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Propagation of the Vistula Lagoon outflow plume into the Baltic Sea: Satellite observations, in-situ measurements and numerical modeling

机译:维斯杜拉泻湖流出羽流向波罗的海的传播:卫星观测,现场测量和数值模拟

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The influence of wind and hydrodynamic processes on spreading of turbid waters from the Vistula Lagoon into the Baltic Sea was studied. The research was based on joint analysis of remote sensing data, simultaneous subsatellite measurements and numerical modeling. The sharp difference in water optical properties of the Baltic Sea and the Vistula Lagoon, affected by intense summer bloom of cyanobacteria, made it possible to study the evolution and transformation of the outflow in July - early August 2014 using visible satellite data. Forced by coastal jet streams, the outflow spread throughout the Bay of Gdansk, dramatically affected by the circulation processes in the bay. A three-dimensional structure of the outflow was analyzed. In-situ measurements revealed the presence of the Vistula waters exclusively at the upper water layer. A numerical simulation of suspended matter spreading over the Bay of Gdansk was performed using a modified Princeton Ocean Model (POM).
机译:研究了风和水动力过程对浑水从维斯杜拉泻湖扩散到波罗的海的影响。该研究基于对遥感数据的联合分析,同时进行的亚卫星测量和数值建模。波罗的海和维斯杜拉泻湖的水光学特性存在明显差异,受到蓝藻夏季盛放的影响,因此有可能使用可见的卫星数据研究2014年7月至2014年8月初流出的演变和转化。在沿海喷气流的推动下,流出物扩散到格但斯克湾,并受到该湾环流过程的极大影响。分析了流出物的三维结构。原位测量表明,维斯瓦河水仅存在于上水层。使用改进的普林斯顿海洋模型(POM)对悬浮在格但斯克湾的悬浮物进行了数值模拟。

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