The Netherlands. The Netherlands: 18% water (area) 180 x 300 km2; ~ 21% below sea population: 17 mln; ~ 30-40% below sea 2
|
|
|
- Amberly Monica Stokes
- 5 years ago
- Views:
Transcription
1 (3) Where Applied Mathematics, Hydrodynamics and Ocean Science meet: Predictive, Diagnostic & Sea Going Assessments of Water levels & Global- and Internal Tides 1: Dr. R. (Ramses) van der Toorn, Prof. Dr. A.W. Heemink, (TUD) 2: Dr. M. Verlaan (Deltares) 3: Dr. Th. Gerkema, Dr. H. van Haren (NIOZ) (2) (1 )
2 The Netherlands The Netherlands: 18% water (area) 180 x 300 km2; ~ 21% below sea population: 17 mln; ~ 30-40% below sea 2
3 The Netherlands The Netherlands: water management 1953 flood: 1800 killed, lost home. Oosterscheldekering (finished 1986) Oosterschelde: crucial eco-zone ocean species breed here 3
4 The Netherlands The Netherlands Rotterdam harbor: largest port in Europe offshore 4 Petrochemicals
5 The Netherlands The Netherlands Rotterdam harbor: largest port in Europe Maeslantkering: storm surge protection: 5
6 Water Level / Storm Surge Forecasting Dutch Continental Shelf Model (DCSMv6) Water Level Forecasting content: non-linear shallow water dynamics captures tide-surge interaction 6
7 Water Level / Storm Surge Forecasting Dutch Continental Shelf Model (DCSMv6) Water Level Forecasting content: non-linear shallow water dynamics captures tide-surge interaction bathymetry 7
8 Water Level / Storm Surge Forecasting Dutch Continental Shelf Model (DCSMv6) Water Level Forecasting content: non-linear shallow water dynamics captures tide-surge interaction bathymetry forcing: tidal (gravity field: sun, moon)* meteorology (pressure, winds) R Re α 8 *Courtesy: E. Schrama, TU Delft
9 Water Level / Storm Surge Forecasting Dutch Continental Shelf Model (DCSMv6) Water Level Forecasting content: non-linear shallow water dynamics captures tide-surge interaction bathymetry forcing: tidal (gravity field: sun, moon) meteorology (pressure, winds) operation: data assimilation: Kalman Filtering RMSE(m) a.f.o. lead time, with and without Kalman Filter real time input data stations 5/6 December 2013 storm surge event, Hoek van Holland 9
10 Water Level / Storm Surge Forecasting Dutch Continental Shelf Model (DCSMv6) Water Level Forecasting content: non-linear shallow water dynamics captures tide-surge interaction bathymetry forcing: tidal (gravity field: sun, moon) meteorology (pressure, winds) operation: data assimilation: Kalman Filtering (dynamic) calibration (parametric) comes first in real life comes last this presentation: link to oceanography & science! 10
11 Global Ocean Mixing As Driven by Mechanics Abyssal Recipes II: Energetics of Tidal and Wind Mixing Walter Munk & Carl Wunsch Deep Sea Res., 1998 Something Stirs in the Deep Peter Killworth Nature, December
12 Mixing in Action.. Kelvin-Helmholtz billows, "Extremely long Kelvin-Helmholtz billow trains in the Romanche Fracture Zone" Hans van Haren, Louis Gostiaux, Eugene Morozov & Roman Tarakanov Geophys. Res. Lett., Dec
13 Mixing in Action.. Kelvin-Helmholtz billows.. shear induced overturning.. "Extremely long Kelvin-Helmholtz billow trains in the Romanche Fracture Zone" Hans van Haren, Louis Gostiaux, Eugene Morozov & Roman Tarakanov Geophys. Res. Lett., Dec
14 Mixing in Action.. wave breaking and turbulence, over sea-mount slopes.. "Where large deep-ocean waves break" Hans van Haren, Andrea Cimatoribus and Louis Gostiaux Geophys. Res. Lett., April
15 Relations global tides and mixing forcing Tides Mixing dissipation Global tide models can distinguish between impact/significance of bottom friction dissipation wave drag dissipation (parameterized generation by tide-topography interaction): M2 wave drag dissipation Modelling the global tides: modern insights from FES2004 F.Lyard, F. Lefevre, T. Letellier; Oc. Dyn. (2006) 15
