1. World Climate Research Programme Climate Information for Decision Making Ghassem R. Asrar Director, WCRP

2. Outline Science Based Decision Making –World Climate Conference-3: Climate info. for better future –OceanObs09: Ocean observations for society –ICSU visioning: Environment & sustainable development WCRP Contribution –Seasonal Predictions –Decadal Predictions –Regional climate predictions –Sea Level variability and change

3. Seasonal Climate Prediction WCRP, through its Working Group on Seasonal to Interannual Prediction (WGSIP), –Launched the Climate-system Historical Forecast Project (CHFP) a multi-model and multi-institutional experimental framework for sub-seasonal to decadal complete physical climate system prediction http://www.clivar.org/organization/wgsip/chfp/chfp.php CHFP will provide: - A baseline assessment of seasonal prediction capabilities using the best available models of the climate system and data for initialization

4. Seasonal Climate Prediction Challenges Quantifying Forecast Uncertainty Due to Uncertainty in Model Formulation –Multi-Model Helps, but Ad-Hoc Quantifying Forecast Uncertainty Due to Uncertainty in Observational Estimates –Initial Condition Problem Model Error –Need for International Coordinated Effort at Improving Models (Multi-Model is Not an Excuse for Neglecting Model Improvement) Climate System Component Interactions –Coupled Ocean-Land-Ice-Atmosphere –External Forcing vs. Natural Variability Quantifying the Limit of Predictability

5. Seasonal Prediction-South Africa 10% Rainfall forecast issued in Dec. 2008 by a multi-model operational Seasonal Forecast by the South African Weather Service.

6. Decadal Climate Experiments additional predictions Initialized in ‘01, ’02, ’03 … ‘09 100-yr “control” & 1% CO 2 prediction with 2010 Pinatubo- like eruption alternative initialization strategies atmos. chemistry &/or aerosols &/or regional air quality prescribed SST time- slices extend ensembles from O(3) to O(10) members hindcasts without volcanoes 30-year hindcast and prediction ensembles: initialized 1960, 1980 & 2005 10-year hindcast & prediction ensembles: initialized 1960, 1965, …, 2005 WCRP, through its Working Group on Coupled Modelling (WGCM) - has developed the coupled- model intercomparison project (CMIP5) that coordinates the decadal predictability/prediction experiments - will provide the foundation for the simulations to be assessed as part of the IPCC AR5

7. Decadal Climate Predictability Observed decadal climate variability in Pacific and Atlantic sectors (left) and first attempts to make decadal predictions (right)

8. Regional Climate The need for climate information at the regional-to-local scale is one of the central issues within the global change debate. In 2008 WCRP established a Task Force on Regional Climate Downscaling (TF-RCD), whose mandate is: –to summarize the shortcomings, difficulties and scientific basis of existing downscaling methods to serve as guidance to the climate change assessment community; –to develop a framework for evaluation and intercomparison of regional downscaling techniques.

9. Regional Climate Uncertainty in regional climate projectionEmis./Conc.(MultipleScenarios) AOGCM Configuration (Multiple AOGCMs) Internal variability (Multiple realizations) RCD Configuration (Multiple models) RCD approach (Multiple RCD methods) Regional cover (Multiple regions) Schematic depiction of the primary uncertainties in regional climate change projections. Systematic Errors (Model eval./impr.)

10. Regional Climate: Africa - Example January-February- March mean precipitation for 1998-2008 period.

11. Regional Climate: Africa - Example July-August-Septmeber mean precipitation for 1998-2008 period.

12. Sea-Level Variability and Change The main challenge is to address the uncertainties in the projection of future sea-level changes due to recently discovered processes in the Greenland and Antarctic regions. The joint WCRP/IOC Task Group on Sea-Level Variability and Change (TF-RCD) was established with the mandate to: –Improve further our ability to monitor, explain and predict changes in global and regional sea level and associated environmental factors. –Make available this information for stakeholders and policy- makers

13. Climate variability affects the regional distribution of sea-level rise. CSIRO - Australia Sea-Level Variability and Change: Regional Impacts

14. 2.35 2.30 2.00 2.25 2.20 2.05 2.15 2.10 Sea Level (m) Return Period (Years) 0.1101100 +0.08m x3.1 Post-1950 Pre-1950 20 th Century – Fort Denison 20 th Century sea- level rise has already caused a significant increase in extreme events - three-fold increase post-1950. By 2100, 1 in 100 year events are projected to happen several times a year!

15. Conclusions WCRP will continue to: –Provide Scientific Knowledge on climate variability and change. –Facilitate research on climate projections and predictions on centuries, decades and seasons. –Place a major emphasis on regional climate variability and change with special attention to extreme events. –Support development and delivery of climate information for decision makers. –Sponsor training and development of next generation of regional and global climate experts.