Indian Ocean wave Modeling Beijing, China, 25 to 29 July 2005 Joint Regional Conference on Disaster Relief and Management – International Cooperation &

Slides:



Advertisements
Similar presentations
Basic Wave Theory Review
Advertisements

2. The WAM Model: Solves energy balance equation, including Snonlin
The Wave Model ECMWF, Reading, UK.
Slide 1 The Wave Model ECMWF, Reading, UK. Slide 2The Wave Model (ECWAM) Resources: Lecture notes available at:
Chapter 7 Waves in the Ocean ©2003 Jones and Bartlett Publishers.
Transformation of Shallow-Water Waves The Certificate Program in Tsunami Science and Preparedness. Held at the University of Washington in Seattle, Washington.
Transformation of Shallow-Water Waves Annual National Symposium on Computational Science and Engineering (ANSCSE11) Held at Phuket, Thailand, March 28-30,
WAVES disturbance caused by the movement of energy from a source through some medium (solid, liquid or gas). THERE ARE MANY DIFFERENT SIZES AND SHAPES.
Introduction to Oceanography Dynamic Oceanography: Waves.
Operational Forecasting Wave Models. WaveWatch III (Tolman 1997, 1999a) Model description: – Third generation wave model developed at NOAA/NCEP. – Solves.
Waves. 2 3  Waves are created on the surface of water as the result of a generating force.  An additional force, called the restoring force, acts to.
WAVES.
Waves.
Chapter 21 Section 2.
Waves in the Ocean Words from these PPT slides are already on the course web site. Waves in the Ocean Words from these PPT slides are already on the course.
Waves. 2 3 Waves are created on the surface of water as the result of a generating force. An additional force, called the restoring force, acts to return.
2 – SEA WAVE CHARACTERIZATION António F. de O. Falcão Instituto Superior Técnico, Universidade Técnica de Lisboa, Portugal Renewable Energy Resources 2008.
The Fourth Session of the Joint WMO-IOC Technical Commission for Oceanography and Marine Meteorology (JCOMM-4), Coupling of high-resolution meteorological.
9.2 Ocean Waves, Tides and Currents
WAVES disturbance caused by the movement of energy from a source through some medium (solid, liquid or gas).
Waves, beaches, & sand transport
Juan Carlos Ortiz Royero Ph.D.
Ocean Waves What causes ocean waves to form and move?
Forecasting Ocean Waves Problem: Given observed or expected weather, what will be the sea state? Ships are sunk not by winds, but by waves!
Chapter 10 Ocean Waves Part 1 ftp://ucsbuxa.ucsb.edu/opl/tommy/Geog3awinter2011/
Coastlines. Beaches and Coasts The coastal zone and beaches along the continental margin are among the most dynamic geologic setting on earth Human settlements.
OCEAN WAVES. OBJECTIVES Identify the generating force of different waves Describe the factors that influence wind wave development Describe the basic.
How are waves formed and what are the characteristics of waves?
The Air-Sea Momentum Exchange R.W. Stewart; 1973 Dahai Jeong - AMP.
Waves Caused by wind, tides, and earthquakes STORMSSWELL SURF (energy in) (energy out) Waves move away from the sea that generated them; this energy can.
Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from.
Waves How Does Ocean Water Move?
New Topic - Waves Always wind, so always waves Transfer of energy from a windy area to a narrow coastal band General topics to cover: (1) Generation (2)
Waves. What processes drive ocean waves?  If you have ever been to the beach or sailed on the sea, you know the ocean’s surface has many faces.  Sometimes.
Waves and Water Dynamics
Wsws wpwp dw wpwp wsws NARR ONLY Variations in x (size parameter)
–wave –crest –trough –breaker Objectives Describe the physical properties of waves. Explain how tides form. Compare and contrast various ocean currents.
WAVE PROCESSES ON A COAST HOW WAVES ARE FORMED Ocean surface waves are occur on the free surface of the ocean. They usually result from wind, and are also.
Chapter 10 Waves.
Ocean Waves Chapter 10 Oceanography.
Unit 3: Waves and tides.
Chapter 7 Waves in the Ocean.
Wave Properties. S8P4. Students will explore the wave nature of sound and electromagnetic radiation. d. Describe how the behavior of waves is affected.
Wave motion. A wave is a means of transferring energy.
Milton Garces, Claus Hetzer, and Mark Willis University of Hawaii, Manoa Source modeling of microbarom signals generated by nonlinear ocean surface wave.
Waves Waves result from interplay between disturbing forces & restoring forces In the oceans, disturbances originate –At the surface, winds, ships, etc.
Waves Chapter 9.
The Waves An Introduction to the World’s Oceans Sverdrup et al. - Chapter Ten - 8th Ed.
Definition Undulation that forms as a disturbance moves along the surface of the water.
© 2014 Pearson Education, Inc. W Waves and Water Dynamics Chapter 8.
Physical Oceanography Surface Gravity Waves Properties Dispersion Refraction & Diffraction Group velocity Generation Assignment: Read Chapter 16 of Stewart:
Conclusion Model is already available to represent tsunami
Waves Transmit energy (not mass) across the ocean’s surface
WAVES.
Waves Transmit energy (not mass) across the ocean’s surface
Lab 5 WAVES. What is waves ? how do waves form? Wave is a movement of upper surface of water due to transfer of energy from the wind into the water without.
Wave Parameters (Figure 7-1a)
Waves.
Wave Parameters (Figure 7-1a)
Chapter 16.2 Waves and Tides.
Forecasting Ocean Waves
Waves Page 49 in Notebook.
Waves and Tides Notes.
Waves, Tides, and Currents
Waves in the Ocean.
Lets Review! Handout 10 Waves
Wave Dynamics And Wind Waves
Waves.
Lesson 9: Waves Physical Oceanography
Coastal system A system is may be defined as all the inputs, outputs and interactions that affect a physical process or event. Appropriate design considers.
Presentation transcript:

