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Reconstruction of the space and time variability of thermohaline fields in the Sevastopol Bay

机译:塞瓦斯托波尔湾热盐场的时空变化重建

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The aim of the present work is to reconstruct the space and time variability of the three-dimensional fields of currents, temperature, salinity, and density in the Sevastopol Bay under the influence of the actual external factors in 1999. For this purpose, we use a version of the numerical multilayer model on the σ-coordinates. A vast array of the data of observations accumulated as a result of regular monitoring of the Sevastopol Bay contains, in particular, the data on the sea-surface temperature measured with six-hour intervals (at the hydrometeorological station located near the center of the bay) and almost monthly vertical profiles of temperature and salinity obtained at seven hydrological stations. The comparison of the numerical results with the data of observations enables us to conclude that, in general, the model fairly correctly describes the space structure and rearrangements of the fields of temperature and salinity. Among the most important distinctions, we can mention the fact that the fresh river water penetrating into the bay is mixed with seawater faster than predicted by the model. We also discuss the causes of these distinctions.
机译:本工作的目的是在1999年实际外在因素的影响下,重建塞瓦斯托波尔湾海流,温度,盐度和密度这三个三维场的时空变化。为此,我们使用σ坐标上的多层数值模型的一种形式。定期对塞瓦斯托波尔海湾进行定期监测的结果是,收集到的大量观测数据尤其包含以六小时为间隔测量的海面温度数据(位于靠近海湾中心的水文气象站) )以及在七个水文站获得的几乎每月的温度和盐度垂直分布图。数值结果与观测数据的比较使我们得出结论,总的来说,该模型相当正确地描述了温度和盐度场的空间结构和重排。在最重要的区别中,我们可以提到一个事实,即渗入海湾的新鲜河水与海水混合的速度比模型预测的要快。我们还将讨论造成这些区别的原因。

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