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The effect of wave-induced radiation stress on storm surge during Typhoon Saomai(2006) 被引量:9

The effect of wave-induced radiation stress on storm surge during Typhoon Saomai(2006)
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摘要 The effects of wave-induced radiation stress on storm surge were simulated during Typhoon Saomai using a wave-current coupled model based on ROMS (Regional Ocean Modeling System) ocean model and SWAN (Simulating Waves Nearshore) wave model. The results show that radiation stress can cause both set-up and set-down in the storm surge. Wave-induced set-up near the coast can be explained by decreasing significant wave heights as the waves propagate shoreward in an approximately uniform direction; wave-induced set-down far from the coast can be explained by the waves propagating in an approximately uniform direction with increasing significant wave heights. The shoreward radiation stress is the essential reason for the wave-induced set-up along the coast. The occurrence of set-down can be also explained by the divergence of the radiation stress. The maximum wave-induced set-up occurs on the right side of the Typhoon path, whereas the maximum wave induced set-down occurs on the left side. The effects of wave-induced radiation stress on storm surge were simulated during Typhoon Saomai using a wave-current coupled model based on ROMS (Regional Ocean Modeling System) ocean model and SWAN (Simulating Waves Nearshore) wave model. The results show that radiation stress can cause both set-up and set-down in the storm surge. Wave-induced set-up near the coast can be explained by decreasing significant wave heights as the waves propagate shoreward in an approximately uniform direction; wave-induced set-down far from the coast can be explained by the waves propagating in an approximately uniform direction with increasing significant wave heights. The shoreward radiation stress is the essential reason for the wave-induced set-up along the coast. The occurrence of set-down can be also explained by the divergence of the radiation stress. The maximum wave-induced set-up occurs on the right side of the Typhoon path, whereas the maximum wave induced set-down occurs on the left side.
出处 《Acta Oceanologica Sinica》 SCIE CAS CSCD 2011年第3期20-26,共7页 海洋学报(英文版)
基金 supported by the Special Funding of Marine Science Study State Ocean Administration under contract No.20090513-2 the National Natural Science Foundation of China under contract No.40976008 Innovation Project from the Chinese Academy of Sciences under contract No.KZCX2-EW-209 the Key program of Knowledge Innovation Project of Chinese Academyof Sciences under contract No.KZCX1-YW-12
关键词 radiation stress storm surge wave-current interactions Typhoon Saomai radiation stress, storm surge, wave-current interactions, Typhoon Saomai
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