The next AI for Climate seminar will be held on Friday the 5th of October (instead of 30th of September) 2022, at 14h30 ECT, at the Pierre et Marie Curie campus of Sorbonne Université, in seminar room 105 of LiP6, located on the first floor of the corridor 25/26 (easier access through tower 26).


The seminar can also be followed remotely through zoom (see here)

You can ask questions during and after the talk, in the slack channel.


Arthur Filoche’s talk is entitled:

« Variational data assimilation with deep prior »

Data Assimilation remains the operational choice when it comes to forecast and estimate Earth’s dynamical systems, and proposes a large panel of methods to optimally combine a dynamical model and observations allowing to predict, filter, or smooth system state trajectory.

The classical variational assimilation cost function is derived from modelling errors prior with uncorrelated in times Gaussian distribution. The optimization then relies on errors covariance matrices as hyperparameters.
But such statistics can be hard to estimate particularly for background and model errors. In this work, we propose to replace the Gaussian prior with a deep convolutional prior circumventing the use of background error covariances.

To do so, we reshape the optimization so that the initial condition to be estimated is generated by a deep architecture. The neural network is optimized on a single observational window, no learning is involved as in a classical variational inversion.
The bias induced by the chosen architecture regularizes the proposed solution with the convolution operators imposing locality.
 From a computational perspective, control parameters have simply been organized differently and are optimized using only the observational loss function corresponding to a maximum-likelihood estimation.

We propose several experiments highlighting the regularizing effect of deep convolutional prior. First, we show that such prior can replace background regularization in a strong-constraints 4DVar using a shallow water model. We extend the idea in a 3DVar set-up using spatio-temporal convolutional architecture to interpolate sea surface satellite tracks and obtain results on par with optimal interpolation with fine-tuned background matrix. Finally, we give perspective toward applying the same
method in weak-constrained 4DVar removing the need for model-errors covariances but still enforcing correlation in space and time of model errors.


Biographic notice:
Arthur Filoche is a Ph.D. student at the LiP6 of Sorbonne Université in France, under the supervision of Dominique Béréziat, Julien Brajard, and Anastase Charantonis. His research interests lie in combining deep learning and data assimilation