SOES 3015 Modelling Practical The GENIE Climate Simulator









- Slides: 9
SOES 3015 Modelling Practical The GENIE Climate Simulator: Introduction, Getting Started & CO 2 Expts Bob Marsh National Oceanography Centre University of Southampton
Ø The GENIE model has been recently adapted for teaching by colleagues at the Open University Ø With appropriate setup (see practical notes) The application runs under Windows Ø Read this introductory talk before commencing on the practicals Ø Work may be carried out individually or in pairs, running GENIE in a small range of CO 2 experiments Ø The practical is designed to give you some direct experience of: • • • what an EMIC looks like how fast it runs the kind of data that is produced
Increasing Realism: Earth System Models of Intermediate Complexity (EMICs) Ø Millennial transient simulations presently restricted to somewhat simplified Earth System Models of Intermediate Complexity (EMICs): Many components/processes - e. g. , “GENIE” Low resolution / reduced dimensionality - framework for Earth system modelling e. g. , CLIMBER-2 (PIK, Germany) Schematic only, for accurate model refer to: Petoukhov, V. , Ganopolski, A. , Brovkin, V. , Claussen, M. , Eliseev, A. , Kubatzki C. , Rahmstorf, S. , (2000) CLIMBER-2: a climate system model of intermediate complexity. Part I: model description and performance for present climate. Climate Dynamics, v. 16, no. 1, p. 1 -17. Ø Around a dozen such models developed in last 10 -15 years Ø Sufficiently fast & complex to simulate past/future millennia Ø Combine simulations & statistics provide best way forwards?
Five Stages (approximate times - depends on machine speed): Ø Getting Started (2. 30 -2. 40) Ø Ø Initial State (2. 40 -2. 50) Idealized CO 2 forcing (2. 50 -3. 00) Anthropogenic CO 2 forcing (3. 00 -3. 30) Climate Sensitivity Experiments (3. 30 -5. 00) • Proceed stage by stage • Be patient! • While waiting for longer expts to complete, look at data you have already produced • Organize yourselves to tackle stage 5 • Health Warning: First time this practical has been tried (second time GENIE used in Uo. S teaching - previously went OK!)
Climate Sensitivities Ø Quantified & assessed with combination of Simple Climate Models (SCMs), EMICs and GCMs Ø Equilibrium Climate Sensitivity vs. Transient Climate Response (TCR) Ø Equilibrium Climate Sensitivity = change in global-mean temperature for doubling of CO 2 (from pre-industrial level) Ø Transient Climate Response = change in global-mean temperature at doubling of CO 2, increasing at 1% p. a. (from pre-industrial level) Strong link between TCR and Climate sensitivity: Dots = AOGCMs Grey lines = EMIC results Courtesy of IPCC: AR 4: Climate Change 2007: Working Group I: The Physical Science Basis
Climate Sensitivity: Uncertainty & Probability Ø Probability Density Functions (PDFs) of Climate Sensitivity: Ø Most uncertainty attributed to differences in cloud physics? Courtesy of IPCC: AR 4
Relevance of/for Palaeoclimate Change? Proxies tell us: • how warm it got locally • and globally? • and even how much CO 2 was in the atmosphere (fossil stomata, carbon isotopes) So, in principle, proxies for global-mean temperature & CO 2 can tell us something about equilibrium climate sensitivity Indeed, there is evidence for: • Glacial-Interglacial CO 2 & associated cooling/warming (but global temperature response is compicated by ice sheets) • Elevated CO 2 in the Pliocene & associated warmth • Pulse of CO 2 (or CH 4) at the PETM & associated hyper-warmth
Why we need Models? Earth system models, incorporating synthetic proxies, provide a means of interpreting measured proxies, and testing the extent to which different processes (e. g. , climate sensitivity) can be inferred from multi-proxy datasets
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