Enhancing the spatial resolution of GRACE ocean bottom pressure using deep learning algorithms

The gravimetry measurements from the Gravity Recovery and Climate Experiment (GRACE) satellite mission provide an essential way to monitor changes in ocean bottom pressure (OBP), which is a key variable in understanding ocean circulation. However, the coarse spatial resolution of GRACE OBP hinders r...

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Main Authors: Gou, J., Börger, L., Schindelegger, M., Soja, B.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018723
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5018723 2023-07-02T03:33:07+02:00 Enhancing the spatial resolution of GRACE ocean bottom pressure using deep learning algorithms Gou, J. Börger, L. Schindelegger, M. Soja, B. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018723 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-2108 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018723 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-2108 2023-06-11T23:39:57Z The gravimetry measurements from the Gravity Recovery and Climate Experiment (GRACE) satellite mission provide an essential way to monitor changes in ocean bottom pressure (OBP), which is a key variable in understanding ocean circulation. However, the coarse spatial resolution of GRACE OBP hinders resolving mass transports with refined details, particularly on the continental slope. By contrast, classical ocean forward models or reanalyses provide small-scale OBP information, but typically suffer from other problems (e.g., uncertainties in forcing fields, bathymetry, or structural errors in the dynamical formulation). In this study, we downscale the GRACE measured OBP to the eddy-permitting resolution of 0.25º using a self-supervised deep learning model by considering inputs from external high-resolution ocean models. The proposed deep learning model combines the principles of convolutional neural networks, residual learning, and an encoder-decoder structure. By a specific design of the loss function, the model learns to retain the short spatial scale signals contained in the ocean model and calibrate their magnitudes based on GRACE measurements over an area larger than the effective resolution of GRACE. We will compare the downscaled OBP signals to in-situ observations obtained from globally distributed bottom pressure recorders. The possibility of using the downscaled OBP changes for monitoring the meridional overturning circulation via boundary pressures on the continental slope in the North Atlantic will also be discussed. Conference Object North Atlantic GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description The gravimetry measurements from the Gravity Recovery and Climate Experiment (GRACE) satellite mission provide an essential way to monitor changes in ocean bottom pressure (OBP), which is a key variable in understanding ocean circulation. However, the coarse spatial resolution of GRACE OBP hinders resolving mass transports with refined details, particularly on the continental slope. By contrast, classical ocean forward models or reanalyses provide small-scale OBP information, but typically suffer from other problems (e.g., uncertainties in forcing fields, bathymetry, or structural errors in the dynamical formulation). In this study, we downscale the GRACE measured OBP to the eddy-permitting resolution of 0.25º using a self-supervised deep learning model by considering inputs from external high-resolution ocean models. The proposed deep learning model combines the principles of convolutional neural networks, residual learning, and an encoder-decoder structure. By a specific design of the loss function, the model learns to retain the short spatial scale signals contained in the ocean model and calibrate their magnitudes based on GRACE measurements over an area larger than the effective resolution of GRACE. We will compare the downscaled OBP signals to in-situ observations obtained from globally distributed bottom pressure recorders. The possibility of using the downscaled OBP changes for monitoring the meridional overturning circulation via boundary pressures on the continental slope in the North Atlantic will also be discussed.
format Conference Object
author Gou, J.
Börger, L.
Schindelegger, M.
Soja, B.
spellingShingle Gou, J.
Börger, L.
Schindelegger, M.
Soja, B.
Enhancing the spatial resolution of GRACE ocean bottom pressure using deep learning algorithms
author_facet Gou, J.
Börger, L.
Schindelegger, M.
Soja, B.
author_sort Gou, J.
title Enhancing the spatial resolution of GRACE ocean bottom pressure using deep learning algorithms
title_short Enhancing the spatial resolution of GRACE ocean bottom pressure using deep learning algorithms
title_full Enhancing the spatial resolution of GRACE ocean bottom pressure using deep learning algorithms
title_fullStr Enhancing the spatial resolution of GRACE ocean bottom pressure using deep learning algorithms
title_full_unstemmed Enhancing the spatial resolution of GRACE ocean bottom pressure using deep learning algorithms
title_sort enhancing the spatial resolution of grace ocean bottom pressure using deep learning algorithms
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018723
genre North Atlantic
genre_facet North Atlantic
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-2108
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018723
op_doi https://doi.org/10.57757/IUGG23-2108
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