Dynamics of Atmospheric-Driven Surface Currents on The Gulf of Cadiz Continental Shelf and its link with The Strait of Gibraltar and The Western Alboran Sea

IF 3.8 3区 地球科学 Q1 OCEANOGRAPHY
S. Sirviente , M. Bolado-Penagos , J.J. Gomiz-Pascual , J. Romero-Cózar , A. Vázquez , M Bruno
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引用次数: 0

Abstract

Several studies about the coastal circulation over the continental shelf of the Gulf of Cadiz have been published in the last twenty years. One of the most studied features in these papers are the so-called Coastal Counter Currents (CCCs) which are located roughly between the 100 m isobath and the coastline and are directed westwards. Despite the considerable number of articles devoted to the analysis of this phenomenon, the actual along-coast extension and origin of these CCCs currently remain unclear.

In the present study, different mechanisms are proposed to explain the development of these CCCs. They have been revised and discussed taking into account the latest findings from a recent analysis that utilized surface currents derived from High Frequency Radar (HFR) as well as numerical model simulations. The most interesting finding is that the most intense CCCs events are initiated on the coastal margin of the westernmost side of the Strait of Gibraltar, and they are extended further west of Cape Santa Maria. Furthermore, these intense and extensive CCCs seem to be triggered by the joint action of local winds over the Gulf of Cadiz and additional remote effects which are coming from (i) the wind forcing over the Alboran Sea and the easternmost side of the Strait of Gibraltar, and (ii) the Sea Level Atmospheric Pressure forcing over the Ligurian Sea (western Mediterranean Sea). In addition, the same forcing mechanisms are valid to explain the eastward intensification of the coastal currents.

The most relevant feature of the hydrodynamic pattern originated by this combination of forcing agents is its quasi-geostrophic adjustment against the coast in the whole spatial dominion. In addition, these results offer a clear example of how important the effects of forcing in rather remote regions may be in defining the hydrodynamic patterns of certain oceanographic regions.

加的斯大陆架海湾大气驱动的表面流动力学及其与直布罗陀海峡和西阿尔博兰海的联系
近二十年来,关于加的斯湾大陆架沿岸环流的研究已经发表了几篇。这些论文中研究最多的特征之一是所谓的海岸逆流(CCCs),它大致位于100米等深线和海岸线之间,并向西移动。尽管有相当多的文章致力于分析这一现象,但这些CCCs的实际沿海延伸和起源目前仍不清楚。在本研究中,提出了不同的机制来解释这些CCCs的发展。考虑到利用高频雷达(HFR)获得的表面电流以及数值模式模拟的最近分析的最新结果,对它们进行了修订和讨论。最有趣的发现是,最强烈的CCCs事件发生在直布罗陀海峡最西端的沿海边缘,并向圣玛丽亚角以西延伸。此外,这些强烈和广泛的CCCs似乎是由加的斯湾当地风的共同作用和来自(i)阿尔博兰海和直布罗陀海峡最东侧的风强迫和(ii)利古里亚海(地中海西部)的海平面大气压力强迫的额外远程影响引发的。此外,同样的强迫机制也可以解释沿海流向东增强的原因。这种强迫因素组合所产生的水动力格局最相关的特征是其在整个空间范围内对海岸的准地转调整。此外,这些结果提供了一个清楚的例子,说明在相当偏远的地区,强迫的影响在确定某些海洋学区域的水动力模式方面可能是多么重要。
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来源期刊
Progress in Oceanography
Progress in Oceanography 地学-海洋学
CiteScore
7.20
自引率
4.90%
发文量
138
审稿时长
3 months
期刊介绍: Progress in Oceanography publishes the longer, more comprehensive papers that most oceanographers feel are necessary, on occasion, to do justice to their work. Contributions are generally either a review of an aspect of oceanography or a treatise on an expanding oceanographic subject. The articles cover the entire spectrum of disciplines within the science of oceanography. Occasionally volumes are devoted to collections of papers and conference proceedings of exceptional interest. Essential reading for all oceanographers.
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