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Seasonal Fluctuations of the Baltic Sea Level

机译:波罗的海海平面的季节性波动

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摘要

Seasonal annual (Sa) and seasonal semiannual (Ssa) fluctuations are the dominant feature of long-period sea level variability in the Baltic Sea. Long-term series of observations (monthly mean sea level data) from the PSMSL database are used to estimate amplitudes and phases and to reveal spatial and temporal variations. It was found that the variations of seasonal amplitudes were quite significant from year to year and synchronous both within the Baltic Sea and in the Kattegat and Skagerrak straits. Climatologically averaged amplitudes and phases were calculated from 74 tide gauges, and the maps of spatial variability of seasonal constituents are plotted. The annual harmonic of the sea level gradually increases from the entrance (Danish Straits) to the heads of gulfs. The maximum amplitude of 12.7 cm is observed in the heads of the Gulf of Finland and Gulf of Bothnia. It is revealed that seasonal fluctuations in the Baltic Sea are caused by the zonal wind component.
机译:季节性的年度(Sa)和季节性的半年(Ssa)波动是波罗的海长期海平面变化的主要特征。来自PSMSL数据库的长期观测数据(每月平均海平面数据)被用于估计振幅和相位,并揭示时空变化。结果发现,在波罗的海以及卡特加特海峡和斯卡格拉克海峡内,季节性振幅的变化每年都非常显着,并且是同步的。由74个潮汐仪计算出气候平均振幅和相位,并绘制了季节性成分的空间变化图。从入口(丹麦海峡)到海湾的顶部,海平面的年谐波逐渐增加。在芬兰湾和博特尼亚湾的头部观测到最大振幅为12.7厘米。结果表明,波罗的海的季节性波动是由纬向风分量引起的。

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  • 来源
    《Russian meteorology and hydrology》 |2014年第12期|814-822|共9页
  • 作者

    I. P. Medvedev;

  • 作者单位

    Shirshov Institute of Oceanology, Russian Academy of Sciences, Nakhimovskii pr. 36, Moscow, 117997 Russia;

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  • 正文语种 eng
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