根据 2004-2020 年观测数据得出的白色海潮水位波动情况

A. Kondrin, A.D. Korablina
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摘要

根据 2004-2020 年期间的观测数据,考虑了时间尺度同步范围内白海剩余水位的波动,包括浪涌波动。分析了索斯诺维茨、塞韦罗德文斯克、索洛夫基和坎达拉克沙沿海点的每小时水位数据。根据对残余海平面(RSL)波动的分析,对涌浪的上升和径流进行了研究,残余海平面是通过去除观测数据中的潮汐成分计算得出的。德维纳湾的 RSL 波动差异最大。索斯诺维茨和索洛夫基的 RSL 波动方差大致相同,明显低于德维纳湾。坎达拉沙的方差最小。根据在塞韦罗文斯克站和索洛夫基站获得的数据,在所考虑的时间段内,发现 RSL 波动的方差明显增大,这表明其强度在增加。如果将五年期进行比较,2004-2008 年,塞韦罗德文斯克的平均离散度为 327.3 平方厘米,2009-2013 年为 341.4 平方厘米,2016-2020 年为 386.8 平方厘米。这一结论在 RSL 正偏差概率的计算中得到了证实,2004-2015 年的 12 年间,高度不低于 100 厘米的涌浪次数仅为 2 次,而在 2016-2020 年的 5 年间,已经出现了 5 次这样的涌浪。文中描述了白海发生涌浪上升的七种天气形势,其中两种是以前从未考虑过的。在本文考虑的 98 个浪涌上升案例中,各种轨迹的西方气旋占 73 个(74.5%)。在本报告所述期间,塞维罗德文斯克最大的浪涌高达 130 厘米(2018 年 8 月 22 日)和 153 厘米(2011 年 11 月 15 日)。显著的浪涌径流频率低于浪涌暴涨频率,通常绝对值较低。在整个 2004-2020 年期间,2005 年 1 月 31 日的浪涌径流最为明显。塞韦罗德文斯克的 RSL 比月平均值下降了 123 厘米,索洛夫基下降了 112 厘米。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
WHITE SEA SURGE LEVEL FLUCTUATIONS ACCORDING TO OBSERVATION DATA 2004-2020
Fluctuations of the residual level of the White Sea in the synoptic range of time scales, including surge fluctuations, are considered on the basis of observation data covering 2004-2020 period. Hourly data on the level at coastal points of Sosnovets, Severodvinsk, Solovki and Kandalaksha were analyzed. The surge run-ups and run-offs are studied based on the analysis of residual sea level (RSL) fluctuations, which is calculated by removing the tidal component from the observation data. The Dvina Bay RSL fluctuations are characterized by the greatest variance. The RSL fluctuations at Sosnovets and Solovki have approximately the same variance, which is significantly lower than in Dvina Bay. The lowest variance is observed in Kandalaksha. According to the data obtained at the Severodvinsk and Solovki stations, a noticeable increase in the variance of RSL fluctuations is observed over the considered period of time, which indicates an increase in their intensity. If five-year periods are compared, the average dispersion in Severodvinsk is 327,3 cm2 in 2004-2008, 341,4 cm2 in 2009-2013, and 386,8 cm2 in 2016-2020. This conclusion is confirmed by the calculations of the probability of positive RSL deviations, as well as by the fact that the number of surge run-ups with a height no less than 100 cm was only two during 12 years from 2004 to 2015, and there were already five such surges in the five-year period 2016-2020. Seven types of synoptic situations are described in which surge run-ups occurred in the White Sea, two of which were not previously considered. Western cyclones of various trajectories account for 73 (74,5%) out of 98 cases of surge run-ups considered in the paper. The largest surge run-ups in Severodvinsk during the period under review reached a height of 130 cm (August 22, 2018) and 153 cm (November 15, 2011). Significant surge run-offs are less frequent than surge run-ups, being, as a rule, lower in their absolute value. The surge run-off on January 31, 2005 was the most pronounced for the entire period 2004-2020. The RSL in Severodvinsk dropped by 123 cm below the monthly average, and by 112 cm in Solovki.
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