Development and Implementation of Depth Dependent Wave Forcing and Stokes Drift into Coupled 3D PADCIRC/PUNSWAN Joshua Todd Coastal Engineering Department.

Slides:



Advertisements
Similar presentations
Phoenics User Conference on CFD May 2004 Vipac Engineers & Scientists Ltd COMPUTATIONAL FLUID DYNAMICS Simulation of Turbulent Flows and Pollutant Dispersion.
Advertisements

Scour holes/Scour protection: Effect on wave loads EWEC 2007 MILANO Erik Asp Hansen Erik Damgaard Christensen.
What is Projectile Motion?
Lecture 15: Capillary motion
Continuity Equation. Continuity Equation Continuity Equation Net outflow in x direction.
Basic Governing Differential Equations
Research Lead  The University of North Carolina at Chapel Hill CHC-R 5 th Annual Meeting January 31-February 1,
Update on Hurricane Modeling Scenarios in the Houston Region Using ADCIRC Clint Dawson and Jennifer Proft Casey Dietrich, Nishant Panda, Adnan Muhammad.
The effect of ocean tides on a climate model simulation Ocean Modelling September, 2010 M. Müller, H. Haak, J.H. Jungclaus, J. Sündermann, M. Thomas Erik.
WORKING GROUP 1 MODELING OF WIND WAVES AND SURGE EVENTS IN THE CASPIAN, BLACK, AZOV AND BALTIC SEAS.
Continuum Mechanics General Principles M. Ali Etaati Eindhoven University of Technology Math. & Computer Science Dept. CASA Apr
Fluid Mechanics –For Civil Engineers is all about SMU Storing– Moving– Using ( Incompressible fluids - water) To design and manage these systems we need.
Chapter 3.1 Weakly Nonlinear Wave Theory for Periodic Waves (Stokes Expansion)  Introduction The solution for Stokes waves is valid in deep or intermediate.
Coupling the RCM to LFM Frank Toffoletto (Rice) and John Lyon (Dartmouth)
Ocean surface currents and the Craig-Banner boundary condition Charles Tang Bedford Institute of Oceanography Dartmouth, Nova Scotia, Canada POM for the.
ABSTRACT Many new devices and applications are being created that involve transporting droplets from one place to another. A common method of achieving.
Institute of Oceanogphy Gdańsk University Jan Jędrasik The Hydrodynamic Model of the Southern Baltic Sea.
The Role of Surface Freshwater Flux Boundary Conditions in Arctic Ocean/Sea-Ice Models EGU General Assembly, Nice, April 2004 Matthias Prange and Rüdiger.
Juan Carlos Ortiz Royero Ph.D.
An Assimilating Tidal Model for the Bering Sea Mike Foreman, Josef Cherniawsky, Patrick Cummins Institute of Ocean Sciences, Sidney BC, Canada Outline:
Extratropical Storm-Induced Coastal Inundation: Scituate, MA Robert C. Beardsley 1, Changsheng Chen 2, Qichun Xu 2, Jianhua Qi 2, Huichan Lin 2 2 School.
US IOOS Modeling Testbed Leadership Teleconference May 3, 2011 FVCOM Development Team Robert C. Beardsley and Changsheng Chen
Nobuhito Mori and Junichi Ninomiya Disaster Prevention Research Institute Kyoto University, Japan Collaborators John C. Warner (USGS) Eric D’Asaro (U Washington)
Model overview: A hierarchy of ocean models Jay McCreary Summer School on: Dynamics of the North Indian Ocean National Institute of Oceanography Dona Paula,
Management Unit of the North Sea Mathematical Models MUMM | BMM | UGMM [1][1] MUMM’s Operational Tools and Services for Belgian.
Lecture I of VI (Claudio Piani) Course philosophy, the Navier-Stokes equations, Shallow Water, pressure gradient force, material derivative, continuity,
Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas Physical and Biogeochemical Coupled Modelling.
The Stokes Drift and Mean Flows Induced by Two-Dimensional Internal Gravity Wave Packets Ton van den Bremer 1,2 & Bruce Sutherland 2,3 1. Department of.
SURA Super-Regional Testbed on Coastal Inundation – Extra-tropical Storm Harry V. Wang, Yi-cheng Teng, Yanqiu Meng and Derek Loftis Virginia Institute.
AdcircLite-NC Rapid computation of storm surge and waves for NC coastal waters Brian Blanton Renaissance Computing Institute/UNC Chapel Hill Jesse Bikman,
Prof. dr. A. Achterberg, Astronomical Dept., IMAPP, Radboud Universiteit.
USF FVCOM Tropical Cyclone Inundation Testbed Progress by Robert H. Weisberg, Lianyuan Zheng and Yong Huang College of Marine Science University of South.
Yoon kichul Department of Mechanical Engineering Seoul National University Multi-scale Heat Conduction.
Reynolds Transport Theorem We need to relate time derivative of a property of a system to rate of change of that property within a certain region (C.V.)
The Governing Equations The hydrodynamic model adopted here is the one based on the hydrostatic pressure approximation and the boussinesq approximation,
OCN 5401 Chapter 6 Effect of Earth’s Rotation Instructor: Dr. George A. Maul / X 7453.
Presentation of the paper: An unstructured grid, three- dimensional model based on the shallow water equations Vincenzo Casulli and Roy A. Walters Presentation.
Lecture 6: Open Boundaries Solid wall Open boundary Let us first consider the ocean is incompressible, which satisfies (6.1) H  Integrating (6.1) from.
HEAT TRANSFER FINITE ELEMENT FORMULATION
Investigation of Mixed Layer Depth in the Southern Ocean by using a 1-D mixed layer model Chin-Ying Chien & Kevin Speer Geophysical Fluid Dynamics Institute,
1D Long-term Modelling of Longshore Sediment Transport
MODEL RESPONSE SENSITIVITY TO WAVES, NONLINEAR ADVECTION, AND BOTTOM FRICTION Patrick C. Kerr 17 th ADCIRC WORKSHOP April 29-30, Patrick Corbitt.
Ekman pumping Integrating the continuity equation through the layer:. Assume and let, we have is transport into or out of the bottom of the Ekman layer.
Evaluation of the Real-Time Ocean Forecast System in Florida Atlantic Coastal Waters June 3 to 8, 2007 Matthew D. Grossi Department of Marine & Environmental.
Vibrations and Waves Hooke’s Law Elastic Potential Energy Simple Harmonic Motion.
CHANGSHENG CHEN, HEDONG LIU, And ROBERT C. BEARDSLEY
CMEMS Mediterranean MFC. Update on specific development for CMEMS Med-MFC V2 Analysis and Forecast Product 1.Data Assimilation: Grid point EOFs ( * )
Tropical Report: Modeling Hurricane Ike with SLOSH Don Slinn, Jeff Ren, Go Fujita Univ of Florida Coastal Engineering.
Application of the Continuity Equation Dr. Eyad Abushandi.
AO-FVCOM Development: A System Nested with Global Ocean Models Changsheng Chen University of Massachusetts School of Marine Science, USA
The shallow water equations in geomorphic modeling
Estuarine Hydrodynamics
Modelling of Marine Systems. Shallow waters Equations.
Forecasting Wind Setup in a Coastal Estuary Presenter: Jeff Colvin Steven Lazarus, Michael Splitt, Bryan Holman Robert Weaver, Peyman Taeb, Atoosa Saberi.
MAE 5130: VISCOUS FLOWS Lecture 2: Introductory Concepts
Estuarine Variability
Enhancement of Wind Stress and Hurricane Waves Simulation
The β-spiral Determining absolute velocity from density field
Florida Institute of Technology
What is Projectile Motion?
Mark A. Bourassa and Qi Shi
Virginia Institute of Marine Sciences College of William and Mary
Momentum:.
Conservation of momentum
Kinetic Theory.
Branches of Oceanography
Scattering by free charges
Branches of Oceanography
Kinetic Theory.
Unit 3 - Energy Learning Target 3.2 – Be able to use the equations for Potential Energy & Kinetic Energy.
Presentation transcript:

