STWAVE Usage & Theory Taylor Asher.

Slides:



Advertisements
Similar presentations
INWAVE: THE INFRAGRAVITY WAVE DRIVER OF THE COAWST SYSTEM
Advertisements

Operational Forecasting Wave Models. WaveWatch III (Tolman 1997, 1999a) Model description: – Third generation wave model developed at NOAA/NCEP. – Solves.
Radio Frequency Fundamentals Wireless Networking Unit.
The Hydrogen Spectrum Experiment 6 amplitude Wavelength -λ.
Reflections Diffraction Diffusion Sound Observations Report AUD202 Audio and Acoustics Theory.
2 – SEA WAVE CHARACTERIZATION António F. de O. Falcão Instituto Superior Técnico, Universidade Técnica de Lisboa, Portugal Renewable Energy Resources 2008.
The role of resonant wave interactions in the evolution of extreme wave events R. Gibson and C. Swan Imperial College London.
Electromagnetic Spectrum. Waves are everywhere! Wave – Disturbance that moves through space – Takes energy/information and moves it from one location.
Wavelength – λ – distance between successive points on a wave (crest to crest)
Wave Modeling Local Wave Transformations Billy L. Edge & Margery Overton CVEN
Classical vs Quantum Mechanics Rutherford’s model of the atom: electrons orbiting around a dense, massive positive nucleus Expected to be able to use classical.
Chapter 8 Decomposition & Superposition of Irregular Waves 8.1 Introduction 8.2 Decomposition 8.3 Superposition 8.4 Uni-Directional Hybrid Wave Model (HWM)
Spectral Analysis of Wave Motion Dr. Chih-Peng Yu.
Remote Sensing: John Wilkin Active microwave systems Coastal HF Radar IMCS Building Room 214C ph: Dunes of sand and seaweed,
Waves can also be reflective and refractive Waves can bounce off of something after striking it. That is a reflection. Sound and light waves can equally.
Electromagnetic Wave Theory
Suggested components of a GW parameterization design that includes the major sources and modifying influences: 1. individual source spectra in amplitude,
SeaSonde Overview.
Spectra of Gravity Wave Turbulence in a Laboratory Flume S Lukaschuk 1, P Denissenko 1, S Nazarenko 2 1 Fluid Dynamics Laboratory, University of Hull 2.
Chapter 5 Solutions for Interacting Waves Using A MCM 5.1 Governing Equations and Hierarchy Eq.s 5.2 An Example of Applying A Mode Coupling Method (MCM)
Waves & Sound.
Properties of ElectroMagnetic Radiation (Light)
Review Game. The distance from the peak of a wave to the adjacent wave is the _____. a) amplitude b) wavelength Answer: b) wavelength.
Wave Theory Essential Question: What is a wave?. Answer Me!!!  Give an example of a wave. Then describe what that wave carries.
The Electromagnetic Spectrum and Light. Wavelength - The distance between two consecutive peaks of a wave.
Mid-term meeting report AquaPark – Norad funded project Planning and management of aquaculture parks for sustainable development of cage farms in the Philippines.
Introduction to Optics. 1. The Great Debate 2. What is light? 3. Properties of light 4. The wave-like model 5. Theories of colour.
National Center for Computational Hydroscience and Engineering The University of Mississippi Wave Model of CCHE2D-Coast For Model Training Course Yan Ding,
Electromagnetic Radiation in vacuum
Effects of a Suspended Bottom Boundary Layer on Sonar Propagation Michael Cornelius June 2004.
Wsws wpwp dw wpwp wsws NARR ONLY Variations in x (size parameter)
UPenn NROTC Unit, dtd Fall 2004 Naval Weapons Systems Energy Fundamentals.
The incoming wave travels at 5ms -1 and has a wavelength of 4m. The wave changes its speed once it moves onto a shallower region and as the result its.
1 Honors Physics 1 Summary and Review - Fall 2013 Quantitative and experimental tools Mathematical tools Newton’s Laws and Applications –Linear motion.
Part 1 – Wave Characteristics. What is a Wave? A disturbance that carries energy through matter or space.
Calculating Wave Speed
OBSERVATIONSMODELINGPROJECT SWAN (Simulating Waves Nearshore) ADCIRC (Advanced Circulation Model) BOM (Bergen Ocean Model) WRF-ARW (Weather Research.
Author: Holly Clark Date: May 2015 Supporting Authors: Ralph A. Stephen, Gopu R. Potty, James H. Miller Wave Propagation in Muddy Sediments using Time.
Wave Breaking (10pt)  Which type of breaker for the steepest bottom slope?  Spilling breaker  Plunging breaker  X Surging breaker.
Which of the following would represent a measurement of frequency? 40 m400 Hz 3.00 x 10 8 m/s150 J.
Click me for movie Get a 100% before moving on to next slide Screenshot here.
Nonstationary regimes in gravity wave turbulence S Lukaschuk 1, R Bedard 1, S Nazarenko 2 1 Fluid Dynamics Laboratory, University of Hull 2 Mathematics.
Physical Oceanography Surface Gravity Waves Properties Dispersion Refraction & Diffraction Group velocity Generation Assignment: Read Chapter 16 of Stewart:
Wave speed equation v=ƒλ.
Basic Science in Remote Sensing
Fang Liu and Arthur Weglein Houston, Texas May 12th, 2006
Phonons and lattice vibration
the wavelength increases and the frequency is unchanged.
The Earth is {image} meters from the sun
Review of basic EM concepts
NET 301 LECTURE3 30/11/1436 Lect3 NET 301.
For a periodic complex sound
Forecasting Ocean Waves
Waves in Two Dimensions
Lecture 2: SIGNALS 2nd semester By: Elham Sunbu.
Calculating Wave Speed
Bohr Model of Atoms & Electron Energy 2.5
The FOCI method versus other wavefield extrapolation methods
Extreme and unexpected waves
Bohr Model of Atoms & Electron Energy 2.5
Wireless Communications Chapter 4
24.2 Speed of Waves.
Review of basic EM concepts
Natalie Laudier Operational Oceanography 13Feb2009
Monterey Buoy LT Karen Wingeart.
Uses of filters To remove unwanted components in a signal
Diyu Yang Mentor: Xu Chen Advisor: José E. Schutt-Ainé Abstract
The speed of light in air is essentially c. (c = 3.00x108 m/s).
An optimized implicit finite-difference scheme for the two-dimensional Helmholtz equation Zhaolun Liu Next, I will give u an report about the “”
Honghui Zhang, Andrew J. Watrous, Ansh Patel, Joshua Jacobs  Neuron 
Presentation transcript:

