Upper ocean near-inertial response to the passage of two sequential typhoons in the northwestern South China Sea

被引:11
作者
Ma, Yonggui [1 ]
Zhang, Shuwen [1 ,2 ]
Qi, Yiquan [3 ]
Jing, Zhiyou [4 ]
机构
[1] Guangdong Ocean Univ, Coll Ocean & Meteorol, Zhanjiang 524088, Peoples R China
[2] Qingdao Natl Lab Marine Sci & Technol, Lab Reg Oceanog & Numer Modeling, Qingdao 266237, Shandong, Peoples R China
[3] Hohai Univ, Coll Oceanog, Nanjing 210098, Jiangsu, Peoples R China
[4] Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, Guangzhou 510301, Guangdong, Peoples R China
基金
中国国家自然科学基金;
关键词
Typhoon Nesat; Typhoon Nalgae; Near-inertial waves; Near-inertial kinetic energy; Inertial wave propagation; CHLOROPHYLL-A ENHANCEMENT; INTERNAL WAVES; ENERGY; SHELF; VARIABILITY; GENERATION; EDDIES; SHEAR; WIND;
D O I
10.1007/s11430-018-9292-3
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Fifty-seven days of moored current records are examined, focusing on the sequential passage of Typhoons Nesat and Nalgae separated by 5 days in the northwestern South China Sea. Both typhoons generated strong near-inertial waves (NIW) as detected by a moored array, with the near-inertial velocity to the right of the typhoon path significantly larger than to the left. The estimated vertical phase and group velocities of the NIW induced by Typhoon Nesat are 0.2 cm s(-1) and 0.85 m h(-1), respectively, corresponding to a vertical wavelength of 350 m. Both the vertical phase and group velocities of the NIW induced by Typhoon Nalgae are lower than those of Typhoon Nesat, with the corresponding vertical wavelength only one-half that of Nesat. The threshold values of induced near-inertial kinetic energy (NIKE) of 5 J m(-3) reach water depths of 300 and 200 m for Typhoons Nesat and Nalgae, respectively, illustrating that the NIKE induced by Typhoon Nesat dissipated less with depth. Obvious blueshifts in the induced NIW frequencies are also detected. The frequency of NIW induced by Typhoon Nesat significantly increases at water depths of 100-150 m because of Doppler shifting, but decreases significantly at water depths of 100-150 m for Nalgae because of the greater influence of the background vorticity during the passage of Typhoon Nalgae.
引用
收藏
页码:863 / 871
页数:9
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