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

    Source: Journal of Atmospheric and Oceanic Technology:;2017:;volume( 034 ):;issue: 007::page 1449
    Author:
    Marsooli, Reza;Orton, Philip M.;Mellor, George;Georgas, Nickitas;Blumberg, Alan F.
    DOI: 10.1175/JTECH-D-17-0005.1;AbstractThe 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-dime
    Publisher: American Meteorological Society
    Abstract: AbstractThe 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.
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      A Coupled Circulation–Wave Model for Numerical Simulation of Storm Tides and Waves

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    contributor authorMarsooli, Reza;Orton, Philip M.;Mellor, George;Georgas, Nickitas;Blumberg, Alan F.
    date accessioned2018-01-03T10:59:53Z
    date available2018-01-03T10:59:53Z
    date copyright4/7/2017 12:00:00 AM
    date issued2017
    identifier otherjtech-d-17-0005.1.pdf
    identifier urihttp://138.201.223.254:8080/yetl1/handle/yetl/4245835
    description abstractAbstractThe 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.
    publisherAmerican Meteorological Society
    titleA Coupled Circulation–Wave Model for Numerical Simulation of Storm Tides and Waves
    typeJournal Paper
    journal volume34
    journal issue7
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/JTECH-D-17-0005.1;AbstractThe 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-dime
    journal fristpage1449
    journal lastpage1467
    treeJournal of Atmospheric and Oceanic Technology:;2017:;volume( 034 ):;issue: 007
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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