首页> 外文期刊>Journal of Waterway, Port, Coastal and Ocean Engineering >Sea-Level Rise Effects on Storm Surge and Nearshore Waves on the Texas Coast: Influence of Landscape and Storm Characteristics
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Sea-Level Rise Effects on Storm Surge and Nearshore Waves on the Texas Coast: Influence of Landscape and Storm Characteristics

机译:海平面上升对德克萨斯州海岸风暴潮和近岸波浪的影响:景观和风暴特征的影响

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Sea-level rise (SLR) estimates vary broadly, but most estimates predict significant increases in sea levels within the next century. Through the use of validated, coupled wave and hydrodynamic models, this study investigates SLR effects on storm surge and nearshore waves, including variation with coastal landscape type and storm characteristics. Both the wave and hydrodynamic models account for bottom friction based on land-use type, so the modeling procedure accounted for SLR-related changes to land cover, in addition to higher mean sea levels. Simulation of storms with similar meteorological characteristics and track but with landfall in the northeastern and southwestern coastal areas allowed examination of how the coastal features influenced the storm surge and wave response to increased sea levels. The simulation results analyzed here demonstrate that the relationship between storm surge and relative SLR (RSLR) varies between geographic region and storm scenario. The increase in an inundated area is linear in the north, and in the south, the inundated area approaches the northern values for similar storms asymptotically. Nearshore wave results indicate, as expected, that larger water depths created by positive RSLR and amplified surge allow larger waves to propagate into inland areas. For the Texas simulations, it was found that an increase in hurricane wind speeds of 25 % is approximately equivalent to a RSLR of 0.5 m in terms of increased area of inundation impact. Because of the complexities of storm-surge dependency on storm strength, track, and local topography, there is no one-size-fits-all response to RSLR descriptive of all locations. Site-specific computer modeling should be used to evaluate the risk facing coastal communities.
机译:海平面上升(SLR)估计值差异很大,但是大多数估计值都预测下一个世纪内海平面将显着增加。通过使用经过验证的耦合波和流体动力学模型,本研究调查了SLR对风暴潮和近岸波浪的影响,包括沿海景观类型和风暴特征的变化。波浪模型和流体动力学模型都考虑了基于土地利用类型的底部摩擦,因此,除了较高的平均海平面外,建模过程还考虑了SLR相关的土地覆盖变化。通过模拟具有相似气象特征和航迹但在东北和西南沿海地区有登陆的风暴,可以检查沿海特征如何影响风暴潮和海浪对海平面上升的响应。此处分析的模拟结果表明,风暴潮和相对SLR(RSLR)之间的关系在地理区域和风暴情景之间有所不同。北部的淹没面积增加是线性的,而在南部,渐近的相似风暴的淹没面积接近北部的值。如预期的那样,近岸海浪结果表明,由正RSLR和放大的浪涌产生的较大水深允许较大的海浪传播到内陆地区。对于得克萨斯州的模拟,发现飓风风速增加25%大约相当于淹没影响面积增加0.5m的RSLR。由于风暴潮依赖于风暴强度,航迹和当地地形的复杂性,因此无法对描述所有位置的RSLR做出千篇一律的回应。应使用特定地点的计算机建模来评估沿海社区面临的风险。

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