Development and Implementation of Depth Dependent Wave Forcing and Stokes Drift into Coupled 3D PADCIRC/PUNSWAN Joshua Todd Coastal Engineering Department of Marine and Environmental Systems Florida Institute of Technology Advisor: Dr. Robert Weaver April 29,2013

Objective To modify the three dimensional version of ADCIRC to use wave forcing and mass flux in the calculation of sea surface elevation and current velocities

Background Stokes 1847 – Study of Water Waves Longuet-Higgins and Stewart 1962 – Studied shoreward directed momentum flux by water waves Mellor 2003,2008 – Included wave effects on three dimensional equations of motion in addition to the LHS radiation stress

Modifications Add three dimensional depth dependent radiation stress to the momentum equations Add depth dependent Stoke’s drift to the velocity solution

Mellor 2008

Stokes Drift Incorporates mass transport from waves into the 3D model

SWAN Coupling Uses SWAN to provide: – Wave Number – Direction – Frequency – Energy (from the Action Density)

Couple2Swan Added 3D Radiation Stress equation to the ComputeRadiationStress and ComputeWaveDrivenForces Subroutines Created Compute3DStokesDrift Subroutine Set up equations to be able to turn them on and off with Input File Flags

VSMY Added Stoke’s Drift Velocity to the velocity at each node Added the 3D Radiation Stress to the RHS forcing vector in the VSSOL subroutine

IM Types 3 Different Models – IM 7 - Depth Dependent Radiation Stress – IM 8- Depth Dependent Radiation Stress and Stokes Drift – IM 9- Stokes Drift

Stability Testing Hurricane Gustav – EC95 Grid – Quick Run – No Tides – 5 day run Results Pending

Questions?