Transcript Slide 1
Analysis of extremes in a changing climate in support of informed decisions for adaptation [email protected] EURANDOM & KNMI, May 2009 Agenda • Changing climate extremes • Traditional practices • WMO guidance document • Analyses of extremes • Take home message EURANDOM & KNMI, May 2009 EURANDOM & KNMI, May 2009 Changing climate extremes • IPCC-AR4: ‘confidence has increased that some extremes will become more frequent, more widespread and/or more intense during the 21st century’ EURANDOM & KNMI, May 2009 EURANDOM & KNMI, May 2009 Changing climate extremes • Definitions? – High impact events – Exceedence of a relatively low threshold (e.g., 95th percentile of daily precipitation amounts) – Rare events (long return periods) – Unprecedented events (in the available record) EURANDOM & KNMI, May 2009 Changing climate extremes • Definitions? – High impact events – Exceedence of a relatively low threshold (e.g., 95th percentile of daily precipitation amounts) – Rare events (long return periods) – Unprecedented events (in the available record) • Wide range of space and time scales – From very small scale (tornadoes) to large scale (drought) EURANDOM & KNMI, May 2009 Extremes table IPCC-AR4, WG1 report EURANDOM & KNMI, May 2009 Traditional practices • Design criteria for safety of infrastructure are typically based on historical observations of extremes, assuming a stationary climate EURANDOM & KNMI, May 2009 Traditional practices • Design criteria for safety of infrastructure are typically based on historical observations of extremes, assuming a stationary climate • Methods fit extreme value distributions to selected observations of extremes EURANDOM & KNMI, May 2009 Annual maxima of daily precipitation amounts Station De Bilt, the Netherlands, 1906-2003 EURANDOM & KNMI, May 2009 Map of daily rainfall, 31 July 2002 EVT estimates: 70 mm: once in 50yr 50 mm : once in 5yr EURANDOM & KNMI, May 2009 11 August 2002 EURANDOM & KNMI, May 2009 31 July 2002 24 August 2002 11 August 2002 EURANDOM & KNMI, May 2009 31 July 2002 Traditional practices • Climate change makes it likely that there will be change in some extremes that lies outside the envelope of constant variability assumed under stationary climate conditions EURANDOM & KNMI, May 2009 Traditional practices • Climate change makes it likely that there will be change in some extremes that lies outside the envelope of constant variability assumed under stationary climate conditions • Adaptation strategies should begin to take into account the observed and projected changes in extremes EURANDOM & KNMI, May 2009 WMO Guidance document • A new WMO/WCRP guidance document on this topic is now in press: – Albert M.G. Klein Tank, Francis W. Zwiers and Xuebin Zhang, 2009: Analysis of climate and weather extremes in a changing climate in support of informed decisions for adaptation. WMO/TD-No ???? EURANDOM & KNMI, May 2009 WMO Guidance document • Targeted at National Meteorological and Hydrological Services (NMHSs) around the world • Aim is: – to help build capacity to identify and describe changes in extremes, and – to improve the information services on extremes under climate change conditions EURANDOM & KNMI, May 2009 WMO Guidance document • The focus is on climate extremes defined as rare events within the statistical reference distribution of particular weather elements that are monitored daily at a particular place, such as temperature and precipitation • More complicated weather elements that involve compound factors, such as tropical cyclones or storm surges, fall outside the scope EURANDOM & KNMI, May 2009 Analysis of extremes • Need long and quality controlled observational series with high time resolution 3 2 TN, Amos (Canada) °C 1 0 -1 -2 1927 -3 1910 1920 1963 1930 1940 1950 1960 EURANDOM & KNMI, May 2009 1970 1980 1990 2000 Analysis of extremes • Tests for nonclimatic jumps and/or gradual shifts due to changes in station location, environment (exposure), instrumentation or observing practices EURANDOM & KNMI, May 2009 Analysis of extremes • For analyzing moderate extremes an internationally coordinated set of descriptive indices can be used, which describe frequency, amplitude, persistence • User-friendly