Indian Ocean wave Modeling Beijing, China, 25 to 29 July 2005 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Wave Basic Knowledge Wave Basic Knowledge Ocean Wave Modeling Ocean Wave Modeling - Hard Computing Approach - Hard Computing Approach - Soft Computing Approach - Soft Computing Approach VirtualWave3D Program VirtualWave3D Program

Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Wave Basic Knowledge

Anatomy of a wave A wave can be regarded initially as an ideal a sinusoidal wave (though the ideal regular waves bears little resemblance to real waves observed at sea  irregular in form and period) Characteristics: H: Height (from crest to trough) L: Wavelength (from crest to crest) T: Period (time required for two successive crests to pass a point) h: Depth of water column below mean surface level Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

Anatomy of a wave A few waves: A case of temporal- and spatial-scales Waves are classified according to their wave period Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

© 2002 Brooks/Cole, a division of Thomson Learning, Inc. What characteristics are used to classify waves?  Disturbing force  Free waves vs. forced waves  Restoring force  Wavelength Classifying Waves Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

© 2002 Brooks/Cole, a division of Thomson Learning, Inc. Classifying Waves Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

© 2002 Brooks/Cole, a division of Thomson Learning, Inc. Wave Dynamics And Wind Waves Waves transmit energy across the ocean’s surface. Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

© 2002 Brooks/Cole, a division of Thomson Learning, Inc. Ocean Waves Orbital waves are waves in which the particles of water move in closed circles as the wave passes. Progressive waves are waves of moving energy in which the wave form moves in one direction along the surface (or junction) of the transmission medium. Orbital waves are a type of progressive wave because the waveform moves forward Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

© 2002 Brooks/Cole, a division of Thomson Learning, Inc. What are the parts of an ocean wave? Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

© 2002 Brooks/Cole, a division of Thomson Learning, Inc. Deep Water Waves, Shallow Water Waves Note the importance of the relationship between wavelength and depth in determining wave type. Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

Anatomy of wind waves Wind waves: As the wind blows  formation of ripples (capillary waves) As the wind increases in speed  waves become larger (gravity waves) Variety and size of wind-generated waves are controlled by four principal factors: Wind velocityWind velocity Wind durationWind duration Unobstructed distance over which wind blows (fetch)Unobstructed distance over which wind blows (fetch) Original sea stateOriginal sea state Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

