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首页> 外文期刊>Journal of Marine Science and Engineering >Multi-Layered Stratification in the Baltic Sea: Insight from a Modeling Study with Reference to Environmental Conditions
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Multi-Layered Stratification in the Baltic Sea: Insight from a Modeling Study with Reference to Environmental Conditions

机译:波罗的海的多层分层:参考环境条件的模型研究的启示

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The hydrodynamic and transport characteristics of the Baltic Sea in the period 2000–2009 were studied using a fully calibrated and validated 3D hydrodynamic model with a horizontal resolution of 4.8 km. This study provided new insight into the type and dynamics of vertical structure in the Baltic Sea, not considered in previous studies. Thermal and salinity stratification are both addressed, with a focus on the structural properties of the layers. The detection of cooler regions (dicothermal) within the layer structure is an important finding. The detailed investigation of thermal stratification for a 10-year period (i.e., 2000–2009) revealed some new features. A multilayered structure that contains several thermocline and dicothermal layers was identified from this study. Statistical analysis of the simulation results made it possible to derive the mean thermal stratification properties, expressed as mean temperatures and the normalized layer thicknesses. The three-layered model proposed by previous investigators appears to be valid only during the winter periods; for other periods, a multi-layered structure with more than five layers has been identified during this investigation. This study provides detailed insight into thermal and salinity stratification in the Baltic Sea during a recent decade that can be used as a basis for diverse environmental assessments. It extends previous studies on stratification in the Baltic Sea regarding both the extent and the nature of stratification.
机译:我们使用水平校准为4.8 km的经过完全校准和验证的3D水动力模型,研究了2000-2009年期间波罗的海的水动力和输运特征。这项研究为波罗的海垂直结构的类型和动力学提供了新的见识,而先前的研究并未考虑这一点。着重讨论了热分层和盐分分层,重点是层的结构特性。层结构内较冷区域(双热)的检测是一个重要发现。对热分层进行了为期10年(即2000-2009年)的详细调查,发现了一些新功能。从这项研究中鉴定出了包含几个温跃层和双热层的多层结构。对模拟结果进行统计分析,可以得出平均热分层特性,表示为平均温度和归一化层厚度。以前的研究人员提出的三层模型似乎仅在冬季才有效。在其他时期,在此调查过程中已经确定了具有五层以上的多层结构。这项研究提供了对近十年来波罗的海热盐度分层的详细见解,可以用作进行各种环境评估的基础。它扩展了先前关于波罗的海分层的研究,涉及分层的范围和性质。

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