Synoptic Level Fluctuations of the White Sea

IF 0.7 Q4 GEOSCIENCES, MULTIDISCIPLINARY
A. Kondrin, Anastasia Korablina
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引用次数: 0

Abstract

The level fluctuations of the White Sea (WS) in the synoptic range of time scales including tides and surge fluctuations are considered based on observational data covering the period 2004–2020. The hourly level observation data of the coast stations were used: Sosnovets, Severodvinsk, Solovki, Kem-Port, Kandalaksha, as well as in the area of the White Sea Biological Station of Lomonosov Moscow State University (WSBS MSU) in 2008–2009. The values of spring and neap tides at these points are refined, and their features such as parallax inequality and the influence of shallow water components are considered. The surge run-offs and run-ups are explored based on the analysis of residual sea level fluctuations (RSL), which is determined by removing the tidal component from the observational data. The RSL fluctuations in the Dvina Bay are characterized by the greatest variance. The RSL fluctuations at Solovki and Sosnovets have approximately the same variance, which is significantly lower than in the Dvina Bay. The lowest variance is observed at Kandalaksha. According to the data obtained at the Severodvinsk and Solovki stations, a noticeable increase in RSL variance is observed, which indicates that the intensity of RSL fluctuations increased during the time interval under consideration. This conclusion is also confirmed by the calculations of the positive RSL values survivor function, as well as by the fact that the number of surge run-ups with a height of no less than 100 cm for 11 years (from 2004 to 2014) was only two, and in the six-year period (2015–2020) there were already five such events. The largest surge run-ups at 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 occur less frequently than surge run-ups and, as a rule, are inferior to the latter in their absolute value. The surge run-off on January 31, 2005 was the strongest for the entire period of 2004–2020. At Severodvinsk RSL decreased by 123 cm below the average monthly mark. In other cases, the most significant RSL falls relative to the average monthly value were about 70 cm.
白海天气水平波动
基于2004-2020年期间的观测资料,考虑了白海在天气时间尺度范围内的水位波动,包括潮汐和浪涌波动。2008-2009年使用了Sosnovets、Severodvinsk、Solovki、kemo - port、Kandalaksha沿岸站以及莫斯科国立大学(WSBS MSU)罗蒙诺索夫白海生物站区域的每小时观测数据。对这些点的大潮和小潮值进行了细化,并考虑了它们的视差不等和浅水分量的影响等特征。在对残差海平面波动(RSL)进行分析的基础上,探讨了潮涌径流和潮涌径流,残差海平面波动是通过从观测资料中去除潮汐分量来确定的。德维纳湾的RSL波动幅度最大。Solovki和Sosnovets的RSL波动具有大致相同的方差,显著低于Dvina湾。在坎大拉克沙观察到的差异最小。根据在北德文斯克站和索洛夫基站获得的数据,观察到RSL变化明显增加,这表明在考虑的时间间隔内RSL波动的强度有所增加。正RSL值存活函数的计算也证实了这一结论,并且11年中(2004 - 2014年)高度不低于100 cm的浪涌只有2次,而在6年期间(2015-2020年)已经有5次这样的事件。在本报告所述期间,北德文斯克最大的浪涌高度达到130厘米(2018年8月22日)和153厘米(2011年11月15日)。显著的浪涌径流比浪涌径流发生的频率要低,并且通常在绝对值上低于后者。2005年1月31日的决胜选举是2004-2020年整个期间最强劲的一次。在北德文斯克,RSL比月平均水平下降了123厘米。在其他情况下,相对于月平均值,最显著的RSL下降约为70厘米。
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来源期刊
Russian Journal of Earth Sciences
Russian Journal of Earth Sciences GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
1.90
自引率
15.40%
发文量
41
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