16 Water Level Forecasting Dutch Continental Shelf Model (DCSMv6) Water Level Forecasting content: non-linear shallow water dynamics captures tide-surge interaction bathymetry forcing: tidal (gravity field: sun, moon) meteorology (pressure, winds) operation: data assimilation: Kalman Filtering (dynamic) real time adjustment of dynamic fields calibration (parametric) optimization of model parameters for model accuracy bathymetry bottom roughness "(..) water-level forecasting (..) through direct modeling of tide, surge and non-linear interaction" F.Zijl, M. Verlaan, H. Gerritsen, Ocean Dyn. (2013) 63 16
17 Segmentation for Calibration init left: segmentation for calibration of bottom roughness and bathymetry right: calibrated bottom roughness 17
18 Calibrated Energy Dissipation vs. bathymetry 18
19 The next step (in progress) Global tide model 19
20 Global flood risk and intervention analyzer Starts in 2015 PL: Hessel Winsemius
21 Case: Storm December again: tide & surge
22 Necessary improvements (in progress!) Self attraction and loading Tides modify the gravity potential as well Internal tides Tides create internal tide where there is stratification and steep bathymetry This creates dissipation (roughly ¼ of total tidal dissipation on global scale) N= f x =β g h x g ρ ρ0 z Depends on stratification
23 Conclusion Ocean Science: Global effort ongoing, inspired by the vision of Munk & Wunsch '98, to construct & verify a detailed picture of the ocean's distributions & dynamics complementary approaches: theory & observations of mixing & dissipation processes global circulation models (not in this presentation) tidal modeling modeling of dynamics satellite data assimilation Hydrology: water-level forecasting (tide & surge) physics based simulation of dynamics parameter tuning & Kalman filtering => data assimilation improving forecasts thanks to increased physical content.... to the extent that engineering meets science: tuning forecast models hinted where increased dissipation occurs in the ocean => to be explored and continued.. 23
24 Thank you 24
The impact of ocean bottom morphology on the modelling of long gravity waves from tides and tsunami to climate
The impact of ocean bottom morphology on the modelling of long gravity waves from tides and tsunami to climate Christian Le Provost and Florent Lyard Laboratoire d Etudes en Géophysique et Océanographie
Surface Wave Dynamics in the Coastal Zone
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Surface Wave Dynamics in the Coastal Zone Gerbrant Ph. van Vledder Department of Civil engineering and Geosciences, Delft
Impact of the tides, wind and shelf circulation on the Gironde river plume dynamics
Impact of the tides, wind and shelf circulation on the Gironde river plume dynamics F. Toublanc 1, N. Ayoub 2, P. Marsaleix 3, P. De Mey 2 1 CNES/LEGOS 2 CNRS/LEGOS 3 CNRS/LA, Toulouse, France 5th GODAE
Hydrodynamic and hydrological modelling to support the operation and design of sea ports
Hydrodynamic and hydrological modelling to support the operation and design of sea ports Data needs and examples Martijn de Jong (port/nautical requirements, waves, currents) Sofia Caires (mean and extreme
An Atlas of Oceanic Internal Solitary Waves (February 2004) by Global Ocean Associates Prepared for Office of Naval Research Code 322 PO
Overview The is located in the North Atlantic Ocean between southern Ireland and southwest England (Figure 1). The Sea s western edge covers a continental shelf region characterized by rough and irregular
Conditions for Offshore Wind Energy Use
