| Issue |
ESAIM: ProcS
Volume 70, 2021
CEMRACS 2019 - Geophysical Fluids, Gravity Flows
|
|
|---|---|---|
| Page(s) | 137 - 146 | |
| DOI | https://doi.org/10.1051/proc/202107009 | |
| Published online | 01 June 2021 | |
Partial differential equations for oceanic artificial intelligence
1 LMBA/UMR 6205, University of South Brittany
2 MIO, University of Marseille
3 Numerical Analysis and Scientific Computing, Department of Mathematics, Technical University of Darmstadt
4 LMBA/UMR 6205, University of South Brittany and See-d, Vannes
5 LMBA/UMR 6205, University of South Brittany
6 LOCEAN, IPSL
The Sea Surface Temperature (SST) plays a significant role in analyzing and assessing the dynamics of weather and also biological systems. It has various applications such as weather forecasting or planning of coastal activities. On the one hand, standard physical methods for forecasting SST use coupled ocean- atmosphere prediction systems, based on the Navier-Stokes equations. These models rely on multiple physical hypotheses and do not optimally exploit the information available in the data.
On the other hand, despite the availability of large amounts of data, direct applications of machine learning methods do not always lead to competitive state of the art results. Another approach is to combine these two methods: this is data-model coupling. The aim of this paper is to use a model in another domain. This model is based on a data-model coupling approach to simulate and predict SST. We first introduce the original model. Then, the modified model is described, to finish with some numerical results.
Key words: Data Assimilation / Data-Model Coupling / Artificial Intelligence / SST / PDE
© EDP Sciences, SMAI 2021
This is an Open Access article distributed under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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