Climate Modeling using Gaussian Processes
We want to produce high-fidelity temperature predictions for a mountainous, costal region of Peru.
Region of Interest (ROI) for high-fidelity temperature predictions
We have access to a Regional Climate Model (RCM) which can compute these predictions, but it is prohibitively expensive to run for the whole region of interest. We also have access to high-fidelity altitude data and a Global Climate Model (GCM) which can compute inexpensive, low-fidelity temperature and wind speed predictions.
Low-fidelity temperature and wind speed (GCM)
High-fidelity altitude
High-fidelity temperature (RCM, target)
We use the RCM to produce high-fidelity temperature predictions over small regions within the region of interest. These are much less expensive to produce. Then, we use Gaussian Processes combine these predictions with the low-fidelity temperature predictions from the GCM and the high-fidelity altitude data to infer the high-fidelity temperature predictions over the entire region of interest.
For example:
Low-fidelity temperature training data
High-fidelity temperature training data
Inferred high-fidelity temperature predictions
True high-fidelity temperature predictions
This work done during my master’s degree at University of Cambridge.