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  4. Data assimilation and parameter identification for water waves using the nonlinear Schrödinger equation and physics-informed neural networks
 
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Data assimilation and parameter identification for water waves using the nonlinear Schrödinger equation and physics-informed neural networks

Citation Link: https://doi.org/10.15480/882.13594
Publikationstyp
Journal Article
Date Issued
2024-10-01
Sprache
English
Author(s)
Ehlers, Svenja  
Strukturdynamik M-14  
Wagner, Niklas A.  
Scherzl, Annamaria
Klein, Marco  orcid-logo
Strukturdynamik M-14  
Hoffmann, Norbert  orcid-logo
Strukturdynamik M-14  
Stender, Merten  orcid-logo
Strukturdynamik M-14  
TORE-DOI
10.15480/882.13594
TORE-URI
https://hdl.handle.net/11420/49882
Journal
Fluids  
Volume
9
Issue
10
Article Number
231
Citation
Fluids 9 (10): 231 (2024)
Publisher DOI
10.3390/fluids9100231
Scopus ID
2-s2.0-85207721450
Publisher
Multidisciplinary Digital Publishing Institute
The measurement of deep water gravity wave elevations using in situ devices, such as wave gauges, typically yields spatially sparse data due to the deployment of a limited number of costly devices. This sparsity complicates the reconstruction of the spatio-temporal extent of surface elevation and presents an ill-posed data assimilation problem, which is challenging to solve with conventional numerical techniques. To address this issue, we propose the application of a physics-informed neural network (PINN) to reconstruct physically consistent wave fields between two elevation time series measured at distinct locations within a numerical wave tank. Our method ensures this physical consistency by integrating residuals of the hydrodynamic nonlinear Schrödinger equation (NLSE) into the PINN’s loss function. We first showcase a data assimilation task by employing constant NLSE coefficients predetermined from spectral wave properties. However, due to the relatively short duration of these measurements and their possible deviation from the narrow-band assumptions inherent in the NLSE, using constant coefficients occasionally leads to poor reconstructions. To enhance this reconstruction quality, we introduce the base variables of frequency and wavenumber, from which the NLSE coefficients are determined, as additional neural network parameters that are fine tuned during PINN training. Overall, the results demonstrate the potential for real-world applications of the PINN method and represent a step toward improving the initialization of deterministic wave prediction methods.
Subjects
data assimilation
hydrodynamic nonlinear Schrödinger equation
inverse problem
parameter identification
physics-informed neural network
wave surface reconstruction
MLE@TUHH
DDC Class
550: Earth Sciences, Geology
510: Mathematics
620: Engineering
Lizenz
https://creativecommons.org/licenses/by/4.0/
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