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Stokes drift
Transport Due to Transient Progressive Waves of Small As Well As of Large Amplitude
Arxiv:2002.03434V3 [Physics.Flu-Dyn] 25 Jul 2020
The Stokes Drift in Ocean Surface Drift Prediction
Part II-1 Water Wave Mechanics
Stokes Drift and Net Transport for Two-Dimensional Wave Groups in Deep Water
Final Program
Stokes' Drift of Linear Defects
Calculating Stokes Drift: Problem!!! Stokes Drift Can Be Calculated a Number of Ways, Depending on the Specific Wave Parameters Available
Impacts of Surface Gravity Waves on a Tidal Front: a Coupled Model Perspective
Dissipative Solitons, Wave Asymmetry and Dynamical Ratchets
1470 Ghaffari Materie.Pdf (6.362Mb)
Salinity and Tides in Alluvial Estuaries
Quantification of Stokes Drift As a Mechanism for Surface Oil Advection in the Gulf of Mexico During the Deepwater Horizon Oil Spill Matthew Clark
The Three-Dimensional Current and Surface Wave Equations
Title a New Approach to Stokes Wave Theory Author(S) TSUCHIYA
Steep Progressive Waves in Deep and Shallow Water
The Relationship of Near-Surface Flow, Stokes Drift and the Wind Stress
Challenges for Sustained Observing and Forecasting Systems in the Mediterranean Sea
Top View
Upslope Internal-Wave Stokes Drift, and Compensating Downslope Eulerian Mean Currents, Observed Above a Lakebed
Answers on the Comments of Reviewer 2 of the Paper
The Lagrange Form of the Nonlinear Schrödinger Equation for Low-Vorticity Waves in Deep Water: Rogue Wave Aspect” by Anatoly Abrashkin and Efim Pelinovsky
A Reanalysis of the October 2016 ``Meteotsunami
The Absence of Stokes Drift in Waves
Stokes Drift for Random Gravity Waves
Approximate Stokes Drift Profiles in Deep Water
Fundamentals of Geophysical Fluid Dynamics
CMEMS MED-MFC and the Downscaling MONGOOS Effort
A Tsunami in Lisbon Engenharia Civil
Downloaded 10/01/21 10:23 PM UTC 1314 JOURNAL of PHYSICAL OCEANOGRAPHY VOLUME 42
Lagrangian and Tracer Evolution in the Vicinity of an Unstable Jet
The Role of Ekman Currents, Geostrophy, and Stokes Drift in The
Project Final Report
ATOC5051-Lecture10.Pdf
The Role of Stokes Drift in the Dispersal of North Atlantic Surface Marine Debris
Waves in the Ocean in This Document We Will Discuss Three Types of Waves: Wind-Driven Waves, Tides and Tsunamis
Tsunami and Coastal Disaster Risk Management in Indonesia
Lateral Stirring in the Ocean on Scales of 0.1-10 Km: the Role of Internal Waves
Two-Dimensional Computations of Stokes Drift and Undertow at The
Hydrodynamics of Western Lake Erie During a Major Harmful Algal Bloom Event
Finite Amplitude Ocean Waves Waves with Peaked Crests and Broad Troughs
Lectures on “Introduction to Geophysical Fluid Dynamics” Pavel Berloff
Tidal Rectification and Stokes Drift
Influence of Tidal Current, Wind, and Wave in Hebei Spirit Oil Spill
The Role of River Flow and Tidal Asymmetry on 1-D Estuarine
Wave-Flow Interactions and Acoustic Streaming
On the Coupling of Wave and Three-Dimensional Circulation Models
Stokes Drift in Internal Equatorial Kelvin Waves: Continuous Stratification Versus Two-Layer Models
Concepts from Linear Theory
Wave Model and Wave Drift Caused by the Asymmetry of Crest and Trough
CEM Part II: Chapter 1 Water Wave Mechanics
A Stokes Drift Approximation Based on the Phillips Spectrum Arxiv:1601.08092V2 [Physics.Ao-Ph] 1 Feb 2016
A Cnoidal Approximation Wave Theory
Oceanography Chapter 10 Waves – Disturbances Caused by the Movement of Energy from a Source Through Some Medium. Floating Gull
Stokes Drift in Internal Equatorial Kelvin Waves: Continuous Stratification Versus Two-Layer Models
CHAPTER 45 Particle Velocity Distribution in Surface Waves Geir
EAS/BIOEE 154 Lecture 12 Introduction to Oceanography Waves Fundamental Principles Ideally, Waves Represent a Propagation of Energy, Not Matter
Observations and a Model of Undertow Over the Inner Continental Shelf Steven J
SOL Solitons