R-based software (RClimDex) for their calculation is available from http://cccma.seos.uvic.ca/ETCCDI EURANDOM & KNMI, May 2009 Analysis of extremes • For analyzing moderate extremes an internationally coordinated set of descriptive indices can be used, which describe frequency, amplitude, persistence • User-friendly R-based software (RClimDex) for their calculation is available from http://cccma.seos.uvic.ca/ETCCDI • One key approach involves counting the number of days in a season or a year that exceed specific thresholds EURANDOM & KNMI, May 2009 Analysis of extremes upper 10-ptile 1961-1990 the year 1996 lower 10-ptile 1961-1990 EURANDOM & KNMI, May 2009 Analysis of extremes upper 10-ptile 1961-1990 the year 1996 lower 10-ptile 1961-1990 EURANDOM & KNMI, May 2009 “cold nights” Analysis of extremes “warm nights” upper 10-ptile 1961-1990 the year 1996 lower 10-ptile 1961-1990 EURANDOM & KNMI, May 2009 “cold nights” Analysis of extremes De Bilt, the Netherlands EURANDOM & KNMI, May 2009 Analysis of extremes • The results (in a series of journal papers) contributed to IPCC-AR4, Ch3 AR4 map of observed trends (days per decade) for 1951 to 2003 (Alexander et al., JGR, 2006) EURANDOM & KNMI, May 2009 Analysis of extremes • The results (in a series of journal papers) contributed to IPCC-AR4, Ch3 – Workshops held post-AR4 – New workshops organized in 2009 EURANDOM & KNMI, May 2009 AR4 map of observed trends (days per decade) for 1951 to 2003 (Alexander et al., JGR, 2006) Analysis of extremes Linking the trends in extremes indices to regional circulation changes Example for Europe (van den Besselaar et al., Theor. Appl. Climatol, in press) EURANDOM & KNMI, May 2009 Analysis of extremes • Classic EVT provides a framework for analyzing extremes further in the tails of the statistical distributions EURANDOM & KNMI, May 2009 Analysis of extremes • Classic EVT provides a framework for analyzing extremes further in the tails of the statistical distributions • Possible to account for “non-stationarity”, but the best way to do this is still under debate EURANDOM & KNMI, May 2009 Analysis of extremes • Classic EVT provides a framework for analyzing extremes further in the tails of the statistical distributions • Possible to account for “non-stationarity”, but the best way to do this is still under debate • One option is making the parameters of the GEV models time-dependent EURANDOM & KNMI, May 2009 EURANDOM & KNMI, May 2009 Analysis of extremes • Among others, a user-friendly R-based toolkit (extRemes) is available from http://www.assessment.ucar.edu/toolkit (Stephenson and Gilleland, 2006; Gilleland and Katz, 2005) EURANDOM & KNMI, May 2009 Empirical 0.4 0.0 0.2 0.4 0.6 0.8 1.0 20 40 50 Model Return Level Plot Density Plot 60 0.00 30 f(z) 50 70 0.04 Empirical 10 Return Level 30 0.02 Model 0.0 10 20 30 40 50 60 Quantile Plot 0.8 Probability Plot 0.1 1 10 100 1000 Return Period EURANDOM & KNMI, May 2009 10 20 30 40 z 50 60 EURANDOM & KNMI, May 2009 EURANDOM & KNMI, May 2009 160 120 80 40 Empirical 0.2 0.4 0.6 0.8 1.0 40 60 80 100 140 Model Return Level Plot Density Plot f(z) 100 0.000 50 0.010 Empirical 150 200 0.0 Return Level Quantile Plot 0.0 0.2 0.4 0.6 0.8 1.0 Model Probability Plot 0.1 1 10 100 1000 Return Period EURANDOM & KNMI, May 2009 20 40 60 80 120 z 160 EURANDOM & KNMI, May 2009 EURANDOM & KNMI, May 2009 Kharin et al., J.Climate, 2007 EURANDOM & KNMI, May 2009 Take home message • For providing information services on changing climate extremes the combined use of different techniques is recommended, as this will also provide information on the uncertainties EURANDOM & KNMI, May 2009 Take home message • For providing information services on changing climate extremes the combined use of different techniques is recommended, as this will also provide information on the uncertainties • New infrastructural works should be designed on the basis of both historical information on changes in extremes and projected future changes EURANDOM & KNMI, May 2009 the end EURANDOM & KNMI, May 2009 http://eca.knmi.nl EURANDOM & KNMI, May 2009 http://eca.knmi.nl EURANDOM & KNMI, May 2009 http://eca.knmi.nl EURANDOM & KNMI, May 2009 Alexander et al.,2006; in IPCC-AR4 EURANDOM & KNMI, May 2009