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Analysis on the Extreme Sea Levels Changes along the Coastline of Bohai Sea, China

机译:环渤海沿岸极端海平面变化分析

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Using hourly sea level data from four tide gauges, the changes of the extreme sea level in the Bohai Sea were analyzed in this work. Three components (i.e., mean sea level, tide and surge) as well as the tide–surge interaction were studied to find which component was important in the changes of extreme sea levels. Significant increasing trends exist in the mean sea level at four tide gauges from 1980 to 2016, and the increase rate ranges from 0.2 to 0.5 cm/year. The mean high tide levels show positive trends at four tide gauges, and the increasing rate (0.1 to 0.3 cm/year) is not small compared with the long-term trends of the mean sea levels. However, the mean tidal ranges show negative trends at Longkou, Qinhuangdao and Tanggu, with the rate from about ?0.7 to ?0.2 cm/year. At Qinhuangdao and Tanggu, the annual surge intensity shows explicit long-term decreasing trend. At all four tide gauges, the storm surge intensity shows distinct inter-annual variability and decadal variability. All four tide gauges show significant tide–surge interaction, the characteristics of the tide–surge interaction differ due to their locations, and no clear long-term change was found. Convincing evidence implies that the extreme sea levels increase during the past decades from 1980 to 2016 at all tide gauges, with the increasing rate differing at different percentile levels. The extreme sea level changes in the Bohai Sea are highly affected by the changes of mean sea level and high tide level, especially the latter. The surge variation contributes to the changes of extreme sea level at locations where the tide–surge interaction is relatively weak.
机译:这项工作使用来自四个潮汐仪的每小时海平面数据,分析了渤海的极端海平面变化。研究了三个要素(即平均海平面,潮汐和潮汐)以及潮汐-潮汐相互作用,以找出哪个要素在极端海平面变化中很重要。从1980年到2016年,四个潮位仪的平均海平面存在明显的上升趋势,并且上升速度在0.2至0.5厘米/年之间。平均高潮位在四个潮位仪上均显示出正趋势,并且与平均海平面的长期趋势相比,增长率(0.1至0.3厘米/年)不小。然而,在龙口,秦皇岛和塘沽,平均潮汐范围呈负趋势,速率约为每年0.7至0.2厘米/年。在秦皇岛和塘沽,年潮强度显示出明显的长期下降趋势。在所有四个潮位仪上,风暴潮强度都显示出明显的年际变化和年代际变化。所有四个潮位计均显示出明显的潮-潮相互作用,其潮-潮相互作用的特性因其位置而异,并且未发现明显的长期变化。有说服力的证据表明,在1980年至2016年的过去几十年中,所有潮汐标尺的极端海平面都在增加,增长率在不同的百分位上有所不同。渤海的极端海平面变化受平均海平面和高潮水平(尤其是后者)的变化影响很大。潮汐变化导致潮汐-潮汐相互作用相对较弱的位置处的极端海平面变化。

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