EGU26-15749, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-15749
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Wednesday, 06 May, 14:00–15:45 (CEST), Display time Wednesday, 06 May, 14:00–18:00
 
Hall X5, X5.202
Physics-informed neural network for gridded SSH from SWOT observations considering the next-order balanced model
Junyang Gou1,2, Ryan Shìjié Dù3, K. Shafer Smith4, Benedikt Soja1, and Abigail Bodner2,5
Junyang Gou et al.
  • 1Institute of Geodesy and Photogrammetry, ETH Zurich, Zurich, Switzerland (jungou@ethz.ch)
  • 2Department of Earth, Atmospheric and Planetary Sciences, Massachusets Institute of Technology, Cambridge, MA, USA
  • 3Department of Geophysics, Colorado School of Mines, Golden, CO, USA
  • 4Courant Institute of Mathematical Sciences, New York University, New York, NY, USA
  • 5Department of Electrical Engineering and Computer Science, Massachusets Institute of Technology, Cambridge, MA, USA

The Surface Water and Ocean Topography (SWOT) satellite mission, launched in December 2022, provides revolutionary measurements of the sea surface height (SSH) variations with unprecedented spatial resolution down to Ο(1 km). As a result, SWOT products have significant potential in monitoring ocean dynamics down to the submesoscale. However, the repeat cycle of 21 days introduces a barrier to fully capture these dynamics as they vary on the order of days. To fully exploit the potential of the satellite mission and simplify processing requirements for potential users, we propose a physics-informed neural network (PINN) to generate gridded SSH products from SWOT L3 along-track snapshots. The neural network has a U-Net-like architecture combined with residual learning to consider the spatial variations of the SSH field, and takes time, geolocations, and gridded SSH from conventional altimetry missions as input features, while the SWOT observations serve as ground truth. In addition to the classical data loss, the PINN model applies direct constraints on the model's trainable parameters by forcing them to fulfill the next-order correction of the quasi-geostrophic theory (SQG+1), which has been demonstrated to be able to capture cyclogeostrophic balance and frontogenesis attributed to submesoscale dynamics. To this end, the high resolution of SWOT observations is kept, while the velocities and pressure fields associated with the SQG+1 theory are predicted. We conducted experiments using both simulated data and real-world data. Both experiments demonstrate the benefits of incorporating physical loss to achieve higher generalizability, thereby filling the gaps between SWOT tracks reasonably. Based on the real-world data, 2-km gridded SSH products with a temporal resolution of five days are achieved. The proposed method shows promising potential for generating high-resolution gridded products while considering physical constraints. The product will be beneficial for the community to analyze mesoscale to submesoscale ocean dynamics, and compare with other sources of surface and in-situ data in the upper ocean.

How to cite: Gou, J., Dù, R. S., Smith, K. S., Soja, B., and Bodner, A.: Physics-informed neural network for gridded SSH from SWOT observations considering the next-order balanced model, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-15749, https://doi.org/10.5194/egusphere-egu26-15749, 2026.