Trends in Extreme Weather and Climate Events: Issues Related to Modeling Extremes in Projections of Future Climate Change*

Projections of statistical aspects of weather and climate extremes can be derived from climate models representing possible future climate states. Some of the recent models have reproduced results previously reported in the Intergovernmental Panel on Climate Change (IPCC) Second Assessment Report, such as a greater frequency of extreme warm days and lower frequency of extreme cold days associated with a warmer mean climate, a decrease in diurnal temperature range associated with higher nighttime temperatures, increased precipitation intensity, midcontinent summer drying, decreasing daily variability of surface temperature in winter, and increasing variability of northern midlatitude summer surface temperatures. This reconfirmation of previous results gives an increased confidence in the credibility of the models, though agreement among models does not guarantee those changes will occur. New results since the IPCC Second Assessment Report indicate a possible increase of extreme heat stress events in a warm...

[1]  Zong-ci Zhao,et al.  Climate models—evaluation , 2001 .

[2]  W. Collins,et al.  Response of the NCAR Climate System Model to Increased CO2 and the Role of Physical Processes , 2000 .

[3]  M. Collins The El Niño–Southern Oscillation in the Second Hadley Centre Coupled Model and Its Response to Greenhouse Warming , 2000 .

[4]  Francis W. Zwiers,et al.  An Introduction to Trends in Extreme Weather and Climate Events: Observations, Socioeconomic Impacts, Terrestrial Ecological Impacts, and Model Projections* , 2000 .

[5]  S. Manabe,et al.  Detectability of Summer Dryness Caused by Greenhouse Warming , 1999 .

[6]  T. Delworth,et al.  Changes in Heat Index Associated with CO2-Induced Global Warming , 1999 .

[7]  Uwe Ulbrich,et al.  A shift of the NAO and increasing storm track activity over Europe due to anthropogenic greenhouse gas forcing , 1999 .

[8]  T. Knutson,et al.  Increased hurricane intensities with CO2-induced warming as simulated using the GFDL hurricane prediction system , 1999 .

[9]  John F. B. Mitchell,et al.  Causes of twentieth-century temperature change near the Earth's surface , 1999, Nature.

[10]  K. Lau,et al.  Interannual, Decadal–Interdecadal, and Global Warming Signals in Sea Surface Temperature during 1955–97 , 1999 .

[11]  A. Timmermann,et al.  Increased El Niño frequency in a climate model forced by future greenhouse warming , 1999, Nature.

[12]  D. Gaffen,et al.  Increased summertime heat stress in the US , 1998, Nature.

[13]  John F. B. Mitchell,et al.  Simulated changes in Southeast Asian monsoon precipitation resulting from anthropogenic emissions , 1998 .

[14]  R. Blender,et al.  North Atlantic cyclones in CO2-induced warm climate simulations: frequency, intensity, and tracks , 1998 .

[15]  F. Zwiers,et al.  Changes in the Extremes of the Climate Simulated by CCC GCM2 under CO2 Doubling , 1998 .

[16]  S. Manabe,et al.  Model assessment of decadal variability and trends in the tropical Pacific Ocean , 1998 .

[17]  G. Meehl,et al.  The Asian-Australian Monsoon and El Niño-Southern Oscillation in the NCAR Climate System Model*. , 1998 .

[18]  C. Senior,et al.  Changes in mid-latitude variability due to increasing greenhouse gases and sulphate aerosols , 1998 .

[19]  F. Chauvin,et al.  A Gcm Study of the Impact of Greenhouse Gas Increase on the Frequency of Occurrence of Tropical Cyclones , 1998 .

[20]  M. Latif,et al.  The impact of current and possibly future sea surface temperature anomalies on the frequency of Atlantic hurricanes , 1998 .

[21]  T. Knutson,et al.  Simulated increase of hurricane intensities in a CO2-warmed climate , 1998, Science.

[22]  Thomas R. Karl,et al.  Secular Trends of Precipitation Amount, Frequency, and Intensity in the United States , 1998 .

[23]  W. M. Gray,et al.  Tropical Cyclones and Global Climate Change: A Post-IPCC Assessment , 1998 .

[24]  A. Kitoh,et al.  Simulated Changes in the Asian Summer Monsoon at Times of Increased Atmospheric CO2 , 1997 .

[25]  J. D. Mahlman,et al.  Uncertainties in Projections of Human-Caused Climate Warming , 1997, Science.

[26]  John F. B. Mitchell,et al.  Changes in daily precipitation under enhanced greenhouse conditions , 1997 .

[27]  John F. B. Mitchell,et al.  Global and regional variability in a coupled AOGCM , 1997 .

[28]  U. Ulbrich,et al.  Midwinter Suppression of Northern Hemisphere Storm Track Activity in the Real Atmosphere and in GCM Experiments , 1997 .

[29]  S. Manabe,et al.  Transient response of a coupled model to estimated changes in greenhouse gas and sulfate concentrations , 1997 .

[30]  G. Komen,et al.  An analysis of extra-tropical storms in the North Atlantic region as simulated in a control and 2 × CO 2 time-slice experiment with a high-resolution atmospheric model , 1997 .

[31]  J. Wallace,et al.  ENSO-like Interdecadal Variability: 1900–93 , 1997 .

[32]  J. Gregory,et al.  Summer Drought in Northern Midlatitudes in a Time-Dependent CO2 Climate Experiment , 1997 .

[33]  Z. Kothavala Extreme precipitation events and the applicability of global climate models to the study of floods and droughts , 1997 .

[34]  S. Manabe,et al.  Simulated ENSO in a Global Coupled Ocean–Atmosphere Model: Multidecadal Amplitude Modulation and CO2 Sensitivity , 1997 .

[35]  G. Meehl Vulnerability of freshwater resources to climate change in the tropical pacific region , 1996, Water, Air, and Soil Pollution.

[36]  J. Katzfey,et al.  GCM Simulations of Eastern Australian Cutoff Lows , 1996 .

[37]  Warren M. Washington,et al.  El Niño-like climate change in a model with increased atmospheric CO2 concentrations , 1996, Nature.

[38]  R. Sausen,et al.  Cyclonic activity in a warmer climate , 1996 .

[39]  J. Houghton,et al.  Climate change 1995: the science of climate change. , 1996 .

[40]  L. Bengtsson,et al.  Will greenhouse gas-induced warming over the next 50 years lead to higher frequency and greater intensity of hurricanes ? , 1996 .

[41]  S. Manabe,et al.  Time-Mean Response over the Tropical Pacific to Increased C02 in a Coupled Ocean-Atmosphere Model , 1995 .

[42]  J. Gregory,et al.  Simulation of daily variability of surface temperature and precipitation over europe in the current and 2 × Co2 climates using the UKMO climate model , 1995 .

[43]  G. Meehl,et al.  South Asian Summer Monsoon Variability in a Model with Doubled Atmospheric Carbon Dioxide Concentration , 1993, Science.

[44]  G. Meehl,et al.  Tropical Pacific Interannual Variability and CO2 Climate Change , 1993 .

[45]  J. Houghton,et al.  Climate change : the IPCC scientific assessment , 1990 .

[46]  K. Emanuel The dependence of hurricane intensity on climate , 1987, Nature.

[47]  W. M. Gray,et al.  Tropical cyclone genesis , 1975 .