Pierrick Penven, Jean-Francois Ternon, Margaux Noyon, Steven Herbette, Gildas Cambon, Caroline Comby, Pierre L’Hégaret, Bernardino S. Malauene, Claire Ménesguen, Fialho Nehama, Gustav Rauntenbach, Yula Rufino, Floriane Sudre
{"title":"Characterizing the Central Structure of a Mesoscale Eddy-Ring Dipole in the Mozambique Channel From In Situ Observations","authors":"Pierrick Penven, Jean-Francois Ternon, Margaux Noyon, Steven Herbette, Gildas Cambon, Caroline Comby, Pierre L’Hégaret, Bernardino S. Malauene, Claire Ménesguen, Fialho Nehama, Gustav Rauntenbach, Yula Rufino, Floriane Sudre","doi":"10.1029/2024JC021913","DOIUrl":null,"url":null,"abstract":"<p>During the RESILIENCE cruise aboard the R/V Marion Dufresne II (April 19–24 May 2022), a high-resolution in situ observation campaign investigated a mesoscale dipole in the Mozambique Channel, composed of a large anticyclonic ring and a cyclonic eddy. Using an innovative adaptive sampling strategy to track its movement, we employed continuous observing systems, including a Moving Vessel Profiler and Acoustic Doppler Current Profilers, to capture high-resolution vertical sections. The results revealed a distinct dipolar structure: The 250 km-wide anticyclonic ring featured low chlorophyll and homogeneous waters, while the smaller cyclonic eddy exhibited higher chlorophyll concentrations and pronounced salinity variations. These include patches, vertically stacked layers, and filaments, reflecting a mix of contrasted water masses from the southern Mozambique Channel and the Sofala Bank. A central jet between the eddies exhibited horizontal velocities up to 130 cm <span></span><math>\n <semantics>\n <mrow>\n <msup>\n <mi>s</mi>\n <mrow>\n <mo>−</mo>\n <mn>1</mn>\n </mrow>\n </msup>\n </mrow>\n <annotation> ${\\mathrm{s}}^{-1}$</annotation>\n </semantics></math>, facilitating significant offshore transport exceeding 10 Sverdrups in the upper 250 m and emphasizing the dipole's role in eastward water movement. Vertical velocities, derived from the Quasi-Geostrophic Omega equation, highlighted the influence of smaller-scale structures in driving vertical motions, reaching 40 m <span></span><math>\n <semantics>\n <mrow>\n <msup>\n <mtext>day</mtext>\n <mrow>\n <mo>−</mo>\n <mn>1</mn>\n </mrow>\n </msup>\n </mrow>\n <annotation> ${\\text{day}}^{-1}$</annotation>\n </semantics></math> at depth. Lagrangian particle trajectories revealed the dipole's spiraling structure and its connectivity to coastal waters. These findings show that Mozambique Eddy-Ring Dipoles efficiently transport properties from the continental shelf to the open ocean, enhancing regional ecosystem connectivity. This work provides new insights into their biogeochemical, biological and ecological significance, challenging traditional cyclonic/anticyclonic eddy paradigms, and setting the foundation for future studies on mesoscale dipoles in the region.</p>","PeriodicalId":54340,"journal":{"name":"Journal of Geophysical Research-Oceans","volume":"130 3","pages":""},"PeriodicalIF":3.3000,"publicationDate":"2025-03-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2024JC021913","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geophysical Research-Oceans","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1029/2024JC021913","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"OCEANOGRAPHY","Score":null,"Total":0}
引用次数: 0
Abstract
During the RESILIENCE cruise aboard the R/V Marion Dufresne II (April 19–24 May 2022), a high-resolution in situ observation campaign investigated a mesoscale dipole in the Mozambique Channel, composed of a large anticyclonic ring and a cyclonic eddy. Using an innovative adaptive sampling strategy to track its movement, we employed continuous observing systems, including a Moving Vessel Profiler and Acoustic Doppler Current Profilers, to capture high-resolution vertical sections. The results revealed a distinct dipolar structure: The 250 km-wide anticyclonic ring featured low chlorophyll and homogeneous waters, while the smaller cyclonic eddy exhibited higher chlorophyll concentrations and pronounced salinity variations. These include patches, vertically stacked layers, and filaments, reflecting a mix of contrasted water masses from the southern Mozambique Channel and the Sofala Bank. A central jet between the eddies exhibited horizontal velocities up to 130 cm , facilitating significant offshore transport exceeding 10 Sverdrups in the upper 250 m and emphasizing the dipole's role in eastward water movement. Vertical velocities, derived from the Quasi-Geostrophic Omega equation, highlighted the influence of smaller-scale structures in driving vertical motions, reaching 40 m at depth. Lagrangian particle trajectories revealed the dipole's spiraling structure and its connectivity to coastal waters. These findings show that Mozambique Eddy-Ring Dipoles efficiently transport properties from the continental shelf to the open ocean, enhancing regional ecosystem connectivity. This work provides new insights into their biogeochemical, biological and ecological significance, challenging traditional cyclonic/anticyclonic eddy paradigms, and setting the foundation for future studies on mesoscale dipoles in the region.
在R/V Marion Dufresne II号上的“韧性”号巡航期间(2022年4月19日至5月24日),一项高分辨率的原位观测活动调查了莫桑比克海峡的中尺度偶极子,该偶极子由一个大型反气旋环和一个气旋涡旋组成。使用创新的自适应采样策略来跟踪其运动,我们使用连续观测系统,包括移动船舶剖面仪和声学多普勒电流剖面仪,来捕获高分辨率的垂直剖面。结果显示了明显的偶极结构:250公里宽的反气旋环具有低叶绿素和均匀水的特征,而较小的气旋涡具有较高的叶绿素浓度和明显的盐度变化。这些包括斑块、垂直堆叠层和细丝,反映了来自莫桑比克南部海峡和索法拉海岸的对比水团的混合。漩涡之间的中心射流显示出高达130厘米s -1 ${\ mathm {s}}^{-1}$的水平速度。促进了250米以上超过10个Sverdrups的海上运输,并强调了偶极子在东向水运动中的作用。由准地转Omega方程导出的垂直速度突出了较小尺度结构在驱动垂直运动中的影响,在深度达到40 m day -1 ${\text{day}}^{-1}$。拉格朗日粒子轨迹揭示了偶极子的螺旋结构及其与沿海水域的联系。这些发现表明,莫桑比克涡旋环偶极子有效地将性质从大陆架运输到公海,增强了区域生态系统的连通性。本研究为进一步认识其生物地球化学、生物学和生态学意义提供了新的视角,对传统的气旋/反气旋涡旋模式提出了挑战,并为该地区中尺度偶极子的进一步研究奠定了基础。