Satellite Observations of Sea Level and Ocean Circulation

A special issue of Geosciences (ISSN 2076-3263). This special issue belongs to the section "Geophysics".

Deadline for manuscript submissions: closed (1 September 2020) | Viewed by 4974

Special Issue Editors


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Guest Editor
Atlantic Oceanographic and Meteorological Laboratory, Cooperative Institute for Marine and Atmospheric Studies, University of Miami/National Oceanic and Atmospheric Administration, NOAA/AOML/PHOD 4301, Rickenbacker Causeway, Miami, FL 33149, USA
Interests: space-borne observations of sea level and ocean circulation; Atlantic Meridional overturning circulation and its role in the regional and global climate variability; processes determining sea level in semi-enclosed seas; meso- and large-scale processes in polar oceans and seas

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Guest Editor
Department of Meteorology, Stockholm University, SE-106 91 Stockholm, Sweden
Interests: North Atlantic Ocean circulation; variability and climate; satellite oceanography

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Guest Editor
Collecte Localisation Satellites, BU Environment & Climat 11, rue Hermès, Parc Technologique du Canal, 31520 Ramonville Saint-Agne, France
Interests: satellite altimetry; sea level variability

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Guest Editor
Jet Propulsion Laboratory, M/S 233-200, 4800 Oak Grove Dr, Pasadena, CA 91109, USA
Interests: GRACE satellite missions; sea level variability; global and regional ocean/climate interactions and feedbacks

Special Issue Information

Dear Colleagues,

The satellite era has revolutionized physical oceanography by expanding the ocean observing system to the truly global scale and providing continuous, synoptic monitoring of the ocean’s surface. Particular advances have been achieved thanks to the advent of satellite altimetry and gravimetry missions that have enabled mapping of the global ocean surface topography for studying the spatiotemporal variability of sea level and ocean currents, which are considered ‘essential climate variables’. Technological developments and the build-up of a constellation of altimetry satellites over the last decades have led to significant improvements in measurement accuracy as well as in spatial and temporal resolution. Dedicated reprocessing of radar altimetry waveforms has greatly improved data quality in coastal and polar regions. Space-borne observations have unveiled many aspects of sea level and ocean circulation, such as the mean dynamic topography, the global mean sea level change, large-scale patterns of sea level variability, mesoscale eddies and fronts, propagation of planetary waves, ocean tides, etc. Combining satellite measurements with in situ observations provides a three-dimensional view of the ocean state and how it evolves with time. Satellite data are widely used to constrain ocean general circulation and climate models to facilitate mechanistic understanding of processes driving ocean and climate variability on different temporal and spatial scales.

Papers on all aspects of sea level and ocean circulation that utilize satellite measurements and combine them with in situ observations and ocean models for process-oriented studies are welcome in this Special Issue.

Potential topics include but are not limited to the following:

  • Global mean sea level rise;
  • Regional and coastal sea level change;
  • Variability of oceanic gyres and regional current systems;
  • Regional heat divergence and deep-ocean warming;
  • Meridional overturning circulation and how it relates to sea level changes;
  • Atmospheric circulation and sea level variability;
  • Dynamics of eddies, fronts, and planetary waves.
Dr. Denis L. Volkov
Dr. Léon Chafik
Dr. Carmen Boening
Dr. Marie-Isabelle Pujol
Guest Editors

Manuscript Submission Information

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Keywords

  • Sea level
  • Satellite altimetry
  • GRACE
  • Ocean currents
  • Satellite oceanography
  • Mesoscale processes
  • Ocean heat content
  • Meridional overturning circulation
  • Coastal processes

Published Papers (1 paper)

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Research

20 pages, 4164 KiB  
Article
Sea Level Trend and Fronts in the South Atlantic Ocean
by Laura A. Ruiz-Etcheverry and Martin Saraceno
Geosciences 2020, 10(6), 218; https://doi.org/10.3390/geosciences10060218 - 3 Jun 2020
Cited by 13 | Viewed by 4551
Abstract
The understanding of the physical drivers of sea level trend is crucial on global and regional scales. In particular, little is known about the sea level trend in the South Atlantic Ocean in comparison with other parts of the world. In this work, [...] Read more.
The understanding of the physical drivers of sea level trend is crucial on global and regional scales. In particular, little is known about the sea level trend in the South Atlantic Ocean in comparison with other parts of the world. In this work, we computed the South Atlantic mean sea level (SAMSL) trend from 25 years of satellite altimetry data, and we analyzed the contributions of steric height (thermosteric and halosteric components) and ocean mass changes for the period 2005–2016 when all the source data used (Argo, GRACE and satellite altimetry) overlap. The SAMSL trend is 2.65 ± 0.24 mm/yr and is mostly explained by ocean mass trend, which is 2.22 ± 0.21 mm/yr. However, between 50° S–33° S, the steric height component constitutes the main contribution in comparison with the ocean mass component. Within that latitudinal band, three regions with trend values higher than the SAMSL trend are observed when considering 25 years of satellite SLA. In the three regions, a southward displacement of the Subtropical, Subantarctic, and Polar Fronts is observed. The southward shift of the fronts is associated with the strengthening and polar shift of westerly winds and contributes to a clear thermosteric trend that translates to the SLA trend observed in those regions. Full article
(This article belongs to the Special Issue Satellite Observations of Sea Level and Ocean Circulation)
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