Impact of current-wave interaction on storm surge simulation : a case study for Hurricane Bob

• Published in: Journal of Geophysical Research: Oceans
• Main Authors: Sun, Yunfang, Chen, Changsheng, Beardsley, Robert C., Xu, Qichun, Qi, Jianhua, Lin, Huichan
• Format: Article in Journal/Newspaper
• Language: English
• Published: John Wiley & Sons 2013
• Subjects: Hydrodynamic modeling; Surface waves and tides; Tsunamis; Storm surges; Arctic
• Online Access: https://hdl.handle.net/1912/6306

Author Posting. © American Geophysical Union, 2013. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Oceans 118 (2013): 2685–2701, doi:10.1002/jgrc.20207. Hurricane Bob moved up the U.S. east coast and crossed over southern New England and the Gulf of Maine [with peak marine winds up to 54 m/s (100 mph)] on 19–20 August 1991, causing significant damage along the coast and shelf. A 3-D fully wave-current-coupled finite-volume community ocean model system was developed and applied to simulate and examine the coastal ocean responses to Hurricane Bob. Results from process study-oriented experiments showed that the impact of wave-current interaction on surge elevation varied in space and time, more significant over the shelf than inside the inner bays. While sea level change along the coast was mainly driven by the water flux controlled by barotropic dynamics and the vertically integrated highest water transports were essentially the same for cases with and without water stratification, the hurricane-induced wave-current interaction could generate strong vertical current shear in the stratified areas, leading to a strong offshore transport near the bottom and vertical turbulent mixing over the continental shelf. Stratification could also result in a significant difference of water currents around islands where the water is not vertically well mixed. This work was supported by the MIT Sea Grant College Program through grant 2012-R/RC-127 and the NOAA NERACOOS Program funds for NECOFS. The development of the FVCOM system has been supported by the NSF Ocean Sciences Division through grants OCE-0234545, OCE-0227679, OCE-0606928, and OCE- 0712903 and the NSF Office of Polar Programs-Arctic Sciences Division through grants ARC0712903, ARC0732084, ARC0804029, and ARC1203393. C.C.’s contribution was also supported by Shanghai Ocean University International Cooperation Program ...