1.5 or 2 ° C warming for potential impacts? 2 °C may not be sufficient to avoid the loss of summer Arctic sea ice Loss of 3 ± 0.3 m 2 of September Arctic sea ice for each ton CO 2 emitted Screen & Williamson, NCC, 2017 Notz and Stroeve, Science, 2016

  26. What are the implications of climate targets for cumulative CO 2 emissions? <2.0 ° C, >66% Indicative range 450-1050 GtCO 2 20 years 800 GtCO 2 2100 GtCO 2 IPCC 2013; Global Carbon Project 2016

  27. What are the emission trajectories compatible with climate targets? Rogelj et al, Nature, 2016

  28. How can the uncertainty on climate sensitivity be reduced? Emergent contraints : links between observable cloud properties, feedbacks, and climate sensitivity Schneider et al, Nature Climate Change, 2017

  29. How can the uncertainty on land carbon feedbacks be reduced? Emergent contraints : links between evapotranspiration and gross primary production  Multi-model spread in net biome productivity reduced by more than 30% by 2100  Doubled projected decline in land sink Mystakidis et al, Global Change Biology, 2016

  30. When do climate models produce abrupt changes? Drijfhout et al, PNAS, 2015

  31. • Introduction • Current global warming in context • Human influence on extreme events • Implications of warming targets • Sea level

  32. Why has sea level rise accelerated? 25% Greenland 5% Antarctica Terrestrial water Glaciers Ocean thermal expansion Chen et al, Nature Climate Change, 2017

  33. How much could ice sheets contribute to sea level rise? Only the collapse of marine-based sectors of the Antarctic ice sheet, if initiated, could cause global mean sea level to rise substantially above the likely range during the 21st century Multi-millennial sea level rise IPCC, 2013

  34. How much could ice sheets contribute to sea level rise? Marine ice cliff instability Marine ice sheet instability Projected Antarctic contribution to sea level rise DeConto and Pollard, Nature, 2016

  35. To conclude  New knowledge is under development, from multiple lines of evidence : paleoclimate, observations, process studies, theory and numerical models - to document and understand past and current changes - to evaluate model fit for purpose and confidence in projections - to develop regional climate information and near term predictions  Close interplay between developments in climate science and needs for risk assessment, adaptation and mitigation solution options  Challenges to knowledge developments worldwide : long term observation networks, satellite programs, computing resources, data distribution centers for climate model results, and human resources

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