| Diagnostic Analysis of GCM Simulations Driven by SRES A2 and B2 Emissions Scenarios Xianfu Lu Tyndall Centre for Climate Change Research School of Environmental Sciences, University of East Anglia Introduction As an attempt to assist the AIACC study partners in selecting the most "appropriate" GCM experiments to develop climate scenarios for their projects, we performed a preliminary diagnostic analysis of climate simulations from 9 different GCMs driven by SRES A2 and B2 emissions scenarios, for 13 regions covered by 11 AIACC projects. Methodology and Data By comparing model simulated baseline period climatology against observations, one could make a judgment on which simulations perform better over the others for a specific region/area, in term of reproducing observed average climate features. Meanwhile, by examining the range of changes in primary climate features simulated by various GCMs, one could then decide, depending on how much of the uncertainty span should be explored in the I, V &A assessment, which model simulation(s) to use to derive regional climate scenarios. CRU05 0.5 degree seasonal mean climatology was used and compared against GCM simulations. This data set is described in New, M., M. Hulme and P. Jones, 1999. Simulations of "present-day" (1961~90) climatology and climate futures towards the end of this century (2071~2100) from 9 state-of-the-art GCMs driven by SRES emissions scenarios were analysed. These model simulations were reviewed by the IPCC Third Assessment Report (TAR). Two variables (mean temperature and precipitation), two seasons [JJA(June-July-August) and DJF (December-January-February)], and two SRES emissions scenarios (A2 and B2) are included in this analysis. Results
Follow the links below to download the results corresponding to your region/area. (The following are zipped files that contain several images)
Additional Papers and Resources
1 The aggregation of anomalies over each region was achieved by simply averaging the numbers for GCM grid boxes falling inside each region. Scatter plots are missing for a few regions. This is due to the fact that some models produce 0 mm of seasonal precipitation over the baseline period. Therefore, the percentage change of precipitation in the 2080s was not attainable. |