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Variability of internal tides and near‐inertial waves on the continental slope of the northwestern South China Sea
Author(s) -
Xu Zhenhua,
Yin Baoshu,
Hou Yijun,
Xu Yongsheng
Publication year - 2013
Publication title -
journal of geophysical research: oceans
Language(s) - English
Resource type - Journals
eISSN - 2169-9291
pISSN - 2169-9275
DOI - 10.1029/2012jc008212
Subject(s) - internal wave , geology , typhoon , continental shelf , stratification (seeds) , atmospheric sciences , mode (computer interface) , internal tide , climatology , oceanography , seed dormancy , botany , germination , dormancy , computer science , biology , operating system
Structure and variability of internal tides (IT) and near‐inertial waves (NIW) on the continental slope of the northwestern South China Sea were investigated, based on 9‐month moored current observations from autumn to early summer in 2008 and 2009. The diurnal IT kinetic energy, dominant over that of semidiurnal tides, is found to exhibit apparent seasonal variability—strongest in summer and weakest in winter—whereas the semidiurnal variance remained nearly uniform throughout the observation period. Moreover, the diurnal IT were more coherent (i.e., phase‐locked to the astronomical forcing) than the semidiurnal constituents. Coherent diurnal variance accounts for about 40% of diurnal motions, but semidiurnal tides contain a much smaller fraction (10%) of coherent motions. Further analysis demonstrates that the diurnal IT are dominated by the first mode, whereas the semidiurnal tides show a variable multimodal structure: the second mode is dominant in summer and comparable to the first mode in spring and autumn, but the first mode predominates in winter. Multimodal semidiurnal IT are more influenced by varying stratification structures and background currents and thus exhibit highly incoherent and intermittent behavior, which may wash out seasonal variability during their long propagation from the generation source. The observed NIW are seasonally independent and comparable to the semidiurnal motions. During the passage of Typhoon Hagupit, however, the NIW became the most energetic component of the inertia‐gravity waveband motions. NIW energy and shear were significantly enhanced and exceeded tidal counterparts by a factor of 2 to 3 in the upper layer.