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Critical storm thresholds for morphological changes in the western Black Sea coastal zone

机译:黑海西部沿海地区形态变化的关键风暴阈值

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Storms are one of the phenomena determining the short-term evolution of coasts by influencing the erosion and accretion patterns of the beaches. Some severe storms could cause loss of beach sediments, partial or complete destruction of coastal structures and even threaten human life and occupation. Bearing this in mind, it is essential to comprehend, which storms could evoke transient, although in some instances, significant morphological changes, and which could be considered as hazardous and result in catastrophic damage. This issue implies establishment of a set of critical thresholds for storm impact on coastal morphology. The paper presents a regional scale analysis of the near-shore morphological response of five beaches to storms of varying intensity. The analysis is accomplished by coupling of offshore wave and cross-shore profile data obtained for the Bulgarian Black sea coast. The historical storm pattern is reconstructed through hindcast using a coupled wave model system, while resulting morphological changes, such as shoreline alteration and cross-shore profile evolution, are estimated by analysis of long-term series of coastal measurements performed in 1970-1977 and 2008-2010. The storm impact thresholds are set in terms of integral wave energy taking into account both storm pattern and duration. It was found that the morphological response to storm impact is site specific and single-value thresholds are difficult to be established even at regional scale. Nevertheless, a range of critical storm thresholds is proposed. Thus, storms with integral wave energy varying within threshold values 0.4-0.7 × 10~6 J m~(-2) are regarded as capable of significant morphological changes, while less energetic events are supposed to influence predominately the seasonal beach dynamics. Furthermore, storms with integral wave energy higher than 0.7 × 10~6 J m~(-2) represent potentially destructive events that can change irreversibly the beach pattern or damage impact.
机译:暴风雨是通过影响海滩的侵蚀和增生方式而决定海岸短期演变的现象之一。一些严重的风暴可能导致海滩沉积物的损失,沿海结构的部分或全部破坏,甚至威胁到人类的生命和职业。牢记这一点,必须理解,哪些风暴可能会引起短暂的变化,尽管在某些情况下会引起重大的形态变化,并且可以认为这是危险的并导致灾难性破坏。这个问题意味着要建立一套暴风雨对沿海形态影响的关键阈值。本文对五个海滩对不同强度风暴的近岸形态响应进行了区域尺度分析。该分析是通过结合从保加利亚黑海沿岸获得的离岸波和跨岸剖面数据来完成的。通过使用耦合波模型系统通过后播来重建历史风暴模式,同时通过对1970-1977年和2008年进行的长期沿海测量的分析来估计由此产生的形态变化,例如海岸线变化和跨岸剖面演变。 -2010。风暴影响阈值是根据积分波能量设置的,同时考虑了风暴模式和持续时间。发现对风暴影响的形态响应是针对特定地点的,即使在区域范围内也难以建立单值阈值。然而,提出了一系列的暴风雨临界阈值。因此,积分波能量在阈值0.4-0.7×10〜6 J m〜(-2)范围内变化的风暴被认为具有明显的形态变化能力,而较少的高能事件则主要影响季节性海滩动力学。此外,积分波能量高于0.7×10〜6 J m〜(-2)的风暴代表着潜在的破坏性事件,可以不可逆转地改变海滩模式或破坏影响。

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