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Edge wave
Meteotsunami Generation, Amplification and Occurrence in North-West Europe
Destructive Meteotsunamis Along the Eastern Adriatic Coast: Overview
A High-Amplitude Atmospheric Inertia–Gravity Wave-Induced
Infragravity Wave Energy Partitioning in the Surf Zone in Response to Wind-Sea and Swell Forcing
Baroclinic Instability, Lecture 19
Edge Waves
The Life Cycle of Baroclinic Eddies in a Storm Track Environment
Dtic Eecte Feb 006 1992
Propagation of a Meteotsunami from the Yellow Sea to the Korea Strait in April 2019
Signature Redacted Author
Observations of Infragravity Waves
Causes of Reduced North Atlantic Storm Activity in a CCSM3
Scattering and Trapping of Obliquely Incident, Low-Mode Internal Tides Off a Continental Shelf and Slope
Wind Input Function
Lectures on Dynamical Meteorology
Edge Waves and Beach Cusps
EAPS 53600, Spring 2020 Lec 10: Baroclinic Instability (Vallise 8.4-8.7)
Long Waves and Ocean Tides Around 1940, and Then to Indi- Cate How the Subject Has Developed Since Then, with Myrl C
Top View
Baroclinic Instability
Parametrically Forced Surface Waves
Focusing of Surface Waves by Variable Bathymetry
Probabilistic Characteristics of Narrow-Band Long Wave Run-Up Onshore by Sergey Gurbatov and Efim Pelinovsky
Meteotsunami Project FY18
Evolution Equations for Edge Waves and Shear Waves on Longshore Uniform Beaches
Observations of Surf Beat Forcing and Dissipation Stephen M
Propagation of Tsunami on a Linear Slope Between Two Flat Regions
Chapter 8. Shallow-Water Waves
Stratified Rotating Edge Waves
The Hybrid Kelvin–Edge Wave and Its Role in Tidal Dynamics
D.J. Staziker
1 Basic Hydrodynamic Processes in the Coastal
An Investigation Into Edge-Wave Generation by Wind EGU General Assembly, 19–30 April 2021
Water Waves Near a Shoreline in a Flow with Vorticity: Two Classical Examples
Arxiv:2009.00118V1 [Physics.Flu-Dyn] 31 Aug 2020 Ary Layer, That Is, Νe → 0 Or Cs → ∞, Both the fluid the Negative Sign Refers to the Left-Moving Ones
Edge Waves on the Sydney Coast
Development of a Forecast Process for Meteotsunami Events in the Gulf of Mexico Leilani D
Coastal Seiches
'Edge Waves ﹒ the Differences Between the Full .And Shalloww
Chapter 80 Surf Zone Resonance and Coupled
Meteotsunami Modeling Guidelines
Field Observations of Edge Waves and Their Effect on Beach Material
Rogue Edge Waves in the Ocean
Atmospherically Induced Destructive Ocean Waves in the Tsunami Frequency Band
Addressing the Meteotsunami Risk in the United States
The Counter-Propagating Rossby-Wave Perspective on Baroclinic Instability
Rhythmic Beach Cusp Formation: a Conceptual Synthesis*