scholarly journals Propagation characteristics of near-inertial waves along the continental shelf in the wake of the 2008 Typhoon Hagupit in the northern South China Sea

2018 ◽  
Vol 94 (4) ◽  
pp. 1293-1311 ◽  
Author(s):  
Wenxiang Ding ◽  
Chujin Liang ◽  
Guanghong Liao ◽  
Junde Li ◽  
Feilong Lin ◽  
...  
2019 ◽  
Vol 18 (5) ◽  
pp. 1013-1021
Author(s):  
Guanlin Wang ◽  
Dawei Li ◽  
Zexun Wei ◽  
Shujiang Li ◽  
Yonggang Wang ◽  
...  

2015 ◽  
Vol 34 (9) ◽  
pp. 35-42 ◽  
Author(s):  
Hongbao Qian ◽  
Xiaodong Huang ◽  
Jiwei Tian ◽  
Wei Zhao

2006 ◽  
Vol 145-146 ◽  
pp. 55-67 ◽  
Author(s):  
W.W.-S. Yim ◽  
G. Huang ◽  
M.R. Fontugne ◽  
R.E. Hale ◽  
M. Paterne ◽  
...  

2018 ◽  
Vol 48 (6) ◽  
pp. 1349-1365 ◽  
Author(s):  
Xiaojiang Zhang ◽  
Xiaodong Huang ◽  
Zhiwei Zhang ◽  
Chun Zhou ◽  
Jiwei Tian ◽  
...  

AbstractSpatiotemporal variations in internal solitary wave (ISW) polarity over the continental shelf of the northern South China Sea (SCS) were examined based on mooring-array observations from October 2013 to June 2014. Depression ISWs were observed at the easternmost mooring, where the water depth is 323 m. Then, they evolved into elevation ISWs at the westernmost mooring, with a depth of 149 m. At the central mooring, with a depth of 250 m, the ISWs generally appeared as depression waves in autumn and spring but were elevation waves in winter. Seasonal variations in stratification caused this seasonality in polarity. On the intraseasonal time scales, anticyclonic eddies can modulate ISW polarity at the central mooring by deepening the thermocline depth for periods of approximately 8 days. During some days in autumn and spring, depression ISWs and ISWs in the process of changing polarity from depression to elevation appeared at time intervals of 10–12 h because of the thermocline deepening caused by internal tides. Isotherm anomalies associated with eddies and internal tides have a more significant contribution to determining the polarity of ISWs than do the background currents. The observational results reported here highlight the impact of multiscale processes on the evolution of ISWs.


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