A Coupled Circulation-Wave Model for Numerical Simulation of Storm Tides and Waves

被引:34
作者
Marsooli, Reza [1 ,3 ]
Orton, Philip M. [1 ]
Mellor, George [2 ]
Georgas, Nickitas [1 ]
Blumberg, Alan F. [1 ]
机构
[1] Stevens Inst Technol, Davidson Lab, Hoboken, NJ 07030 USA
[2] Princeton Univ, Program Atmospher & Ocean Sci, Princeton, NJ 08544 USA
[3] Princeton Univ, Dept Civil & Environm Engn, Princeton, NJ 08544 USA
基金
美国国家科学基金会;
关键词
3-DIMENSIONAL HYDRODYNAMIC MODEL; RADIATION STRESSES; COASTAL; OCEAN; SURFACE; WIND; SYSTEM; MITIGATION; PREDICTION; TURBULENCE;
D O I
10.1175/JTECH-D-17-0005.1
中图分类号
P75 [海洋工程];
学科分类号
0814 ; 081505 ; 0824 ; 082401 ;
摘要
The Stevens Institute of Technology Estuarine and Coastal Ocean Model (sECOM) is coupled here with the Mellor-Donelan-Oey (MDO) wave model to simulate coastal flooding due to storm tides and waves. sECOM is the three-dimensional (3D) circulation model used in the New York Harbor Observing and Prediction System (NYHOPS). The MDO wave model is a computationally cost-effective spectral wave model suitable for coupling with 3D circulation models. The coupled sECOM-MDO model takes into account wave-current interactions through wave-enhanced water surface roughness and wind stress, wave-current bottom stress, and depth-dependent wave radiation stress. The model results are compared with existing laboratory measurements and the field data collected in New York-New Jersey (NY-NJ) harbor during Hurricane Sandy. Comparisons between the model results and laboratory measurements demonstrate the capabilities of the model to accurately simulate wave characteristics, wave-induced water elevation, and undertow current. The model results for Hurricane Sandy reveal the successful performance of sECOM-MDO in situations where high waves and storm tides coexist. The results indicate that the temporal maximum wave setup in NY-NJ harbor was 0.26 m. On the other hand, the contribution of wave setup to the peak storm tide was 0.13 m, a contribution of only 3.8%. It is found that the inclusion of wave radiation stress and wave-enhanced bottom friction in the circulation model can reduce the errors in the calculated storm tides. At the Battery (New York), for example, the root-mean-square error reduced from 0.17 to 0.12 m.
引用
收藏
页码:1449 / 1467
页数:19
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