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Characterising the relaxation distance of nearshore submarine morphology: A southern Baltic Sea case study

机译:表征近岸海底形态的弛豫距离:波罗的海南部案例研究

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摘要

A method for defining the length of coast with alongshore uniformity of nearshore submarine morphology is required in many shore-normal, nearshore profile modelling approaches. Here, we introduce a new variable, the 'relaxation distance', to describe the alongshore spacing between two adjacent shore-normal profiles characterised by distinct morphologies. Within this distance, alongshore morphological changes are too small to distinguish, so the nearshore submarine morphology is regarded as uniform along the coast. We apply a semi-variogram approach, which expresses decreased spatial correlation of the nearshore submarine morphology with alongshore distance, to quantify relaxation distances. We apply this morphological variable to analyse 225 measured shore-normal submarine profiles at 500 m intervals in three distinct sites of the tideless, wave-dominated southern Baltic coast: Swina, Leba, and Hel. The relaxation distances of these three sites are approximately 4500 m, 3000 m, and 2200 m. Of the three sites, Swina has the smoothest nearshore submarine morphology and the weakest wave energy. The relaxation distances of different quasi-straight segments at each site appear similar but those at different sites decrease with enlarged morphological perturbations, which are residuals resulting from detrending the shore-normal profiles. The standard deviations of these morphological perturbations are correlated with the incidence wave angles and wave energy. We also found that large perturbations (such as longshore bars and channels) have a significant impact on the estimation of underwater volume using shore-normal profile trends. Therefore, relaxation distance can indicate morphological smoothness, the length of shore-parallel uniform nearshore submarine morphology, and the impact of local processes on submarine morphology. (C) 2018 Elsevier B.V. All rights reserved.
机译:许多海岸法线,近岸剖面建模方法都需要一种定义海岸长度和近岸海底形态的近岸均匀性的方法。在这里,我们引入一个新变量“松弛距离”,以描述两个以不同形态表征的相邻海岸法线剖面之间的沿岸间距。在此距离内,沿岸形态变化很小,无法区分,因此近岸海底形态被认为是沿海岸一致的。我们应用半变异函数方法来表达近岸海底形态与沿岸距离的空间相关性降低,以量化松弛距离。我们应用这种形态学变量,分析了波罗的海浪南部波罗的海南部三个不同地点(斯威纳,莱巴和赫尔)的500个间隔处的225个测量的海岸正常海底剖面,间隔500 m。这三个位置的弛豫距离分别约为4500 m,3000 m和2200 m。在这三个地点中,斯威纳州的近海海底形态最平滑,波能最弱。每个地点不同准直线段的弛豫距离看起来相似,但不同地点的弛豫距离随着形态扰动的增大而减小,形态扰动是沿岸法线剖面趋势反趋势产生的残差。这些形态扰动的标准偏差与入射波角和波能量相关。我们还发现,大的扰动(例如,长岸酒吧和航道)对使用海岸正态剖面趋势估计水下体积有重大影响。因此,弛豫距离可以表示形态的平滑度,岸线平行的均匀近岸海底形态的长度以及局部过程对海底形态的影响。 (C)2018 Elsevier B.V.保留所有权利。

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