© 2002 Brooks/Cole, a division of Thomson Learning, Inc. What factors affect wind wave development? Wind strength - wind must be moving faster than the wave crests for energy transfer to continue Wind duration - winds that blow for a short time will not generate large waves Fetch - the uninterrupted distance over which the wind blows without changing direction Factors Affecting Wind Wave Development Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

© 2002 Brooks/Cole, a division of Thomson Learning, Inc. Factors Affecting Wind Wave Development Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Ocean Wave modeling

Ocean wave forecasting techniques Hard computing approach by using WAM (WAve Model) Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Soft computing approach by using NNs (Neural Networks)

Hard computing approach by using WAM Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

Numerical wave modeling - The most used descriptor of the wave field is the energy density spectrum in both frequency and direction, where is the frequency, and the direction of propagation. This representation is particularly useful because we already know how to interpret what we know about wave physics in terms of the spectral components,.Each component can be regarded as a sinusoidal wave of which we have a reasonably well-understood theory. From this spectrum, we can deduce most of the parameters expected of an operational wave model namely, the significant wave height, the frequency spectrum, the peak frequency and secondary frequency maxima, the directional spectrum, the primary wave direction, any secondary wave directions, the zero-crossing period, etc. Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

InputNonlinearDissipationGroup velocity Angular frequencyLatitudeLongitudeDirection Energy balance equation Wave spectrum Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

Third generation models A classification of wave models into first, second and third generation wave models is also used, which takes into account the method of handling the nonlinear source term First generation models do not have an explicit term. Nonlinear energy transfers re implicitly expressed through the and terms.First generation models do not have an explicit term. Nonlinear energy transfers re implicitly expressed through the and terms. Second generation models handle the term by parametric methods, for example by applying a reference spectrum (for example the JONSWAP spectrum or the Pierson/Moskowitz spectrum) to reorganize the energy (after wave growth and dissipation) over the frequencies.Second generation models handle the term by parametric methods, for example by applying a reference spectrum (for example the JONSWAP spectrum or the Pierson/Moskowitz spectrum) to reorganize the energy (after wave growth and dissipation) over the frequencies. Third generation models calculate the nonlinear energy transfers explicitly.Third generation models calculate the nonlinear energy transfers explicitly. Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

- The WAM-model is a third generation wave model which solves the wave transport equation explicitly without any presumptions on the shape of the wave spectrum. It represents the physics of the wave evolution in accordance without knowledge today for the full set of degrees of freedom of a 2D wave spectrum. Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 WAM model

The model was developed at the Max-Planck-Institut Meteorologie in Hamburg (Germany) by S. and K. Hasselmann with the aid of P. Janssen and G. Komen (KNMI, Netherlands), and L. Zambreski and H. (GKSS, Germany, ECMWF, Reading, UK). It has been installed at about 35 institutions world wide and is used for research and also operational application. It is also being applied for interpreting and assimilating satellite wave data. Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

WAM DEVELOPMENT SWAMP STUDY OF 1st AND 2nd GENERATION WAVE MODELS (1984) SWAMP STUDY OF 1st AND 2nd GENERATION WAVE MODELS (1984) DEVELOPMENT OF 3rd GENERATION WAVE MODEL GOAL : DEVELOPMENT OF 3rd GENERATION WAVE MODEL GOAL : DEVELOP A 3G WAVE MODEL BASE ON PHYSICS DEVELOP A 3G WAVE MODEL BASE ON PHYSICS IMPLEMENT A GLOBAL VERSION FOR MEDIUM RANGE FORECASTING IMPLEMENT A GLOBAL VERSION FOR MEDIUM RANGE FORECASTING DEVELOP NESTED VERSIONS OF WAM DEVELOP NESTED VERSIONS OF WAM PERFORM STUDIES OF DYNAMIC WAVE PROCESSES PERFORM STUDIES OF DYNAMIC WAVE PROCESSES DEVELOP DATA ASSIMILATION TECHNIQUES DEVELOP DATA ASSIMILATION TECHNIQUES Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

