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首页> 外文期刊>Journal of Coastal Research: An International Forum for the Littoral Sciences >Modeling of coastal inundation, storm surge, and relative sea-level rise at Naval Station Norfolk, Norfolk, Virginia, U.S.A.
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Modeling of coastal inundation, storm surge, and relative sea-level rise at Naval Station Norfolk, Norfolk, Virginia, U.S.A.

机译:美国弗吉尼亚州诺福克海军基地诺福克海军基地的沿海淹没,风暴潮和相对海平面上升的模型。

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Li, H.; Lin, L., and Burks-Copes, K.A., 2013. Modeling of coastal inundation, storm surge, and relative sea-level rise at Naval Station Norfolk, Norfolk, Virginia, U.S.A. The potential risk and effects of storm-surge damage caused by the combination of hurricane-force waves, tides, and relative sea-level-rise (RSLR) scenarios were examined at the U.S. Naval Station, Norfolk, Virginia. A hydrodynamic and sediment transport modeling system validated with measured water levels from Hurricane Isabel was used to simulate two synthesized storms representing 50-year and 100-year return-period hurricanes, a northeaster, and five future RSLR scenarios to evaluate the combined impacts of inundation on this military installation in the lower Chesapeake Bay. The naval base topography and nearshore water body of Hampton Roads were included in the coastal modeling system (CMS), a suite of surge, circulation, wave, sediment transport, and morphology evolution models. The modeling domain was a rectangular area covering the entire Naval Station Norfolk in the Hampton Roads and the mouths of the James and Elizabeth rivers. A variable-resolution grid system was created with a finer resolution of 10 m in the naval base and a coarser resolution of 300 m in the regions away from the base. The boundary-forcing conditions to the CMS were regional storm surge produced by the ADvanced CIRCulation (ADCIRC),and wave conditions by the Simulating WAve Nearshore (SWAN) model. The CMS calculated the local water-surface elevation and storm-surge inundation for combined RSLR, surge, waves, and wind. Results indicate that synthetic storms would cause extensive inundation of coastal land around the naval base. Approximately 60% of the land would be under water with the 100-year storm for the present sea level, and 80% for estimated RSLR of 2 m.
机译:李华; Lin,L.和Burks-Copes,KA,2013年。美国弗吉尼亚州诺福克海军基地海军淹没,风暴潮和相对海平面上升的建模风暴潮造成的潜在风险和影响在弗吉尼亚州诺福克的美国海军站对飓风波,潮汐和相对海平面上升(RSLR)情景的组合进行了检查。使用经伊莎贝尔飓风测得的水动力和泥沙输送模型系统进行了验证,该系统用于模拟代表50年和100年返回期飓风的两次合成风暴,一场东北暴风雨和五个未来RSLR情景,以评估淹没的综合影响在切萨皮克湾下游的军事设施上。汉普顿路的海军基础地形和近岸水体已包括在海岸建模系统(CMS)中,该系统是一套浪涌,环流,波浪,沉积物传输和形态演化模型。建模区域是一个矩形区域,覆盖了汉普顿路的整个海军诺福克海军基地以及詹姆斯河和伊丽莎白河的河口。创建了一个可变分辨率的网格系统,在海军基地中分辨率更高,分辨率为10 m,而在远离基地的区域中分辨率更高,分辨率为300 m。 CMS的强迫边界条件是由先进的环流(ADCIRC)产生的区域风暴潮,以及由模拟波近岸(SWAN)模型产生的波浪条件。 CMS针对RSLR,潮汐,波浪和风的组合计算了局部水面高度和风暴潮的淹没。结果表明,人造风暴将导致海军基地周围的沿海土地被大量淹没。就目前的海平面而言,在100年的暴风雨中,大约60%的土地将处于水下,而对于估计为2m的RSLR,将有80%的土地处于水下。

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