STWAVE Usage & Theory Taylor Asher

Presentation Introduction Theory Numerical discretization Input/Output Wave action Wave spectrum Numerical discretization Input/Output Input files Model parameters Wave spectrum, wind, water level Output files Selected wave parameters Wave parameter fields Application

Theory Model assumptions Mild bottom slope, negligible reflection Spatially homogeneous offshore (boundary) Steady-state formulation Linear refraction & shoaling Depth-uniform current Frictionless bottom Linear radiation stress

Wave Action Steady-state conservation of spectral wave action NOTE sum of sources and sinks speed of propagation of wave packet wave phase speed kinetic+potential, per unit surface area self-explanatory relative to reference axis

Wave spectrum

Wave spectrum Bretschneider-Mitsuyasu spectrum, with peak frequency fp, and wind speed U with

Wave spectrum Directionalized spectrum, with magnitude-normalized directional term with normalization term

Numerical discretization Domain is made of a grid of NI by NJ square cells, Δx in length, with locally-defined axes Waves start at I=1, propagating toward I=NI No backward-propagation 35 angular bins ±87.5o

Input/Output

Input files Model parameters (options.std) IPRP: Switch for source/sink terms, such as wind waves, wave-wave interactions ICUR: Switch for current IBREAK: Switch for printing wave breaking IRS: Switch for calculating radiation stress gradient NSELCT: Number of special output points; 2-D wave spectra are generated for these points Points: (I,J) pairs for each point.

Input files Wave spectrum, wind, water level (spec.in) NF: Number of frequency bins NA: Number of direction bins (must be 35) Frequency vector of length NF, ordered smallest to largest (Hz) IDD: Integer event identifier U: Wind speed (m/s) UDIR: Wind direction (degrees) FM: Peak spectral frequency (Hz) DADD: Water elevation correction Wave spectrum (m2/s/Hz), ordered lowest frequency & -85 deg to 85 deg, to highest frequency -85 to 85

spec.in NF=25 NA=35 IDDD=200700 U=15 m/s UDIR=10 deg. FM=0.07 Hz DADD=-1 m

Output files Selected wave parameters (selhts.out) IDD: Integer event identifier (from spec.in) I: Integer x-grid cell index J: Integer y-grid cell index N: Integer number of point (points are 1 to NSELCT Hm0: Zeroth-moment (significant) wave height at cell (I,J) in meters Tp: Peak wave period at cell (I,J) in seconds αm: Mean wave direction at cell (I,J) in degrees

Output files Wave parameter fields (wavfld) NI, NJ: Grid dimension DXINC: Grid spacing IDD: Integer event identifier (as before) Wave height for each cell in wave field, ordered in the cross-shore direction from (1,NJ) to (NI,NJ), to (1,1) to (NI,1) Wave period for each cell in wave field, same ordering Wave direction for each cell in wave field, same ordering