Second-Mode Internal Tides in the East China Sea Deduced from Historical Hydrocasts and a Model
Abstract
From historical hydrocasts in the Okinawa Trough region of the East China Sea (ECS), acoustic echo time from 700 dbar to the surface shows a tight relationship with temperature (T) except near the 100-200-dbar layer. This is caused by 2nd- or higher-mode baroclinic variations. Significant out-of-phase correlation between upper and lower layer T from the hydrocasts confirms that 2nd-mode variations are strong. Furthermore, the 2nd-mode variations are dominant during the ebb tide period, which suggests they are caused by 2nd-mode internal tides (ITs) generated at the continental shelf break. For comparison, we investigate historical hydrocasts southeast of the Ryukyu Islands, where no significant 2nd-mode variations are found. A model simulating the Mu2 IT agrees qualitatively with these observations: it predicts relatively strong 2nd-mode IT energy in the ECS, but weak energy in the region southeast of the Ryukyu Islands.
Document Details
- Document Type
- Technical Report
- Publication Date
- Mar 16, 2005
- Accession Number
- ADA455205
Entities
People
- D. R. Watts
- Jae-Hun Park
- Magdalena Andres
- Mark Wimbush
- Paul J. Martin
Organizations
- United States Naval Research Laboratory