Transport dynamics in a complex coastal archipelago

IF 4.1 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Ocean Science Pub Date : 2024-01-17 DOI:10.5194/os-20-69-2024
Elina Miettunen, L. Tuomi, A. Westerlund, H. Kanarik, K. Myrberg
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Abstract

Abstract. The Archipelago Sea (in the Baltic Sea) is characterised by thousands of islands of various sizes and steep gradients of the bottom topography. Together with the much deeper Åland Sea, the Archipelago Sea acts as a pathway to the water exchange between the neighbouring basins, Baltic proper and Bothnian Sea. We studied circulation and water transports in the Archipelago Sea using a new configuration of the NEMO 3D hydrodynamic model that covers the Åland Sea–Archipelago Sea region with a horizontal resolution of around 500 m. The results show that currents are steered by the geometry of the islands and straits and the bottom topography. Currents are highest and strongly aligned in the narrow channels in the northern part of the area, with the directions alternating between south and north. In more open areas, the currents are weaker with wider directional distribution. During our study period of 2013–2017, southward currents were more frequent in the surface layer. In the bottom layer, in areas deeper than 25 m, northward currents dominated in the southern part of the Archipelago Sea, while in the northern part southward and northward currents were more evenly represented. Due to the variation in current directions, both northward and southward transports occur. During our study period, the net transport in the upper 20 m layer was southward. Below 20 m depth, the net transport was southward at the northern edge and northward at the southern edge of the Archipelago Sea. There were seasonal and inter-annual variations in the transport volumes and directions in the upper layer. Southward transport was usually largest in spring and summer months, and northward transport was largest in autumn and winter months. The transport dynamics in the Archipelago Sea show different variabilities in the north and south. A single transect cannot describe water transport through the whole area in all cases. Further studies on the water exchange processes between the Baltic proper and the Bothnian Sea through the Archipelago Sea would benefit from using a two-way nested model set-up for the region.
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复杂沿海群岛的运输动态
摘要群岛海(位于波罗的海)有数千个大小不一的岛屿,海底地形陡峭。群岛海与更深的奥兰海一起,成为相邻流域--波罗的海和波罗的海--之间的水交换通道。我们使用新配置的 NEMO 三维流体力学模型研究了群岛海的环流和水体输送情况,该模型覆盖奥兰海-群岛海区域,水平分辨率约为 500 米。结果表明,水流受岛屿和海峡的几何形状以及海底地形的影响。在该地区北部的狭窄海峡中,海流最高且排列整齐,方向南北交替。在较为开阔的区域,水流较弱,方向分布较广。在 2013-2017 年的研究期间,表层的南向流更为频繁。在底层,在群岛海南部水深超过 25 米的区域,北向洋流占主导地位,而在北部,南向和北向洋流的分布较为均匀。由于海流方向的变化,出现了向北和向南的迁移。在我们的研究期间,上层 20 米水层的净迁移量是向南的。在 20 米深度以下,群岛海域北缘的净湍流为南向,南缘为北向。上层的迁移量和迁移方向存在季节和年际变化。南向迁移量通常在春季和夏季最大,北向迁移量在秋季和冬季最大。群岛海的输运动态呈现出南北不同的变化。单一横断面不可能在所有情况下描述整个海域的水流输送情况。进一步研究波罗的海和 Bothnian 海之间通过群岛海的水交换过程,将受益于为该地区建立的双向嵌套模型。
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来源期刊
Ocean Science
Ocean Science 地学-海洋学
CiteScore
5.90
自引率
6.20%
发文量
78
审稿时长
6-12 weeks
期刊介绍: Ocean Science (OS) is a not-for-profit international open-access scientific journal dedicated to the publication and discussion of research articles, short communications, and review papers on all aspects of ocean science: experimental, theoretical, and laboratory. The primary objective is to publish a very high-quality scientific journal with free Internet-based access for researchers and other interested people throughout the world. Electronic submission of articles is used to keep publication costs to a minimum. The costs will be covered by a moderate per-page charge paid by the authors. The peer-review process also makes use of the Internet. It includes an 8-week online discussion period with the original submitted manuscript and all comments. If accepted, the final revised paper will be published online. Ocean Science covers the following fields: ocean physics (i.e. ocean structure, circulation, tides, and internal waves); ocean chemistry; biological oceanography; air–sea interactions; ocean models – physical, chemical, biological, and biochemical; coastal and shelf edge processes; paleooceanography.
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