Key research themes
1. How can ship responses be used to estimate directional wave spectra and improve wave monitoring coverage?
This research area focuses on utilizing measured ship responses, such as motions and structural loads, to estimate the directional wave spectrum at the ship's location. Such methods offer potentially extensive spatio-temporal wave data coverage by transforming operating ships into moving wave buoys, complementing traditional fixed buoy, satellite, and radar measurements. The theme explores physics-based, data-driven, and hybrid approaches to improve wave estimation accuracy, robustness to operational uncertainties, and real-time applicability, thereby enriching wave monitoring networks and aiding operational performance optimization.
2. What are the dynamics and impacts of ship-generated waves in shallow and coastal waters?
This research theme investigates the characteristics, generation mechanisms, and environmental consequences of waves created by ship movements in shallow water environments such as channels, fjords, and tidal flats. It covers wave hydrodynamics near hulls, wave transformation and propagation in depth-limited domains, interaction with coastal morphology, and resulting sediment mobilization and erosion. The research spans experimental measurements, advanced numerical modeling including nonlinear and dispersive effects, and practical implications for sustainable navigation management and coastal ecosystem preservation.
3. What physical mechanisms govern the generation and statistical properties of extreme and rogue waves at sea?
This theme explores the origins and dynamics of rogue waves, focusing on nonlinear wave interactions and statistical signatures in the open ocean. It critically evaluates competing theories such as third-order quasi-resonant wave-wave modulational instabilities and second-order bound nonlinearities enhanced constructive interference. The theme includes analysis of field measurements, wave spectral modeling, and theoretical frameworks to discern which mechanisms dominate rogue wave formation in realistic multi-directional sea states and how these extremes fit within weakly nonlinear random wave statistics.