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Recent Advances on Oceanic Mesoscale Eddies II

A special issue of Remote Sensing (ISSN 2072-4292). This special issue belongs to the section "Ocean Remote Sensing".

Deadline for manuscript submissions: 1 December 2024 | Viewed by 1754

Special Issue Editors


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Guest Editor
Institute of Marine Sciences, ICM-CSIC, Pg. Marítim Barceloneta, 37-49, 08003 Barcelona, Spain
Interests: physical-biological interactions at submeso- and mesoscales; near-inertial wave dynamics; large-scale currents and ocean biogeochemistry; ocean modeling
Special Issues, Collections and Topics in MDPI journals

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Guest Editor
Consiglio Nazionale delle Ricerche, Istituto per lo Studio Degli Impatti Antropici e Sostenibilità in Ambiente Marino, 09170 Oristano, Italy
Interests: mesoscale oceanic eddy; ocean circulation; water masses properties; mesoscale ocean dynamics and its interactions with marine ecosystem; in situ observations; satellite oceanography; operational oceanography
Special Issues, Collections and Topics in MDPI journals

Special Issue Information

Dear Colleagues,

Mesoscale eddies are energetic coherent structures that play a crucial role in the ocean. They have typical horizontal scales ranging from 10–100 km and lifetimes from months to sometimes years. They can connect the coastal and the open ocean, generate a downscale energy cascade, and trap and transport heat, salt, pollutants and biogeochemical tracers at long distances. They can also modulate the mixed layer depth, regulate air–sea heat and gas fluxes and influence local winds, clouds and rainfall. As a result, they have a profound impact on the ocean–atmosphere–biosphere system. However, the myriad mechanisms that control or impact all the above-mentioned components of the ocean are not yet fully explored.

Major breakthroughs in remote sensing have paved the way for a global understanding of the oceanic circulation. Automatic eddy detection and tracking algorithms, applied to low-resolution altimetric data, are efficient tools to study the dynamics of mesoscale eddies. To complete these standard techniques, new methods such as deep learning have been developed to analyse visible images (SST, Ocean Colour) that contain higher spatial resolution eddy signatures but can be corrupted by cloud coverage. These recent advances, combined with in situ data (Argo floats, gliders, surface drifter, oceanographic cruises, etc.) and eddy resolving models, provide invaluable information on surface dynamics and the three-dimensional nature of eddies.

The aim of this Special Issue is to advance our understanding of complex mesoscale eddy activity. Therefore, this SI welcomes manuscripts dealing with eddy dynamics, eddy properties variability, transport, or impact on ocean circulations and on marine ecosystems We accept contributions based on standard and new methods that can permit the improvement of mesoscale eddy identification and knowledge. We also strongly encourage works that combine these remote sensing techniques with theory, in situ observations data, and/or modelling output to explore complex physical–biological interactions driven by mesoscale eddies or to unveil the vertical structure of surface imprints of eddies detected by satellites.

Dr. Mariona Claret
Dr. Angelo Perilli
Guest Editors

Manuscript Submission Information

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Remote Sensing is an international peer-reviewed open access semimonthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2700 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

  • mesoscale ocean dynamics
  • satellite remote sensing
  • ocean in situ monitoring
  • ocean circulation
  • eddy resolving ocean models
  • eddy detection and tracking algorithms
  • AI applied to oceanic remote sensing analysis
  • marine ecosystems
  • physical–biological interactions

Related Special Issue

Published Papers (3 papers)

