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Abyssal undular vortices in the Easternmediterranean basin

机译:地中海东部盆地的深海波浪状涡旋

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摘要

Abyssal temperature and velocity observations performed within the framework of the neutrinomediterranean observatory, a project devoted to constructing a km3-scale underwatertelescope for the detection of high-energy cosmic neutrinos, demonstrate cross-fertilizationbetween subnuclear physics and experimental oceanography. Here we use data collected southof sicily in the Ionian abyssal plain of the Eastern mediterranean (Em) basin to show for the firsttime that abyssal vortices exist in the Em, at depths exceeding 2,500m. The eddies consist ofchains of near-inertially pulsating mesoscale cyclones/anticyclones. They are embedded in anabyssal current flowing towards north-northwest. The paucity of existing data does not allowfor an unambiguous determination of the vortex origin. A local generation mechanism seemsprobable, but a remote genesis cannot be excluded a priori. The presence of such eddies addsfurther complexity to the discussion of structure and evolution of water masses in the Em.
机译:在中微子地中海天文台的框架内进行的深海温度和速度观测是一个构造km3规模的水下望远镜以检测高能宇宙中微子的项目,该实验证明了亚核物理学与实验海洋学之间的交叉受精。在这里,我们使用在东地中海(Em)盆地爱奥尼亚深渊平原西西里岛南部收集的数据,首次显示出在超过2500m深度的Em中存在深渊涡旋。涡流由近惯性脉动中尺度旋风/反旋风的链组成。它们被嵌入流向西北西北部的深海流中。现有数据的匮乏无法明确确定旋涡的起源。本地生成机制似乎很可能,但是不能先验地排除远程生成。这种涡流的存在使Em中水团的结构和演化的讨论更加复杂。

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