Identifying Ocean Submesoscale Activity From Vertical Density Profiles Using Machine Learning

Abstract Submesoscale eddies are important features in the upper ocean where they mediate air‐sea exchanges, convey heat and tracer fluxes into ocean interior, and enhance biological production. However, due to their small size (0.1–10 km) and short lifetime (hours to days), directly observing subme...

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Main Authors: Leyu Yao, John R. Taylor, Dani C. Jones, Scott D. Bachman
Format: Article
Language:English
Published: American Geophysical Union (AGU) 2025-01-01
Series:Earth and Space Science
Subjects:
Online Access:https://doi.org/10.1029/2022EA002618
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author Leyu Yao
John R. Taylor
Dani C. Jones
Scott D. Bachman
author_facet Leyu Yao
John R. Taylor
Dani C. Jones
Scott D. Bachman
author_sort Leyu Yao
collection DOAJ
description Abstract Submesoscale eddies are important features in the upper ocean where they mediate air‐sea exchanges, convey heat and tracer fluxes into ocean interior, and enhance biological production. However, due to their small size (0.1–10 km) and short lifetime (hours to days), directly observing submesoscales in the field generally requires targeted high resolution surveys. Submesoscales increase the vertical density stratification of the upper ocean and qualitatively modify the vertical density profile. In this paper, we propose an unsupervised machine learning algorithm to identify submesoscale activity using vertical density profiles. The algorithm, based on the profile classification model (PCM) approach, is trained and tested on two model‐based data sets with vastly different resolutions. One data set is extracted from a large‐eddy simulation (LES) in a 4 km by 4 km domain and the other from a regional model for a sector in the Southern Ocean. We show that the adapted PCM can identify regions with high submesoscale activity, as characterized by the vorticity field (i.e., where surface vertical vorticity ζ is similar to Coriolis frequency f and Rossby number Ro=ζ/f∼O(1)), using solely the vertical density profiles, without any additional information on the velocity, the profile location, or horizontal density gradients. The results of this paper show that the adapted PCM can be applied to data sets from different sources and provides a method to study submesoscale eddies using global data sets (e.g., CTD profiles collected from ships, gliders, and Argo floats).
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spelling doaj-art-112453b8c4184467bbbde375fe7f69072025-01-28T11:08:39ZengAmerican Geophysical Union (AGU)Earth and Space Science2333-50842025-01-01121n/an/a10.1029/2022EA002618Identifying Ocean Submesoscale Activity From Vertical Density Profiles Using Machine LearningLeyu Yao0John R. Taylor1Dani C. Jones2Scott D. Bachman3Department of Applied Mathematics and Theoretical Physics University of Cambridge Cambridge UKDepartment of Applied Mathematics and Theoretical Physics University of Cambridge Cambridge UKCooperative Institute for Great Lakes Research (CIGLR) University of Michigan Ann Arbor MI USANational Center for Atmospheric Research Boulder CO USAAbstract Submesoscale eddies are important features in the upper ocean where they mediate air‐sea exchanges, convey heat and tracer fluxes into ocean interior, and enhance biological production. However, due to their small size (0.1–10 km) and short lifetime (hours to days), directly observing submesoscales in the field generally requires targeted high resolution surveys. Submesoscales increase the vertical density stratification of the upper ocean and qualitatively modify the vertical density profile. In this paper, we propose an unsupervised machine learning algorithm to identify submesoscale activity using vertical density profiles. The algorithm, based on the profile classification model (PCM) approach, is trained and tested on two model‐based data sets with vastly different resolutions. One data set is extracted from a large‐eddy simulation (LES) in a 4 km by 4 km domain and the other from a regional model for a sector in the Southern Ocean. We show that the adapted PCM can identify regions with high submesoscale activity, as characterized by the vorticity field (i.e., where surface vertical vorticity ζ is similar to Coriolis frequency f and Rossby number Ro=ζ/f∼O(1)), using solely the vertical density profiles, without any additional information on the velocity, the profile location, or horizontal density gradients. The results of this paper show that the adapted PCM can be applied to data sets from different sources and provides a method to study submesoscale eddies using global data sets (e.g., CTD profiles collected from ships, gliders, and Argo floats).https://doi.org/10.1029/2022EA002618oceanographymachine learning
spellingShingle Leyu Yao
John R. Taylor
Dani C. Jones
Scott D. Bachman
Identifying Ocean Submesoscale Activity From Vertical Density Profiles Using Machine Learning
Earth and Space Science
oceanography
machine learning
title Identifying Ocean Submesoscale Activity From Vertical Density Profiles Using Machine Learning
title_full Identifying Ocean Submesoscale Activity From Vertical Density Profiles Using Machine Learning
title_fullStr Identifying Ocean Submesoscale Activity From Vertical Density Profiles Using Machine Learning
title_full_unstemmed Identifying Ocean Submesoscale Activity From Vertical Density Profiles Using Machine Learning
title_short Identifying Ocean Submesoscale Activity From Vertical Density Profiles Using Machine Learning
title_sort identifying ocean submesoscale activity from vertical density profiles using machine learning
topic oceanography
machine learning
url https://doi.org/10.1029/2022EA002618
work_keys_str_mv AT leyuyao identifyingoceansubmesoscaleactivityfromverticaldensityprofilesusingmachinelearning
AT johnrtaylor identifyingoceansubmesoscaleactivityfromverticaldensityprofilesusingmachinelearning
AT danicjones identifyingoceansubmesoscaleactivityfromverticaldensityprofilesusingmachinelearning
AT scottdbachman identifyingoceansubmesoscaleactivityfromverticaldensityprofilesusingmachinelearning