Volume 9 Issue 1
Jan.  2016
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Dong-mei Xie, Qing-ping Zou, John W. Cannon. 2016: Application of SWAN+ADCIRC to tide-surge and wave simulation in Gulf of Maine during Patriot’s Day storm. Water Science and Engineering, 9(1): 33-41. doi: 10.1016/j.wse.2016.02.003
Citation: Dong-mei Xie, Qing-ping Zou, John W. Cannon. 2016: Application of SWAN+ADCIRC to tide-surge and wave simulation in Gulf of Maine during Patriot’s Day storm. Water Science and Engineering, 9(1): 33-41. doi: 10.1016/j.wse.2016.02.003

Application of SWAN+ADCIRC to tide-surge and wave simulation in Gulf of Maine during Patriot’s Day storm

doi: 10.1016/j.wse.2016.02.003
Funds:  This work was supported by the Maine Sea Grant and National Oceanic and Atmospheric Administration (Grant No. NA10OAR4170072), and the Ensemble Estimation of Flood Risk in a Changing Climate (EFRaCC) project funded by the British Council under its Global Innovation Initiative.
  • Received Date: 2015-06-23
  • Rev Recd Date: 2015-11-12
  • The southern coast of the Gulf of Maine in the United States is prone to flooding caused by nor’easters. A state-of-the-art fully-coupled model, the Simulating WAves Nearshore (SWAN) model with unstructured grids and the ADvanced CIRCulation (ADCIRC) model, was used to study the hydrodynamic response in the Gulf of Maine during the Patriot’s Day storm of 2007, a notable example of nor’easters in this area. The model predictions agree well with the observed tide-surges and waves during this storm event. Waves and circulation in the Gulf of Maine were analyzed. The Georges Bank plays an important role in dissipating wave energy through the bottom friction when waves propagate over the bank from offshore to the inner gulf due to its shallow bathymetry. Wave energy dissipation results in decreasing significant wave height (SWH) in the cross-bank direction and wave radiation stress gradient, which in turn induces changes in currents. While the tidal currents are dominant over the Georges Bank and in the Bay of Fundy, the residual currents generated by the meteorological forcing and waves are significant over the Georges Bank and in the coastal area and can reach 0.3 m/s and 0.2 m/s, respectively. In the vicinity of the coast, the longshore current generated by the surface wind stress and wave radiation stress acting parallel to the coastline is inversely proportional to the water depth and will eventually be limited by the bottom friction. The storm surge level reaches 0.8 m along the western periphery of the Gulf of Maine while the wave set-up due to radiation stress variation reaches 0.2 m. Therefore, it is significant to coastal flooding.

     

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