Carl von Ossietzky Universität Oldenburg Institute of Physics Energy Meteorology Group Detlev Heinemann Conditions for Offshore Wind Energy Use Detlev Heinemann ForWind Carl von Ossietzky Universität Oldenburg
Patchy mixing in the Indian Ocean
CPT: Representing internal-wave driven mixing in global ocean models The Team: Matthew Alford (UW) Brian Arbic (U Michigan) Frank Bryan (NCAR) Eric Chassignet (FSU) Gokhan Danabasoglu (NCAR) Peter Gent
Review of Equivalent Neutral Winds and Stress
Review of Equivalent Neutral Winds and Stress Mark A. Bourassa Center for Ocean-Atmospheric Prediction Studies, Geophysical Fluid Dynamics Institute & Department of Earth, Ocean and Atmospheric Science
Wave-Current Interaction in Coastal Inlets and River Mouths
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Wave-Current Interaction in Coastal Inlets and River Mouths Tim T. Janssen Department of Geosciences, San Francisco State
WAVE FORECASTING FOR OFFSHORE WIND FARMS
9 th International Workshop on Wave Hindcasting and Forecasting, Victoria, B.C. Canada, September 24-29, 2006 WAVE FORECASTING FOR OFFSHORE WIND FARMS Morten Rugbjerg, Ole René Sørensen and Vagner Jacobsen
PRINCIPLES OF FLUID FLOW AND SURFACE WAVES RIVERS, ESTUARIES, SEAS AND OCEANS. Leo C. van Rijn
PRINCIPLES OF FLUID FLOW AND SURFACE WAVES IN RIVERS, ESTUARIES, SEAS AND OCEANS (Edition 2011) Leo C. van Rijn Physical Geography Other publications: Principles of Sediment Transport in Rivers, Estuaries
LONG WAVES OVER THE GREAT BARRIER REEF. Eric Wolanski ABSTRACT
LONG WAVES OVER THE GREAT BARRIER REEF by Eric Wolanski k ABSTRACT Low-frequency forcing of water currents over the continental shelf f Australia is quite strong and should be taken into account when the
Beach Wizard: Development of an Operational Nowcast, Short-Term Forecast System for Nearshore Hydrodynamics and Bathymetric Evolution
Beach Wizard: Development of an Operational Nowcast, Short-Term Forecast System for Nearshore Hydrodynamics and Bathymetric Evolution Ad Reniers Civil Engineering and Geosciences, Delft University of Technology
An Observational and Modeling Study to Quantify the Space/Time Scales of Inner Shelf Ocean Variability and the Potential Impacts on Acoustics
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. An Observational and Modeling Study to Quantify the Space/Time Scales of Inner Shelf Ocean Variability and the Potential
OCEANOGRAPHY STUDY GUIDE
OCEANOGRAPHY STUDY GUIDE Chapter 2 Section 1 1. Most abundant salt in ocean. Sodium chloride; NaCl 2. Amount of Earth covered by Water 71% 3. Four oceans: What are they? Atlantic, Pacific, Arctic, Indian
WAVE BREAKING AND DISSIPATION IN THE NEARSHORE
WAVE BREAKING AND DISSIPATION IN THE NEARSHORE LONG-TERM GOALS Dr. Thomas C. Lippmann Center for Coastal Studies Scripps Institution of Oceanography University of California, San Diego 9500 Gilman Dr.
Preliminary Wake Wash Impact Analysis Redwood City Ferry Terminal, Redwood City, CA
Technical Memorandum Preliminary Wake Wash Impact Analysis Redwood City Ferry Terminal, Redwood City, CA 1. Introduction The following preliminary wake wash impact analysis was initiated by the Port of
Unsteady Wave-Driven Circulation Cells Relevant to Rip Currents and Coastal Engineering
Unsteady Wave-Driven Circulation Cells Relevant to Rip Currents and Coastal Engineering Andrew Kennedy Dept of Civil and Coastal Engineering 365 Weil Hall University of Florida Gainesville, FL 32611 phone:
Tides. Tides: longest waves. or seas. or ripples
Tides or ripples or seas Tides: longest waves Tides Definition: The rise and fall of sea level due to the gravitational forces of the Moon and Sun and the rotation of the Earth. Why tides are important?
