Distribution, Mixing, and Transformation of a Loop Current Ring Waters: The Case of Gulf of Mexico

Abstract Mesoscale warm‐core rings, known as Loop Current rings (LCRs) reshape the Gulf of Mexico water masses by redistributing large amounts of heat and salt laterally. LCRs also transform water masses via diapycnal mixing, but the mechanisms by which this occurs are poorly measured. Here, we present glider‐MicroPod turbulence observations that reveal enhanced mixing below the mixed layer, along the eddy edges, driving the LCR's heat, salt, and oxygen exchanges. Interleavings of adjacent water masses may be interpreted mainly as a manifestation of submesoscale processes through stirring of the spice gradients, which facilitates double‐diffusive mixing that transforms Subtropical Underwater into Gulf Common Water. Our findings highlight the need for ocean models to parameterize double‐diffusive mixing processes directly resulting from submesoscale tracer stirring, which may be important at basin scale in the presence of LCRs in the Gulf of Mexico.

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Publication Details

Journal
Geophysical Research Letters
Published
2024-11-29
DOI
https://doi.org/10.1029/2024gl110845
Citations
2
Primary Topic
Oceanographic and Atmospheric Processes
Type
article
Field-Weighted Citation Impact
0.96

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article

Distribution, Mixing, and Transformation of a Loop Current Ring Waters: The Case of Gulf of Mexico

Enric Pallàs‐Sanz, Sheila N. Estrada‐Allis, Thomas Meunier, Julio Sheinbaum et al.
2 citations
Geophysical Research Letters
Oceanographic and Atmospheric Processes
0.96
article

Distribution, Mixing, and Transformation of a Loop Current Ring Waters: The Case of Gulf of Mexico

Enric Pallàs‐Sanz, Sheila N. Estrada‐Allis, Thomas Meunier, Julio Sheinbaum, Angel Ruiz‐Angulo, Mathieu Gentil, Giovanni Durante, Miguel Tenreiro, Leo Middleton
article en
2 citations

Abstract

Abstract Mesoscale warm‐core rings, known as Loop Current rings (LCRs) reshape the Gulf of Mexico water masses by redistributing large amounts of heat and salt laterally. LCRs also transform water masses via diapycnal mixing, but the mechanisms by which this occurs are poorly measured. Here, we present glider‐MicroPod turbulence observations that reveal enhanced mixing below the mixed layer, along the eddy edges, driving the LCR's heat, salt, and oxygen exchanges. Interleavings of adjacent water masses may be interpreted mainly as a manifestation of submesoscale processes through stirring of the spice gradients, which facilitates double‐diffusive mixing that transforms Subtropical Underwater into Gulf Common Water. Our findings highlight the need for ocean models to parameterize double‐diffusive mixing processes directly resulting from submesoscale tracer stirring, which may be important at basin scale in the presence of LCRs in the Gulf of Mexico.

Geophysical Research LettersVol. 51(23)
Centre National de la Recherche Scientifique (FR), Université de Toulon (FR), Ifremer (FR), Université de Bretagne Occidentale (FR), University of Iceland (IS), Aix-Marseille Université (FR), Ensenada Institute of Technology (MX), Laboratory for Ocean Physics and Satellite Remote Sensing (FR), Institut Universitaire Européen de la Mer (FR), Institut de Recherche pour le Développement (FR), Centro de Investigación Científica y de Educación Superior de Ensenada (MX), Woods Hole Oceanographic Institution (US)
Centro de Investigación Científica y de Educación Superior de Ensenada, Baja California
Life below water
Openalex Percentile: Top 24%
Oceanographic and Atmospheric Processes
0.96
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