2.5
Forecasting global temperatures one year ahead
Chris K. Folland, Hadley Centre, Met Office, Exeter, United Kingdom; and A. W. Colman
Global temperature is an important indicator of global climate change, and has been at near record levels in recent years. Predictions of global temperature for the year ahead are consequently of considerable interest to policy-makers. Analyses of observed and model data have linked interannual to multiannual fluctuations in global mean temperature to natural phenomena including the El Nino-Southern Oscillation (ENSO) and volcanic activity. On decadal and longer time scales, global temperature change in recent decades has also been firmly linked to human activity, including changing greenhouse gas and aerosol concentrations and stratospheric ozone depletion and tropospheric ozone increases.
The existence of these numerous forcings raises the possibility of skilful predictions of global temperature for one year ahead. Here indices of the known important climate forcings and influencing phenomena are used to make a mixed empirical and dynamical prediction of the global temperature anomaly from a 1961-90 average. Based on multiple regression, the state of ENSO is the most important predictor on interannual time scales; on greater than decadal time scales the net radiative forcing of the atmosphere is most important. We use a regression model incorporating the above factors. The ENSO predictor is a coupled model prediction of the SST anomaly in the Nino 3.4 region of the Tropical Pacific in the first half of the year ahead using the Met Office GLOSEA model.
Global temperature anomaly forecasts are issued both in best estimate form and as probability forecasts. Intrinsic skill is high (based on cross validation) and equivalent to a correlation of 0.82 for interannual variability and 0.95 when all time scales of variability are considered over 1960-2003. This gives a 2 sigma hindcast annual temperature anomaly uncertainty of +_0.12oC which can be compared to the observed 2 sigma temperature anomaly uncertainty of +-0.06oC. Forecasts are now issued routinely in the previous December as part of an annual press release on global climate made by the UK Met Office. The skill of real-time forecasts issued since 2000 are consistent with cross validation tests, though some details of the forecast procedure have evolved.
Recorded presentationSession 2, Climate Predictions on Seasonal and Interannual Time Scales: 1(parallel with Session 1)
Monday, 10 January 2005, 1:30 PM-5:30 PM
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