WAM model Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

Model physics and dynamics The WAM model describes the evolution of a two- dimensional ocean wave spectrum. In contrast to first and second generation models, the third generation model WAM introduces no ad hoc assumptions on the spectral shape. It computes the 2-d wave variance spectrum through integration of the transport equation The WAM model describes the evolution of a two- dimensional ocean wave spectrum. In contrast to first and second generation models, the third generation model WAM introduces no ad hoc assumptions on the spectral shape. It computes the 2-d wave variance spectrum through integration of the transport equation Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

Model physics and dynamics Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

Wave spectrum Linear wave theory (wave energy spectrum) Statistical theory of linear random waves (wave number spectrum) Ocean Wave model based on WAM Energy balance equation Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

SOURCE TERMS S = S in + S nl + S ds + S bottom SOURCE TERMS S = S in + S nl + S ds + S bottom WIND INPUT SOURCE TERM S in WIND INPUT SOURCE TERM S in CYCLE 1-3 BASED ON SYNDER (1981) CYCLE 1-3 BASED ON SYNDER (1981) CYCLE 4 BASED ON JANSSEN (1991) CYCLE 4 BASED ON JANSSEN (1991) NON-LINEAR SOURCE TERM S nl NON-LINEAR SOURCE TERM S nl BASED ON HASSELMANN’S THEORIES ON WAVE-WAVE INTERACTIONS BASED ON HASSELMANN’S THEORIES ON WAVE-WAVE INTERACTIONS DISSAPATION SOURCE TERM S ds DISSAPATION SOURCE TERM S ds BASED ON HASSELMANN’S THEORY OF DISSAPATION DUE TO WHITE CAPPING. TUNING TERM BASED ON HASSELMANN’S THEORY OF DISSAPATION DUE TO WHITE CAPPING. TUNING TERM BOTTOM FRICTION SOURCE TERM S bottom BOTTOM FRICTION SOURCE TERM S bottom ONLY APPLIES IN SHALLOW WATER ONLY APPLIES IN SHALLOW WATER Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

Soft computing approach by using NNs (Neural Networks) Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

การประชุมสัมมนาวิชาการ เนื่องในวันสถาปนากรมอุตุนิยมวิทยา Ocean Wave model based on GRNN (Generalize Regression Nearal Network ) U = wind velocity at 10 m above the mean sea level,  w : wind direction, F : fetch length, H s : significant wave height, D w : sea depth Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

การประชุมสัมมนาวิชาการ เนื่องในวันสถาปนากรมอุตุนิยมวิทยา Observing GRNN WAM UNOCAL STATION Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

การประชุมสัมมนาวิชาการ เนื่องในวันสถาปนากรมอุตุนิยมวิทยา Observing GRNN WAM HUA-HIN STATION Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

UNOCAL STATION HUA-HIN STATION Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

Create VirtualWave3D Program Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

VirtualWave Algorithm Read Topography (Earth grid points) Read Topography (Earth grid points) Read WAM Output of all time steps (every 3 hours) Read WAM Output of all time steps (every 3 hours) Read Wave Height (WaH) Read Wave Height (WaH) Read Wave Speed (WaS), Wave Direction (WaD) Read Wave Speed (WaS), Wave Direction (WaD) Read Wind Speed (WiS), Wind Direction (WiD) Read Wind Speed (WiS), Wind Direction (WiD) Read Wave Frequency Read Wave Frequency Calculate SWH and ETA of all points Calculate SWH and ETA of all points SWH = (WaH/2)*Cos(2*PI*WaF*t - WaD) SWH = (WaH/2)*Cos(2*PI*WaF*t - WaD) ETA = (WaH/2)*Sin(-2*PI*WaF*t) ETA = (WaH/2)*Sin(-2*PI*WaF*t) Visualize and animate all data of all time steps Visualize and animate all data of all time steps Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

Methodology - Grid Latitude 5N- 15N 10 degrees = 41 points Longitude 95E- 105E 10 degrees =41 points Resolution 0.25 degrees = 27.75km (1 degree = 111km) Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

SWH(Significant Wave Height) - ETA SWH Eta Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

Visualization Results - TY Linda 1997 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

Visualization Results - TD 2003 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007

Visualization Results - TS Muifa 2004 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Help at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007 Joint Regional Conference on Disaster Relief and Management – International Cooperation & Role of ICT Held at Alexandria, Egypt during the period from 14 to 17 April 2007