Ocean response to typhoon Nuri (2008) in western Pacific and South China Sea
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Typhoon Nuri formed on 18 August 2008 in the western North Pacific east of the Philippines and traversed northwestward over the Kuroshio in the Luzon Strait where it intensified to a category 3 typhoon. The storm weakened as it passed over South China Sea (SCS) and made landfall in Hong Kong as a category 1 typhoon on 22 August. Despite the storm’s modest strength, the change in typhoon Nuri’s intensity was unique in that it strongly depended on the upper ocean. This study examines the ocean response to typhoon Nuri using the Princeton Ocean Model. An ocean state accounting for the sea-surface temperature (SST) and mesoscale eddy field prior to Nuri was constructed by assimilating satellite SST and altimetry data 12 days before the storm. The simulation then continued without further data assimilation, so that the ocean response to the strong wind can be used to understand processes. It is found that the SST cooling was biased to the right of the storm’s track due to inertial currents that rotated in the same sense as the wind vector, as has previously been found in the literature. However, despite the comparable wind speeds while the storm was in western Pacific and SCS, the SST cooling was much more intense in SCS. The reason was because in SCS, the surface layer was thinner, the vorticity field of the Kuroshio was cyclonic, and moreover a combination of larger Coriolis frequency as the storm moved northward and the typhoon’s slower translational speed produced a stronger resonance between wind and current, resulting in strong shears and entrainment of cool subsurface waters in the upper ocean.
KeywordsTyphoon Nuri Upper ocean response Inertial currents Resonance between wind and ocean current South China Sea Western North Pacific Ocean Near-inertial internal waves
Comments from the reviewers and editor Dr. Miyazawa improved the manuscript. Part of this work was completed while Jingru Sun conducted her summer research at NCU, Taiwan. LYO is grateful for the award from the Taiwan’s Foundation for the Advancement of Outstanding Scholarship. The research was in part supported by the National Science Council, the Ministry of Education, and the National Central University, Taiwan. Model calculations were conducted on Tsinghua University server Tansuo100 and National Central University ATOP cluster.
- Chang Y-L, Oey L-Y (2014) Instability of the North Pacific subtropical countercurrent. J Phys Oceanogr 44:818–833Google Scholar
- Chiang TL, Wu CR, Oey L-Y (2011) Typhoon Kai-Tak: a perfect ocean’s storm. J Phys Oceanogr 41:221–233Google Scholar
- Csanady, G.T. (1982) Circulation in the coastal ocean. Reidel Publishing Co. 279 ppGoogle Scholar
- Gill AE (1982) Atmosphere–ocean dynamics. Academic Press, 662 ppGoogle Scholar
- Landsea CW (2000) Climate variability of tropical cyclones: past, present and future. In: R. A. Pielke, Sr. and R. A Pielke, Jr (eds) Storms. Routledge, New York, 220–241Google Scholar
- Palmen E (1948) On the formation and structure of tropical cyclones. Geophysics 3:26–38Google Scholar
- Wang D-P, Oey L-Y (2008) Hindcast of Waves and Currents in Hurricane Katrina. Bulletin of the American Meteorological Society (BAMS), April, 487–495Google Scholar