首页> 外文会议>International conference on port and ocean engineering under arctic conditions >ASSESSING THE IMPACT OF THE PLANNED APPROACH CHANNEL TO THE SEAPORT SABETTA ON SALINITY CHANGES IN THE GULF OF OB
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ASSESSING THE IMPACT OF THE PLANNED APPROACH CHANNEL TO THE SEAPORT SABETTA ON SALINITY CHANGES IN THE GULF OF OB

机译:评估计划的方法渠道对海底盐度变化的海港Sabetta的影响

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The assessment is made of the changes in the salt regime near the channel projected in the northern part of the Gulf of Ob that can be caused by topography change due to the construction of the approach channel to the seaport Sabetta. Since the full-scale experiment is not possible in this case, the only way to solve this problem is performing experiments on the salt regime sensitivity to the topography change with using numerical modelling. For this purpose, we use the well-proved Russian universal σ-model of ocean and sea circulation INMOM (Institute of Numerical Mathematics Ocean Model), developed at the Institute of Numerical Mathematics of the Russian Academy of Sciences. This model is implemented to simulate the circulation of the Kara and Pechora Seas. Its global version is used in the framework of international projects CORE (Coordinated Ocean-ice Reference Experiments) and CMIP (Coupled Model Intercomparison Project). The experiments conducted in the Gulf of Ob show us that the strongest annual mean salinity growth due to the presence of the channel occurs near this channel and reaches 0.45 PSU in absolute or 4.5% in relative. While moving away the channel one can see a significant reduction of its impact. The natural interannual salinity variability is revealed in the water area under research (RMS is about 2÷3 PSU, variability is up to 8 PSU), which depends on both river runoff variability and atmospheric forcing. At the same time, using the results of numerical simulations, it was obtained that the natural interannual salinity variability is much higher than its change caused by the presence of the approach channel.
机译:评估是对博士附近的盐制度的变化,这些渠道在ob北部的北部,这可能是由于施工渠道的建设到海港Sabetta而导致的地形变化。由于在这种情况下不可能进行全面的实验,因此解决该问题的唯一方法是使用数值模拟对地形改变的盐度敏感性进行实验。为此目的,我们使用经过熟悉的俄罗斯通用Σ模型的海洋和海洋循环inmom(数学学会海洋模型),在俄罗斯科学院数学研究所开发。该模型是实施以模拟卡拉和Pechora海洋的循环。其全球版用于国际项目核心框架(协调海洋冰参考实验)和CMIP(耦合型号互相项目)。在OB的海湾中进行的实验表明,由于存在通道的存在,在该通道附近发生最强的年平均盐度生长,并且在相对的绝对值或4.5%中达到0.45psu。虽然脱离通道,但可以看到其影响的显着降低。在研究下的水域(RMS约为2÷3psu,可变性高达8psu),自然续始盐度变异性揭示,这取决于河流径流变异性和大气强制。同时,使用数值模拟的结果,获得自然持续的盐度变化远高于由接近通道存在引起的变化。

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