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开发一个模型来模拟海平面上升和夏威夷火奴鲁鲁涨潮引起的地下水泛滥。

Development of a model to simulate groundwater inundation induced by sea-level rise and high tides in Honolulu, Hawaii.

机构信息

University of Hawai'i at Mānoa, School of Ocean and Earth Science and Technology, Department of Geology and Geophysics, POST Building, Suite 701, 1680 East-West Road, Honolulu, HI 96822, USA.

University of Hawai'i at Mānoa, School of Ocean and Earth Science and Technology, Department of Geology and Geophysics, POST Building, Suite 701, 1680 East-West Road, Honolulu, HI 96822, USA.

出版信息

Water Res. 2017 May 1;114:122-134. doi: 10.1016/j.watres.2017.02.035. Epub 2017 Feb 20.

Abstract

Many of the world's largest cities face risk of sea-level rise (SLR) induced flooding owing to their limited elevations and proximities to the coastline. Within this century, global mean sea level is expected to reach magnitudes that will exceed the ground elevation of some built infrastructure. The concurrent rise of coastal groundwater will produce additional sources of inundation resulting from narrowing and loss of the vertical unsaturated subsurface space. This has implications for the dense network of buried and low-lying infrastructure that exists across urban coastal zones. Here, we describe a modeling approach that simulates narrowing of the unsaturated space and groundwater inundation (GWI) generated by SLR-induced lifting of coastal groundwater. The methodology combines terrain modeling, groundwater monitoring, estimation of tidal influence, and numerical groundwater-flow modeling to simulate future flood scenarios considering user-specified tide stages and magnitudes of SLR. We illustrate the value of the methodology by applying it to the heavily urbanized and low-lying Waikiki area of Honolulu, Hawaii. Results indicate that SLR of nearly 1 m generates GWI across 23% of the 13 km study area, threatening $5 billion of taxable real estate and 48 km of roadway. Analysis of current conditions reveals that 86% of 259 active cesspool sites in the study area are likely inundated. This suggests that cesspool effluent is currently entering coastal groundwater, which not only leads to degradation of coastal environments, but also presents a future threat to public health as GWI would introduce effluent at the ground surface.

摘要

由于海拔较低且靠近海岸线,世界上许多大城市都面临海平面上升(SLR)引发的洪水风险。在本世纪内,全球平均海平面预计将上升到超过一些已建基础设施地面高程的程度。沿海地下水位的同时上升将产生额外的淹没源,原因是垂直非饱和地下空间变窄和丧失。这对城市沿海地区存在的密集的地下和低洼基础设施网络产生影响。在这里,我们描述了一种模拟模型方法,该方法模拟了由于沿海地下水位上升引起的 SLR 导致的不饱和空间变窄和地下水淹没(GWI)。该方法结合了地形建模、地下水监测、潮汐影响估计和数值地下水流动建模,以模拟考虑用户指定潮汐阶段和 SLR 幅度的未来洪水情景。我们通过将其应用于高度城市化和地势低洼的夏威夷火奴鲁鲁的怀基基地区来证明该方法的价值。结果表明,海平面上升近 1 米会导致整个 13 公里研究区域 23%的地区发生 GWI,威胁到价值 50 亿美元的应税房地产和 48 公里的道路。对现状的分析表明,研究区域内 259 个活跃的污水池中有 86%可能被淹没。这表明污水池中的污水目前正在进入沿海地下水,这不仅导致沿海环境恶化,而且随着 GWI 将污水引入地面,还对公共健康构成未来威胁。

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