Authors: Doug M Smith Adam A Scaife George J Boer Mihaela Caian Francisco J DoblasReyes Virginie Guemas Ed Hawkins Wilco Hazeleger Leon Hermanson Chun Kit Ho Masayoshi Ishii Viatcheslav Kharin Masahide Kimoto Ben Kirtman Judith Lean Daniela Matei William J Merryfield Wolfgang A Müller Holger Pohlmann Anthony Rosati Bert Wouters Klaus Wyser
Publish Date: 2012/12/05
Volume: 41, Issue: 11-12, Pages: 2875-2888
Abstract
We present the first climate prediction of the coming decade made with multiple models initialized with prior observations This prediction accrues from an international activity to exchange decadal predictions in near realtime in order to assess differences and similarities provide a consensus view to prevent overconfidence in forecasts from any single model and establish current collective capability We stress that the forecast is experimental since the skill of the multimodel system is as yet unknown Nevertheless the forecast systems used here are based on models that have undergone rigorous evaluation and individually have been evaluated for forecast skill Moreover it is important to publish forecasts to enable open evaluation and to provide a focus on climate change in the coming decade Initialized forecasts of the year 2011 agree well with observations with a pattern correlation of 062 compared to 031 for uninitialized projections In particular the forecast correctly predicted La Niña in the Pacific and warm conditions in the north Atlantic and USA A similar pattern is predicted for 2012 but with a weaker La Niña Indices of Atlantic multidecadal variability and Pacific decadal variability show no signal beyond climatology after 2015 while temperature in the Niño3 region is predicted to warm slightly by about 05 °C over the coming decade However uncertainties are large for individual years and initialization has little impact beyond the first 4 years in most regions Relative to uninitialized forecasts initialized forecasts are significantly warmer in the north Atlantic subpolar gyre and cooler in the north Pacific throughout the decade They are also significantly cooler in the global average and over most land and ocean regions out to several years ahead However in the absence of volcanic eruptions global temperature is predicted to continue to rise with each year from 2013 onwards having a 50 chance of exceeding the current observed record Verification of these forecasts will provide an important opportunity to test the performance of models and our understanding and knowledge of the drivers of climate changeThis work was supported by the joint DECC/Defra Met Office Hadley Centre Climate Programme GA01101 and the EU FP7 THOR and COMBINE projects MPI work was supported by the BMBF Nordatlantik and MiKlip projects Ben Kirtman was supported by NOAA grants NA10OAR4320143 and NA10OAR4310203 IC3 work was supported by the EUfunded QWeCI FP7ENV20091243964 and CLIMRUN projects FP7ENV2010265192 the MICINNfunded RUCSS CGL201020657 projects and the Catalan Government The IC3 authors thankfully acknowledge the computer resources technical expertise and assistance provided by the Red Española de Supercomputación RES the European Centre for MediumRange Weather Forecasts ECMWF under the special project SPESICCF and Muhammad Asif for his invaluable support in running the experiments NASA supported J Lean MIROC work was supported by the KAKUSHIN program of the Ministry of Education Culture Sports Science and Technology Japan The Earth Simulator of JAMSTEC was employed to perform MIROC experiments MRI work was supported by the Japan Meteorological Agency research program and partly by the KAKUSHIN Program
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