Anatomy of an Extreme Event

AbstractThe record-setting 2011 Texas drought/heat wave is examined to identify physical processes, underlying causes, and predictability. October 2010–September 2011 was Texas’s driest 12-month period on record. While the summer 2011 heat wave magnitude (2.9°C above the 1981–2010 mean) was larger than the previous record, events of similar or larger magnitude appear in preindustrial control runs of climate models. The principal factor contributing to the heat wave magnitude was a severe rainfall deficit during antecedent and concurrent seasons related to anomalous sea surface temperatures (SSTs) that included a La Nina event. Virtually all the precipitation deficits appear to be due to natural variability. About 0.6°C warming relative to the 1981–2010 mean is estimated to be attributable to human-induced climate change, with warming observed mainly in the past decade. Quantitative attribution of the overall human-induced contribution since preindustrial times is complicated by the lack of a detected cent...

[1]  C. Deser,et al.  Communication of the role of natural variability in future North American climate , 2012 .

[2]  S. Seneviratne,et al.  Hot days induced by precipitation deficits at the global scale , 2012, Proceedings of the National Academy of Sciences.

[3]  Peter E. Thornton,et al.  Simulating the Biogeochemical and Biogeophysical Impacts of Transient Land Cover Change and Wood Harvest in the Community Climate System Model (CCSM4) from 1850 to 2100 , 2012 .

[4]  L. Luo,et al.  Did we see the 2011 summer heat wave coming? , 2012 .

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

[6]  Tao Zhang,et al.  On the Increased Frequency of Mediterranean Drought , 2012 .

[7]  Jane Lubchenco,et al.  Predicting and managing extreme weather events , 2012 .

[8]  T. Karl,et al.  Changes in Intense Precipitation over the Central United States , 2012 .

[9]  S. Rahmstorf,et al.  Increase of extreme events in a warming world , 2011, Proceedings of the National Academy of Sciences.

[10]  J. Seinfeld,et al.  Climatic effects of 1950-2050 changes in US anthropogenic aerosols - Part 2: Climate response , 2011 .

[11]  J. Nielsen‐Gammon,et al.  A New Homogenized Climate Division Precipitation Dataset for Analysis of Climate Variability and Climate Change , 2011 .

[12]  Prashant D. Sardeshmukh,et al.  Critical influence of the pattern of Tropical Ocean warming on remote climate trends , 2011 .

[13]  Tao Zhang,et al.  Was there a basis for anticipating the 2010 Russian heat wave? , 2011 .

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

[15]  M. Hoerling,et al.  Regional Precipitation Trends: Distinguishing Natural Variability from Anthropogenic Forcing , 2010 .

[16]  John F. B. Mitchell,et al.  The next generation of scenarios for climate change research and assessment , 2010, Nature.

[17]  K. Findell,et al.  Impact of Common Sea Surface Temperature Anomalies on Global Drought and Pluvial Frequency , 2010 .

[18]  G. Meehl,et al.  Relative increase of record high maximum temperatures compared to record low minimum temperatures in the U.S. , 2009 .

[19]  B. Cook,et al.  Contribution of soil moisture feedback to hydroclimatic variability , 2009 .

[20]  C. Deser,et al.  A U.S. CLIVAR Project to Assess and Compare the Responses of Global Climate Models to Drought-Related SST Forcing Patterns: Overview and Results , 2009 .

[21]  M. Hoerling,et al.  Distinct causes for two principal U.S. droughts of the 20th century , 2009 .

[22]  D. Dommenget The Ocean’s Role in Continental Climate Variability and Change , 2009 .

[23]  M. Hoerling,et al.  Attribution of the Seasonality and Regionality in Climate Trends over the United States during 1950–2000 , 2009 .

[24]  R. Seager,et al.  Forced and Internal Twentieth-Century SST Trends in the North Atlantic* , 2009 .

[25]  M. Hoerling,et al.  What is causing the variability in global mean land temperature? , 2008 .

[26]  P. Stott,et al.  Human contribution to rapidly increasing frequency of very warm Northern Hemisphere summers , 2008 .

[27]  G. Compo,et al.  Oceanic influences on recent continental warming , 2007 .

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

[29]  K. Kunkel,et al.  Can CGCMs Simulate the Twentieth-Century “Warming Hole” in the Central United States? , 2006 .

[30]  S. Saha,et al.  The NCEP Climate Forecast System , 2006 .

[31]  M. Hoerling,et al.  Warm oceans raise land temperatures , 2006 .

[32]  R. Stouffer,et al.  Assessment of Twentieth-Century Regional Surface Temperature Trends using the GFDL CM2 Coupled Models , 2006 .

[33]  R. Seager,et al.  Modeling of Tropical Forcing of Persistent Droughts and Pluvials over Western North America: 1856–2000* , 2005 .

[34]  P. Stott,et al.  Human contribution to the European heatwave of 2003 , 2004, Nature.

[35]  G. Danabasoglu,et al.  The Community Climate System Model Version 4 , 2011 .

[36]  R. Arritt,et al.  Altered hydrologic feedback in a warming climate introduces a “warming hole” , 2004 .

[37]  D. Lawrence,et al.  Regions of Strong Coupling Between Soil Moisture and Precipitation , 2004, Science.

[38]  Randal D. Koster,et al.  On the Cause of the 1930s Dust Bowl , 2004, Science.

[39]  S. Schubert,et al.  Causes of long-term drought in the U , 2004 .

[40]  Elizabeth C. Kent,et al.  Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century , 2003 .

[41]  E. Kalnay,et al.  The 1998 Oklahoma–Texas Drought: Mechanistic Experiments with NCEP Global and Regional Models , 2002 .

[42]  Song-You Hong,et al.  Role of sea surface temperature and soil-moisture feedback in the 1998 Oklahoma–Texas drought , 2000, Nature.

[43]  Robert G. Quayle,et al.  A Historical Perspective of U.S. Climate Divisions , 1996 .

[44]  Randall M. Dole,et al.  A diagnostic comparison of the 1980 and 1988 U.S. summer heat wave-droughts , 1995 .

[45]  Henry F. Diaz,et al.  Global climatic anomalies associated with extremes in the Southern Oscillation , 1989 .

[46]  C. M. Reed,et al.  The epidemiology of heat-related deaths, Texas--1950, 1970-79, and 1980. , 1983, American journal of public health.

[47]  J. Namias Anatomy of Great Plains Protracted Heat Waves (especially the 1980 U.S. summer drought) , 1982 .

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

[49]  Jill Williams,et al.  The Correlation between Temperature and Precipitation in the United States and Europe , 1978 .