Upper ocean near-inertial response to 1998 Typhoon Faith in the South China Sea

被引：22

作者：

Sun Lu ^{[1
,2
]}

Zheng Quan'an ^{[3
]}

Tang Tswen-Yung ^{[4
]}

Chuang Wen-Ssn ^{[4
]}

Li Li ^{[5
]}

Hu Jianyu ^{[6
]}

Wang Dongxiao ^{[1
]}

机构：

[1] Chinese Acad Sci, State Key Lab Trop Oceanog, S China Sea Inst Oceanog, Guangzhou 510301, Guangdong, Peoples R China

[2] State Ocean Adm, S China Sea Environm Monitoring Ctr, S China Sea Branch, Guangzhou 510300, Guangdong, Peoples R China

[3] Univ Maryland, Dept Atmospher & Ocean Sci, College Pk, MD 20742 USA

[4] Natl Taiwan Univ, Inst Oceanog, Taipei 100, Taiwan

[5] State Ocean Adm, Inst Oceanog 3, Xiamen 361005, Peoples R China

[6] Xiamen Univ, State Key Lab Marine Environm Sci, Xiamen 361005, Peoples R China

来源：

ACTA OCEANOLOGICA SINICA | 2012年 / 31卷 / 02期

基金：

中国国家自然科学基金; 美国国家科学基金会;

关键词：

near-inertial oscillation; Typhoon Faith; mooring buoy; South China Sea; HURRICANE; STORMS; WAVES;

D O I：

10.1007/s13131-012-0189-9

中图分类号：

P7 [海洋学];

学科分类号：

0707 ;

摘要：

During the South China Sea monsoon experiment (SCSMEX), three autonomous temperature line acquisition system (ATLAS) buoys with acoustic Doppler current profiler (ADCP) were moored in the South China Sea to measure temperature, salinity and current velocity. Typhoon Faith passed through about 250 km south to one of the mooring buoys located at 12 degrees 58.5'N, 114 degrees 24.5'E from December 11 to 14, 1998. The data, analysis indicates that the typhoon winds induce a great increase in the kinetic energy at near-inertial frequencies with two maxima in the mixed layer and thermocline. The near-inertial oscillations were observed at the upper 270 m in the wake of Typhoon Faith. The oscillations were originally excited in the sea surface layer and propagated downward. The amplitudes of the oscillations decrease with depth except in the thermocline. The near-inertial oscillation signals are also remarkable in temperature and salinity fields.

引用

页码：25 / 32

页数：8

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