Refined Source Terms in WAVEWATCH III with Wave Breaking and Sea Spray Forecasts
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Refined Source Terms in WAVEWATCH III with Wave Breaking and Sea Spray Forecasts Michael L. Banner School of Mathematics
An experimental study of internal wave generation through evanescent regions
An experimental study of internal wave generation through evanescent regions Allison Lee, Julie Crockett Department of Mechanical Engineering Brigham Young University Abstract Internal waves are a complex
Cross-shore sediment transports on a cut profile for large scale land reclamations
Cross-shore sediment transports on a cut profile for large scale land reclamations Martijn Onderwater 1 Dano Roelvink Jan van de Graaff 3 Abstract When building a large scale land reclamation, the safest
Internal Waves in Straits Experiment Progress Report
DISTRIBUTION STATEMENT A: Approved for public release; distribution is unlimited. Internal Waves in Straits Experiment Progress Report Jody Klymak School of Earth and Ocean Sciences University of Victoria
Dissipation of Internal Waves in Port Susan, Puget Sound
Dissipation of Internal Waves in Port Susan, Puget Sound Proposal Draft Lauren Curry 4317 8 th Ave NE #A303 Seattle, WA 98105 (206) 632-5462 lbcurry@u.washington.edu School of Oceanography University of
Name Class Date. Use the terms from the following list to complete the sentences below. Each term may be used only once. Some terms may not be used.
Assessment Chapter Test B The Movement of Ocean Water USING KEY TERMS Use the terms from the following list to complete the sentences below. Each term may be used only once. Some terms may not be used.
Department of Meteorology. An Analysis of Sea Breezes on the South Coast of England and Evidence of Pre- and Post-Frontal Waves at the Surface.
Department of Meteorology An Analysis of Sea Breezes on the South Coast of England and Evidence of Pre- and Post-Frontal Waves at the Surface. GILLEAN J KEITH A dissertation submitted in partial fulfilment
Surface Wave Processes on the Continental Shelf and Beach
Surface Wave Processes on the Continental Shelf and Beach Thomas H. C. Herbers Department of Oceanography, Code OC/He Naval Postgraduate School Monterey, California 93943-5122 phone: (831) 656-2917 fax:
OECS Regional Engineering Workshop September 29 October 3, 2014
B E A C H E S. M A R I N A S. D E S I G N. C O N S T R U C T I O N. OECS Regional Engineering Workshop September 29 October 3, 2014 Coastal Erosion and Sea Defense: Introduction to Coastal Dynamics David
PROPOSAL OF NEW PROCEDURES FOR IMPROVED TSUNAMI FORECAST BY APPLYING COASTAL AND OFFSHORE TSUNAMI HEIGHT RATIO
PROPOSAL OF NEW PROCEDURES FOR IMPROVED TSUNAMI FORECAST BY APPLYING COASTAL AND OFFSORE TSUNAMI EIGT RATIO Weniza MEE0997 Supervisor: Yutaka AYASI Yushiro FUJII ABSTRACT Regression analysis was performed
Numerical Simulation of Internal Waves in the Littoral Ocean
Numerical Simulation of Internal Waves in the Littoral Ocean Robert L. Street Department of Civil and Environmental Engineering Stanford University Stanford, CA 94305-4020 phone: (650) 723-4969 fax: (650)
Modeling changes to the historic Lower Columbia River Estuary using Delft3D. Drew Mahedy Lumas Helaire Stefan Talke David Jay May 30, 2014
Modeling changes to the historic Lower Columbia River Estuary using Delft3D Drew Mahedy Lumas Helaire Stefan Talke David Jay May 30, 2014 Comparison: Historic and Modern LCRE US Coastal Survey, 1868 Historic
2. Water levels and wave conditions. 2.1 Introduction
18 2. Water levels and wave conditions 2.1 Introduction This Overtopping Manual has a focus on the aspects of wave run-up and wave overtopping only. It is not a design manual, giving the whole design process
Surface Wave Dynamics in the Coastal Zone
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Surface Wave Dynamics in the Coastal Zone Gerbrant van Vledder Alkyon Hydraulic Consultancy & Research Arcadis Netherlands
Large-amplitude internal wave generation in the lee of step-shaped topography
1 Large-amplitude internal wave generation in the lee of step-shaped topography B. R. Sutherland University of Alberta, Edmonton, Canada. Short title: LARGE-AMPLITUDE INTERNAL WAVE GENERATION... 2 Abstract.
