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Coastal trapped waves in the northwestern Mediterranean

机译:地中海西北部沿海被困海浪

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摘要

This paper presents a study of coastal trapped waves on the continental margin of the northwestern Mediterranean. Cyclonically propagating waves along the coast were determined by cross-correlating alongshore current and sea level time series measured at different locations. Significant correlations between alongshore current time series were obtained at different time tags corresponding to the first three coastal trapped waves (CTW) modes. However, correlations between sea level time series were just found for the first CTW mode. The wind-forced coastal trapped theory (with bottom friction and scattering) was applied to the region and model output was compared with data. This application used five coastal sections, a summer or winter stratification, and winds from five coastal sites. The model was able to successfully reproduce observed alongshore current fluctuations in the Catalan Sea. The impact of stratification on CTW was proposed as the mechanism which reduces the effect of the complex topography on low-frequency alongshore flow. (C) 2004 Elsevier Ltd. All rights reserved.
机译:本文介绍了西北地中海大陆边缘的沿海被困波研究。通过沿海岸流和在不同位置测得的海平面时间序列进行互相关,可以确定沿海岸的周期性传播波。在对应于前三个沿海陷波(CTW)模式的不同时间标签上获得了沿岸当前时间序列之间的显着相关性。但是,仅在第一个CTW模式下发现了海平面时间序列之间的相关性。将风力海岸陷陷理论(具有底部摩擦和散射)应用于该区域,并将模型输出与数据进行比较。该应用程序使用了五个沿海地区,夏季或冬季分层以及来自五个沿海站点的风。该模型能够成功地再现加泰罗尼亚海中观察到的近岸海流波动。提出了分层对CTW的影响,作为减少复杂地形对低频沿岸水流影响的机理。 (C)2004 Elsevier Ltd.保留所有权利。

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