1. The Subsurface Mode Tropical Instability Waves in the Equatorial Pacific Ocean and Their Impacts on Shear and Mixing
- Author
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Chuanyu Liu, Zhiyu Liu, Liyuan Fang, William D. Smyth, Fan Wang, and Armin Köhl
- Subjects
010504 meteorology & atmospheric sciences ,Baroclinity ,Equator ,Tropical instability waves ,010502 geochemistry & geophysics ,Atmospheric sciences ,01 natural sciences ,Pacific ocean ,Geophysics ,Amplitude ,Shear (geology) ,Barotropic fluid ,General Earth and Planetary Sciences ,Mean flow ,Geology ,0105 earth and related environmental sciences - Abstract
The tropical instability waves (TIWs) in the eastern tropical Pacific have generally been considered as surface-intensified structures resembling the first baroclinic mode. Here, we report on the existence of subsurface-intensified TIWs on the equator. These TIWs are primarily manifested in zonal velocities, inducing maximum velocity oscillations at 70-90 m depth with amplitudes of 0.1-0.2 m/s and periods of 5-20 days. They account for similar to 20% of the variance at 5- to 30-day periods, with another similar to 50% being contributed by the surface-intensified TIWs. These waves are most significant during the TIW seasons; they are energized in part by barotropic instabilities and usually last for 3-7 months. Via interacting with the mean flow, they can induce strong out-of-phase shear changes between similar to 50-m depth and just above the Equatorial Undercurrent core and may lead to complex diapycnal mixing structures. Their horizontal structures, generation mechanism(s), and large-scale impacts remain to be disclosed.
- Published
- 2019