Modeling Historic Columbia River Flood Impacts
Modeling Historic Columbia River Flood Impacts Columbia River Estuary Workshop May 30, 2014 Present by: Lumas Helaire; Graduate Student, Portland State University Andrew Mahedy; Graduate Student, Portland
SURFACE CURRENTS AND TIDES
NAME SURFACE CURRENTS AND TIDES I. Origin of surface currents Surface currents arise due to the interaction of the prevailing wis a the ocean surface. Hence the surface wi pattern (Figure 1) plays a key
The development of high resolution global ocean surface wave-tidecirculation
PICES Annual Meeting in Qingdao The development of high resolution global ocean surface wave-tidecirculation coupled model Fangli Qiao, Qi Shu and Bin Xiao First Institute of Oceanography, SOA, China Oct
THE POLARIMETRIC CHARACTERISTICS OF BOTTOM TOPOGRAPHY RELATED FEATURES ON SAR IMAGES
THE POLARIMETRIC CHARACTERISTICS OF BOTTOM TOPOGRAPHY RELATED FEATURES ON SAR IMAGES Taerim Kim Professor, Ocean System Eng. Dept. Kunsan University Miryong Dong San 68, Kunsan, Jeonbuk, Korea, trkim@kunsan.ac.kr
A Coastal Storm Modeling System for determination of flood hazards along a high energy coast in response to SLR and 21 st century storms
Li Erikson, Patrick Barnard, Andrea O Neill, Jodi Eshleman, Amy Foxgrover, Michael Fitzgibbon 2, Grant Ballard 2, Kelly Higgason 3 A Coastal Storm Modeling System for determination of flood hazards along
STATIONKEEPING DYNAMIC POSITIONING FOR YACHTS. Hans Cozijn
STATIONKEEPING DYNAMIC POSITIONING FOR YACHTS Hans Cozijn Senior Project Manager Offshore YACHTS VS. OFFSHORE INDUSTRY 2 YACHTS VS. OFFSHORE INDUSTRY Source : www.hdmt21.com Source : www.charterworld.com
Ocean Mixing. James N. Moum
Ocean Mixing James N. Moum College of Oceanic & Atmospheric Sciences Oregon State University Corvallis, OR 97331-5503 ph: (541) 737-2553 fx: (541) 737-2064 email: moum@coas.oregonstate.edu Award #: N00014-96-1-0250
Ocean circulation and surface buoyancy fluxes: dynamics and energetics!
