Articles | Volume 18, issue 4
https://doi.org/10.5194/os-18-1221-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-18-1221-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Four-dimensional temperature, salinity and mixed-layer depth in the Gulf Stream, reconstructed from remote-sensing and in situ observations with neural networks
Etienne Pauthenet
CORRESPONDING AUTHOR
Ifremer, Univ. Brest, CNRS, IRD, Laboratoire d'Océanographie Physique et Spatiale (LOPS), IUEM, 29280, Plouzané, France
Loïc Bachelot
Ifremer, Univ. Brest, CNRS, IRD, Service Ingénierie des Systèmes d'Information (PDG-IRSI-ISI), IUEM, 29280, Plouzané, France
Kevin Balem
Ifremer, Univ. Brest, CNRS, IRD, Laboratoire d'Océanographie Physique et Spatiale (LOPS), IUEM, 29280, Plouzané, France
Guillaume Maze
Ifremer, Univ. Brest, CNRS, IRD, Laboratoire d'Océanographie Physique et Spatiale (LOPS), IUEM, 29280, Plouzané, France
Anne-Marie Tréguier
Ifremer, Univ. Brest, CNRS, IRD, Laboratoire d'Océanographie Physique et Spatiale (LOPS), IUEM, 29280, Plouzané, France
Fabien Roquet
Department of Marine Sciences, University of Gothenburg, Gothenburg, Sweden
Ronan Fablet
IMT Atlantique, CNRS UMR Lab-STICC, Brest, France
Pierre Tandeo
IMT Atlantique, CNRS UMR Lab-STICC, Brest, France
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Short summary
Temperature and salinity profiles are essential for studying the ocean’s stratification, but there are not enough of these data. Satellites are able to measure daily maps of the surface ocean. We train a machine to learn the link between the satellite data and the profiles in the Gulf Stream region. We can then use this link to predict profiles at the high resolution of the satellite maps. Our prediction is fast to compute and allows us to get profiles at any locations only from surface data.
Temperature and salinity profiles are essential for studying the ocean’s stratification, but...