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Evidence of Near-Surface Density Stratification as a Factor in Extreme Seiche Events at Ciutadella Harbor, Menorca Island

机译:在梅诺卡岛休达德亚港发生的极端塞奇事件中,近地表密度分层的证据

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Large-amplitude harbor seiches at Ciutadella on Menorca Island in the western Mediterranean are related to local atmospheric conditions and it has been suggested that the seiche forcing mechanism involves the transfer of atmospheric energy to baroclinic modes in offshore waters. To explore this concept we examined the relationship between seasonal patterns of harbor seiche activity and water temperature. Results indicate that during the season of harbor water cooling, the probability of large harbor seiche activity varies linearly with water temperature. During the season of water warming, however, the probability of large seiche activity varies exponentially with the rate of water warming which is maximum at the summer solstice. These patterns in large seiche activity are in accord with published accounts and may result from seasonal changes in near-surface density stratification of the water offshore of Ciutadella.
机译:地中海西部梅诺卡岛休达德亚的大振幅海港围岩与当地的大气条件有关,有人提出围岩强迫机制涉及将大气能量转移到近海的斜压模式。为了探索这一概念,我们研究了港口清澈活动的季节性模式与水温之间的关系。结果表明,在港口水冷季节,大型港口seiche活动的概率随水温线性变化。然而,在水变暖的季节,大量的seiche活动的可能性随夏至时水变暖的速率呈指数变化。大型塞奇活动的这些模式与已发表的报道相符,可能是由于休达德亚(Ciutadella)海上水的近地表密度分层的季节性变化导致的。

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