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Research

19 pages, 9502 KiB  
Article
Statistical Analysis of Multi-Year South China Sea Eddies and Exploration of Eddy Classification
by Yang Jin, Meibing Jin, Dongxiao Wang and Changming Dong
Remote Sens. 2024, 16(10), 1818; https://doi.org/10.3390/rs16101818 - 20 May 2024
Viewed by 231
Abstract
Mesoscale eddies are structures of seawater motion with horizontal scales of tens to hundreds of kilometers, impact depths of tens to hundreds of meters, and time scales of days to months. This study presents a statistical analysis of mesoscale eddies in the South [...] Read more.
Mesoscale eddies are structures of seawater motion with horizontal scales of tens to hundreds of kilometers, impact depths of tens to hundreds of meters, and time scales of days to months. This study presents a statistical analysis of mesoscale eddies in the South China Sea (SCS) from 1993 to 2021 based on eddies extracted from satellite remote sensing data using the vector geometry eddy detection method. On average, about 230 eddies with a wide spatial and temporal distribution are observed each year, and the numbers of CEs (52.2%) and AEs (47.8%) are almost similar, with a significant correlation in spatial distribution. In this article, eddies with a lifetime of at least 28 days (17% of the number of total eddies) are referred to as strong eddies (SEs). The SEs in the SCS that persist for several years in similar months and locations, such as the well-known dipole eddies consisting of CEs and AEs offshore eastern Vietnam, are defined as persistent strong eddies (PSEs). SEs and PSEs affect the thermohaline structure, current field, and material and energy transport in the upper ocean. This paper is important as it names the SEs and PSEs, and the naming of eddies can facilitate research on specific major eddies and improve public understanding of mesoscale eddies as important oceanic phenomena. Full article
(This article belongs to the Special Issue Recent Advances on Oceanic Mesoscale Eddies II)
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20 pages, 18856 KiB  
Article
A Gaussian Function Model of Mesoscale Eddy Temperature Anomalies and Research of Spatial Distribution Characteristics
by Yingying Duan, Hao Zhang, Xiao Chen and Manli Zhou
Remote Sens. 2024, 16(10), 1716; https://doi.org/10.3390/rs16101716 - 12 May 2024
Viewed by 399
Abstract
Mesoscale eddies are ubiquitous oceanic phenomena and play an important role in ocean circulation, ocean dynamics, and the transport of material energy. Temperature anomalies are a crucial parameter that reflects the state of mesoscale eddies. This study proposes a Gaussian function model to [...] Read more.
Mesoscale eddies are ubiquitous oceanic phenomena and play an important role in ocean circulation, ocean dynamics, and the transport of material energy. Temperature anomalies are a crucial parameter that reflects the state of mesoscale eddies. This study proposes a Gaussian function model to fit the vertical temperature anomaly (TA) profile to facilitate the analysis of variations, and the principle of the model is based on the fact that each TA profile tends to fluctuate around one or more peaks. The model is extracted and validated using Argo profiles within cyclonic and anticyclonic eddies in the Northwest Pacific Ocean spanning over the period from 2002 to 2021. The validation demonstrates that the model can accurately recover the vertical TA profiles with a limited number of parameters. This makes it suitable for analysing the spatial distribution patterns that require a large sample count. The analysis indicates that eddies with different TA profiles have a spatial aggregation effect in geographic distribution. Eddies with lower extreme temperature anomalies, at depths of 200–300 m, are mainly distributed along two bands on the north side of the Kuroshio Extension (KE) and the North Equatorial Current. Eddies with extreme TAs at the deepest depth (500–600 m) are distributed along the KE. Full article
(This article belongs to the Special Issue Recent Advances on Oceanic Mesoscale Eddies II)
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18 pages, 8078 KiB  
Article
Submesoscale Short-Lived Eddies in the Southwestern Taiwan Strait Observed by High-Frequency Surface-Wave Radars
by Hong Zhao, Xianchang Yue, Li Wang, Xiongbin Wu and Zhangyou Chen
Remote Sens. 2024, 16(3), 589; https://doi.org/10.3390/rs16030589 - 4 Feb 2024
Viewed by 729
Abstract
Surface currents obtained from the high-frequency surface-wave radars (HFSWRs) installed along the coast of Fujian Province are utilized to characterize submesoscale eddies in the southwestern Taiwan Strait from 29 January to 26 March 2013. The algorithm based on vector geometry (VG) has been [...] Read more.
Surface currents obtained from the high-frequency surface-wave radars (HFSWRs) installed along the coast of Fujian Province are utilized to characterize submesoscale eddies in the southwestern Taiwan Strait from 29 January to 26 March 2013. The algorithm based on vector geometry (VG) has been applied to datasets and a total of 414 (161 anticyclonic and 253 cyclonic eddies) were obtained. Eddies with both rotations had a relatively short lifespan (≤3.7 h), and their radii were in the range of 5–22.5 km. Eddies with a lifespan of over 30 minutes were more likely to occur north of the Taiwan Strait shoals and move eastward or northeastward. The deviation of moving directions of eddies with a moving distance of more than 20 km was within 18°. Moreover, eddies could hardly hold their original forms with cyclones extending in the east-west and compressing in the north-south direction, and anticyclones were the opposite. The vorticity and strain rate were proportional to the square of the energy intensity (EI). This study shows that the array HFSWRs have a strong capability to observe short-lived submesoscale eddies. Full article
(This article belongs to the Special Issue Recent Advances on Oceanic Mesoscale Eddies II)
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