Latest Advances in Physical Oceanography—2nd Edition

A special issue of Journal of Marine Science and Engineering (ISSN 2077-1312). This special issue belongs to the section "Physical Oceanography".

Deadline for manuscript submissions: 31 August 2024 | Viewed by 783

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Guest Editor
EPHYSLAB, Environmental PHYsics LABoratory, Facultad de Ciencias, Universidad de Vigo, 32004 Ourense, Spain
Interests: physical oceanography; coastal and estuarine hydrodynamics; river plume dynamics; coastal upwelling; atmosphere-ocean interaction; climate change impact; renewable energies (wave and wind energies)
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Special Issue Information

Dear Colleagues,

Physical oceanography focuses on understanding the physical properties and processes of the world's oceans. It primarily deals with the study of the physical characteristics of seawater; the movement of ocean currents, waves, the distribution of temperature and salinity; and the interaction between the ocean and the atmosphere. The processes studied present a wide range of spatial scales, ranging from centimeter scales relevant to turbulence to the many thousand-kilometer scales of the global circulation, as well as from deep ocean and broader scales to shallow waters and local scales.

This Special Issue has specific objectives that aim to advance knowledge, promote collaboration, and disseminate cutting-edge research in this field. The primary objective is to showcase the latest developments and breakthroughs in the field of physical oceanography. This approach involves presenting research that employs novel methods, technologies, or approaches to study ocean processes. Physical oceanography often overlaps with other disciplines, like climate science, marine biology, and environmental science. This Special Issue aims to encourage interdisciplinary research by featuring studies that bridge gaps between these fields, serving as a platform for collaboration among researchers from different institutions, regions, or countries. Encouraging international cooperation and the exchange of ideas is a valuable goal of this Special Issue, which acts as a forum for discussing the future directions of physical oceanography research. This Special Issue will also focus on addressing the numerous challenges that face physical oceanography, including understanding climate change impacts, ocean circulation dynamics, and the behavior of marine ecosystems, by featuring research that provides insights and solutions. As technology evolves, so does our ability to study the ocean. This Special Issue aims to introduce and discuss cutting-edge technologies, such as autonomous underwater vehicles (AUVs), satellite remote sensing, and high-performance computing, used in physical oceanography research. Lastly, this Special Issue aspires to have a lasting impact on the field by contributing to the body of knowledge and serving as a reference source for researchers, educators, and students interested in physical oceanography.

Prof. Dr. João Miguel Dias
Dr. Mª Teresa de Castro Rodríguez
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. Journal of Marine Science and Engineering is an international peer-reviewed open access monthly 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 2600 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

  • thermohaline circulation
  • wind-induced circulation
  • Ekman transport
  • tides
  • sea level change
  • tsunamis
  • storm surges
  • surface waves
  • internal waves
  • planetary waves
  • ocean–atmosphere interaction
  • climate variability
  • remote sensing

Published Papers (1 paper)

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Research

17 pages, 21014 KiB  
Article
Observations of Near-Inertial Internal Waves over the Continental Slope in the Northeastern Black Sea
by Elizaveta Khimchenko and Alexander Ostrovskii
J. Mar. Sci. Eng. 2024, 12(3), 507; https://doi.org/10.3390/jmse12030507 - 19 Mar 2024
Viewed by 549
Abstract
The article presents observations of near-inertial internal waves (NIWs) in the slope waters of the Black Sea in winter and summer. Rotary spectral analysis of a time series of sea current velocity measurements revealed the prevailing anticyclonic component of the motions near the [...] Read more.
The article presents observations of near-inertial internal waves (NIWs) in the slope waters of the Black Sea in winter and summer. Rotary spectral analysis of a time series of sea current velocity measurements revealed the prevailing anticyclonic component of the motions near the local inertial frequency f. The clockwise rotation of the velocity vector with depth implies that the NIWs propagate downwards. The amplitude of NIWs usually was 0.1–0.2 m s−1. NIWs were observed in the layer of the permanent pycnocline and the seasonal pycnocline, which attenuate below depths of 160 m and 80 m in winter and summer, respectively. The amplitude of the near-inertial kinetic energy (NIKE) showed a close relationship with vertical stratification. During winter, NIKE exhibited maximum values in the layer of the permanent pycnocline, whereas, in summer, it was primarily observed in the seasonal pycnocline layer. The near-inertial oscillations were generally more energetic in winter. Full article
(This article belongs to the Special Issue Latest Advances in Physical Oceanography—2nd Edition)
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