Probabilistic Emulation of a Global Climate Model with Spherical DYffusion
📄 Read the paper:
Motivation
→ Limited exploration of mitigation and adaptation strategies.
→ Large ensembles for reducing uncertainties are prohibitive to run.
Solution: Train a cheap-to-run ML model to emulate (parts of) a climate model!
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Source: Milinski et al., “How large does a large ensemble need to be?”
Motivation
→ Limited exploration of mitigation and adaptation strategies.
→ Large ensembles for reducing uncertainties are prohibitive to run.
Solution: Train a cheap-to-run ML model to emulate (parts of) a climate model!
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Source: Milinski et al., “How large does a large ensemble need to be?”
Weather forecasting vs. Climate Modeling
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Our Approach: Spherical DYffusion
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[1] Watt-Meyer et al., “ACE: A fast, skillful learned global atmospheric model for climate prediction” (NeurIPS CCAI 2023)
[2] Bonev et al., “Spherical fourier neural operators: Learning stable dynamics on the sphere” (ICML 2023)
[3] Ruhling Cachay et al., “DYffusion: A Dynamics-informed Diffusion Model for Spatiotemporal Forecasting” (NeurIPS 2023)
Forecasting with DYffusion at inference time
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Forecasting with DYffusion at inference time
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DYffusion’s Key Idea: Couple diffusion steps with physical time steps
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Standard
Ours
Inference & Training
(including forcings)
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SFNO network topology
(single block)
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SFNO network topology
(single block)
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The new part for diffusion modeling
Inference including forcings
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Results: Visualization of two ensemble members
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Results: 10-yr time-mean RMSEs
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Results: 10-yr time-mean RMSEs
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Results: 10-yr time-mean RMSEs (showing more fields)
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Results: Global bias maps of total water path time-mean
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Results: 100-year rollouts
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Computational comparison
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Results: Encouraging
climate variability
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Results: Encouraging ensemble weather forecasts
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Conclusion
→ Using SFNO architecture absolutely key for successful climate emulation!
Outlook/Future work:
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Thanks for listening!
Feel free to reach out :)
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@salvaRC7
sruhlingcachay@ucsd.edu
📄 Read the paper:
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More slides
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Computational comparison
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Key Idea: Couple diffusion steps with physical time steps
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Standard
Ours
Forecasting with DYffusion at inference time
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Forecasting with DYffusion at inference time
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Results: Encouraging
climate variability
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Results: Encouraging ensemble weather forecasts
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Results: SFNO-DYffusion leads to more effective ensembles
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Methods: Training
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Methods: Sampling
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Motivation
Existing ML models for high-dimensional spatiotemporal forecasting tend to be:
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ClimaX: A foundation model for weather and climate, Nguyen et al., ICML 23, https://arxiv.org/abs/2301.10343
Motivation
Existing ML models for high-dimensional spatiotemporal forecasting tend to be:
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Spherical Fourier Neural Operators: Learning stable dynamics on the sphere, Bonev et al., ICML 23, https://arxiv.org/abs/2306.03838
Results: Competitive probabilistic rollouts
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Results: Temporal super-resolution (8x)
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Summary
+ more details, results and extensive ablations in our paper!
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Thanks for listening!
Feel free to reach out :)
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@salvaRC7
sruhlingcachay@ucsd.edu
Paper: arxiv.org/abs/2306.01984