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Spatial distribution of wave attenuation service of coastal wetlands: A case study of Chongming Island,Shanghai, China

机译:沿海湿地波衰减服务的空间分布 - 以崇明岛,中国上海崇明岛

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Global coastal zone is faced with the challenge of increasing threats from sea level rise ' coastal erosion and storm surge as the result of climate change. To improve the adaptability of the coastal area to climate change' many scientists proposed to incorporate wetlands wave attenuation service into conventional coastal protection schemes ' despite the knowledge gap of the spatial distribution of such service. In this study' we incorporated an exponential wave propagation model into GIS' and simulated the spatial distribution of the wave attenuation service of the coastal wetlands in Chongming island' Yangtze Estuary' under two normal scenarios (spring rise and neap rise). The results showed that coastal wetlands could reduce average significant wave heights up to 0.94 m and 0.54 ni' accounting for 83.6% and 60.4% of their incoming wave heights under spring rise and neap rise' respectively. In either case' wave height reduced by the wetlands on the southern coast of Chongming island was lower than that on the northern coast. The spatial characteristics of wave attenuation rate was similar to that of the reduced wave height under neap rise. Compared to the neap rise scenario, wave attenuation rate of the wetlands along the southern coast of Chongming island showed a significant improvement under spring rise. The spatial heterogeneity of the wave attenuation service can be explained by the spatial patterns of coastal physical and biotic factors as well as their interactions. Not the whole transects of vegetation contributed to wave attenuation, even under spring rise scenario. Only a part of the transects, 70.8% in average, were engaged in wave attenuation under spring rise. This result indicates that the increased height of tide and wave may not induce the corresponding proportion increase in the width of ecosystem involved in dissipating waves due to the nonlinear feature of ecosystems' wave attenuation service in space. This study can provide important support for coastal wetland restoration, ecosystem-based coastal management, and natural capital accounting.
机译:全球沿海地区面临着越来越多的海平面上升“沿海侵蚀和风暴浪涌因气候变化而增加的挑战”。为了提高沿海地区对气候变化的适应性“许多科学家建议将湿地波衰减服务纳入传统的沿海保护方案”尽管这种服务的空间分布的知识差距。在这项研究中,“我们将指数波传播模型纳入GIS”并模拟了在两种正常情况下崇明岛“长江河口”沿海湿地波浪衰减服务的空间分布(弹簧上升和Neap上升)。结果表明,沿海湿地可以将平均显着波浪高度降低至0.94米,0.54米,分别在弹簧上升和Neap上升下的83.6%和60.4%的60.4%。在任何案例中,崇明岛南部海岸的湿地减少了低于北部海岸的湿地。波衰减率的空间特性与NeAP升高下的波浪高的空间特性类似。与Neap崛起的情景相比,崇明岛南部海岸湿地的波浪衰减率在春度上升下显着改善。波衰减服务的空间异质性可以通过沿海物理和生物因子的空间模式以及它们的相互作用来解释。不是植被的整个横断面导致波浪衰减,即使在春季上升场景下也是如此。只有一部分横断面,平均水平70.8%,在弹簧上升下从波衰减。该结果表明,由于空间中的生态系统波衰减服务的非线性特征,潮汐和波的增加的潮汐和波的高度可能不会引起所涉及的生态系统宽度的相应比例增加。本研究可以为沿海湿地修复,生态系统的沿海管理和自然资本核算提供重要支持。

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    《Oceanographic Literature Review》 |2021年第5期|1121-1122|共2页
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  • 入库时间 2022-08-19 02:27:32

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