Regional climate‐model predictions of extreme rainfall for a changing climate

Major floods occurred in the United Kingdom during autumn 2000. These were caused by a rapid sequence of heavy rainfall events that occurred over a period of many weeks leading to record-breaking monthly-to-seasonal rainfall totals. The question was raised as to whether such rainfall events may be related to human-induced climate change. Climate-model predictions of future changes in mean precipitation behaviour are well established. However, to understand flooding requires an examination of predictions of extreme rainfall behaviour at a relatively small spatial scale. For three areas within the United Kingdom, output from a Hadley Centre regional climate model, 'nested' within one of its general-circulation models, is compared with raingauge data averaged over these areas for the period 1961-1990. This shows that the modelling system is good at predicting the statistical likelihood of extreme rainfall events seen in historical data. This result holds for extreme rainfall totals over daily to monthly timescales. When the modelling system is used to predict changes in these extreme events resulting from atmospheric CO2 concentrations that may be representative of the period 2080-2100, significant reductions in the return periods of such events are seen. For example, 30-day rainfall totals, which happened in the recent past on average once in 20 years, are predicted to happen once in 3-5 years. An interpolation method based upon climate-model output and incorporating raingauge data is used to estimate how rainfall extremes may have changed between the middle of the 19th century, and for a period centred on the year 2000. This also predicts that increased greenhouse gases have led to reduced return periods of extreme rainfall events for three sites of interest, though in this case the changes are not statistically significant.

[1]  John F. B. Mitchell,et al.  The second Hadley Centre coupled ocean-atmosphere GCM: model description, spinup and validation , 1997 .

[2]  T. N. Palmer,et al.  Quantifying the risk of extreme seasonal precipitation events in a changing climate , 2002, Nature.

[3]  Peter M. Cox,et al.  An analogue model to derive additional climate change scenarios from existing GCM simulations , 2000 .

[4]  M. Collins,et al.  Projections of future climate change , 2002 .

[5]  A. Haines Climate change 2001: the scientific basis. Contribution of Working Group 1 to the Third Assessment report of the Intergovernmental Panel on Climate Change [Book review] , 2003 .

[6]  S. B. Jones The estimation of catchment average point rainfall profiles , 1983 .

[7]  T. V. Ommen,et al.  Observed climate variability and change , 2002 .

[8]  Michael E. Schlesinger,et al.  Developing climate scenarios from equilibrium GCM results , 1990 .

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

[10]  C. Prudhomme,et al.  Downscaling of global climate models for flood frequency analysis: where are we now? , 2002 .

[11]  D. C. Hill,et al.  Estimation of natural and anthropogenic contributions to twentieth century temperature change , 2002 .

[12]  Alexei G. Sankovski,et al.  Special report on emissions scenarios , 2000 .

[13]  J. Murphy,et al.  Simulation of climate change over europe using a nested regional‐climate model. II: Comparison of driving and regional model responses to a doubling of carbon dioxide , 1997 .

[14]  T. Marsh Climate change and hydrological stability: A look at long‐term trends in south‐eastern Britain , 2001 .

[15]  Richard G. Jones,et al.  Simulation of climate change over europe using a nested regional‐climate model. I: Assessment of control climate, including sensitivity to location of lateral boundaries , 1995 .

[16]  Raquel V. Francisco,et al.  Emerging patterns of simulated regional climatic changes for the 21st century due to anthropogenic forcings , 2001 .

[17]  J. Gregory,et al.  A comparison of extreme European daily precipitation simulated by a global and a regional climate model for present and future climates , 2001 .

[18]  S. Levitus Climatological Atlas of the World Ocean , 1982 .

[19]  James M. Murphy,et al.  An Evaluation of Statistical and Dynamical Techniques for Downscaling Local Climate , 1999 .

[20]  P. Jones,et al.  Assessing future changes in extreme precipitation over Britain using regional climate model integrations , 2001 .

[21]  Raquel V. Francisco,et al.  Regional Climate Information—Evaluation and Projections , 2001 .