Standing wave modes observed in the South China Sea deep basin. Issue 7 (8th July 2014)

• Record Type: Journal Article
• Authors: Zheng, Quanan; Hu, Jianyu; Zhu, Benlu; Feng, Ying; Jo, Young‐Heon; Sun, Zhenyu; Zhu, Jia; Lin, Hongyang; Li, Junyi; Xu, Ying
• Is Part Of: Journal of geophysical research. Volume 119:Issue 7(2014:Jul.)
• Page Start: 4185
• Page End: 4199
• Publication Date: 2014-07-08
• Subjects: Oceanography -- Periodicals; 551.4605
• DOI: 10.1002/2014JC009957
• Languages: English
• ISSNs: 2169-9275

Abstract

<abstract abstract-type="main"> <title>Abstract</title> <p>This study deals with standing wave or seiche events using cruise observations, satellite altimeter data, and theoretical analysis. Cruise missions in summer 2007 and 2009 detected internal oscillation signals in the South China Sea (SCS) deep basin. The signals have average wavelengths of 320 and 390 km and the maximum amplitudes of 50–100 m at layers 500–700 m and 1500–1700 m. Satellite altimeter sea level anomaly (SLA) images and the second intrinsic mode function (IMF2) images derived from the empirical mode decomposition (EMD) analysis show that the observed internal oscillations are a portion of 2‐D seiche modes, which lasted for at least 2 weeks. We recognize that the observed internal oscillation signals represent seiche modes <italic>H</italic><sub>5, 3</sub> and <italic>H</italic><sub>5, 1</sub> derived from a rectangular model ocean basin with a uniform depth, a west‐east length of 1000 km and a north‐south width of 800 km. Statistical analysis of standing wave modes <italic>H</italic><sub>4, 0</sub>, <italic>H</italic><sub>5, 1</sub>, and <italic>H</italic><sub>5, 3</sub> with the average wavelength of 500, 390, and 320 km indicates that from 1993 to 2012 (1045 weeks), total 94 events with total temporal coverage of 218 weeks are affirmed. The total occurrence frequency is 20.9%. Histograms of annual distributions of seiche events and timespans show an interannual variability of about 9 years, with peak years 1993, 1994, 1998, 2001, and 2011. While monthly distributions show an intraseasonal variability double‐peaked in May and October, transit periods of East Asia monsoon in the SCS.</p> </abstract>