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Keynote Lecture Series Archive

Fall, 2025

Formation and Evolution of Turbulence in Convectively Unstable Internal Solitary Waves of Depression Shoaling over Gentle Slopes in the South China Sea

Peter Diamessis

Professor
School of Civil and Environmental Engineering
Cornell University
Ithaca, NY

The shoaling of high-amplitude Internal Solitary Waves (ISWs) of depression in the South China Sea (SCS) is examined through large-scale parallel turbulence-resolving high-accuracy/resolution simulations. A select, near-isobath-normal, bathymetric transect of the gentle SCS continental slope is employed together with stratification and current profiles obtained by in-situ measurements. Three simulations of separate ISWs with initial deep-water amplitudes in the range [136m, 150m] leverage a novel wave-tracking capability for a propagation distance of 80km and accurately reproduce key features of in-situ-observed phenomena with significantly higher spatiotemporal resolution. The interplay between convective and shear instability and the associated turbulence formation and evolution are further studied, as a function of deep-water ISW amplitude, in-part revealing processes previously not observed in the field. Across all three waves, the convective instability develops in a similar fashion: heavier water entrained from the wave rear plunges into its interior, giving rise to transient, yet distinct, subsurface vortical structures which transition to turbulence. Ultimately, a gravity current is triggered which horizontally advances through the wave interior and mixes it down to the pycnocline base. Although the waveform remains distinctly symmetric, Kelvin-Helmholtz billows emerge near the well-mixed ISW trough, disturb the wave’s trailing edge and give rise to an active wake. The wake's perturbation kinetic energy is nonlinearly dependent on deep-water wave amplitude and can become a sizable fraction of the kinetic energy of the deep-water ISW, suggesting the wake is a primary mechanism of water column mixing. The talk will conclude with potential interpretations on the origins of the above gravity current as a form of frontogenesis and the associated challenges of measuring such phenomena in the field.

Peter Diamessis, Professor at Cornell University.Peter Diamessis joined the CEE faculty in January 2006. He received his undergraduate degree in Mechanical Engineering from the National Technical University of Athens (NTUA), Greece in 1995. From 1996 to 2001, he pursued graduate studies at the Mechanical and Aerospace Department (formerly Applied Mechanics and Engineering Sciences Dept.) of the University of California, San Diego. Following completion of his PhD studies, Diamessis became a postdoctoral researcher in the fluid dynamics group at the Aerospace and Mechanical Engineering at the University of Southern California where he focused on the development and implementation of numerically stable spectral multidomain techniques and the numerical investigation of stably stratified turbulent wakes and 2-D instabilities under internal solitary waves. Diamessis's recent and ongoing work involves the continued development of spectral multidomain schemes for more complex flow geometries and the application of element-based techniques to other disciplines such as structural mechanics and soil chemistry. The physically focused component of his efforts consists of the study of high Reynolds number stratified wakes and the evolution of the radiated internal wave field and its interaction with the subsurface region, the investigation 3-D turbulence and resuspension under internal solitary waves, the study of nonlinear effects in internal waves propagating through variable environments and the application of stability analysis to environmental boundary layers.

Friday, December 12, 2025
11:00 AM
Laufer Conference Room, (OHE 406)

 

host: Spedding

Published on August 2nd, 2017Last updated on December 8th, 2025