Ocean circulation and surface buoyancy fluxes: dynamics and energetics Ross Griffiths with credits: Graham Hughes, Andy Hogg, Kial Stewart, Julia Mullarney, J.Tan Research School of Earth Sciences The
Waves Part II. non-dispersive (C g =C)
Waves Part II Previously we discussed Surface Gravity Waves Deep Water Waves Shallow Water Waves C g T 2 C g h dispersive (C g =C/2) Definitions: phase speed C= /T= /k non-dispersive (C g =C) group speed
Modelling of Extreme Waves Related to Stability Research
Modelling of Extreme Waves Related to Stability Research Janou Hennig 1 and Frans van Walree 1 1. Maritime Research Institute Netherlands,(MARIN), Wageningen, the Netherlands Abstract: The paper deals
Yellow Sea with contributions by John R. Apel
with contributions by John R. Apel Overview The is a shallow inland sea lying between northeastern China and the Korean Peninsula, with depths in its central north-south trough in excess of 60 to 80 m
Tidal regime along Vietnam coast under impacts of sea level rise
VNU Journal of Science, Earth Sciences 28 (2012) 133-139 Tidal regime along Vietnam coast under impacts of sea level rise Tran Thuc, Duong Hong Son* Vietnam Institute of Meteorology, Hydrology and Environment
WAVE PERIOD FORECASTING AND HINDCASTING INVESTIGATIONS FOR THE IMPROVEMENT OF
WAVE PERIOD FORECASTING AND HINDCASTING INVESTIGATIONS FOR THE IMPROVEMENT OF NUMERICAL MODELS Christian Schlamkow and Peter Fröhle University of Rostock/Coastal Engineering Group, Rostock Abstract: This
Computational Analysis of Oil Spill in Shallow Water due to Wave and Tidal Motion Madhu Agrawal Durai Dakshinamoorthy
Computational Analysis of Oil Spill in Shallow Water due to Wave and Tidal Motion Madhu Agrawal Durai Dakshinamoorthy 1 OUTLINE Overview of Oil Spill & its Impact Technical Challenges for Modeling Review
Directional Wave Spectra from Video Images Data and SWAN Model. Keywords: Directional wave spectra; SWAN; video images; pixels
Jurnal Teknologi Full paper Directional Wave Spectra from Video Images Data and SWAN Model Muhammad Zikra a*, Noriaki Hashimoto b, Masaru Yamashiro b, Kojiro Suzuki c a Department of Ocean Engineering,
Surface Wave Processes on the Continental Shelf and Beach
Surface Wave Processes on the Continental Shelf and Beach Thomas H. C. Herbers Department of Oceanography, Code OC/He Naval Postgraduate School Monterey, California 93943-5122 phone: (831) 656-2917 fax:
Effects of Offshore Forcing in the Nearshore Environment
Effects of Offshore Forcing in the Nearshore Environment Geno Pawlak Department of Ocean and Resources Engineering University of Hawaii at Manoa 2540 Dole St., Holmes Hall 402 Honolulu, HI 96822 phone:
Some basic aspects of internal waves in the ocean & (Tidally driven internal wave generation at the edge of a continental shelf)
Some basic aspects of internal waves in the ocean & (Tidally driven internal wave generation at the edge of a continental shelf) Weifeng (Gordon) Zhang Applied Ocean Physics & Engineering Department Woods
G. Meadows, H. Purcell and L. Meadows University of Michigan
www.coj.net/departments/fire+and+rescue/emergency+preparedness/rip+current.htm G. Meadows, H. Purcell and L. Meadows Over 80% of all surf related rescues are attributable to Rip Currents According to the
Modeling Surfzone/Inner-shelf Exchange
DISTRIBUTION STATEMENT A: Distribution approved for public release; distribution is unlimited. Modeling Surfzone/Inner-shelf Exchange Prof. Falk Feddersen Scripps Institutions of Oceanography IOD/SIO/UCSD
COASTAL MORPHODYNAMICS
COASTAL MORPHODYNAMICS PATRICIA CHARDÓN-MALDONADO, PHD, EIT Miguel Canals, Jack A. Puleo, Alec Torres-Freyermuth & Jens Figlus March 9, 2017 OUTLINE INTRODUCTION Meteorological Phenomena Forcing Conditions
Stefan Emeis
The Physics of Wind Park Optimization Stefan Emeis stefan.emeis@kit.edu INSTITUTE OF METEOROLOGY AND CLIMATE RESEARCH, Photo: Vattenfall/C. Steiness KIT University of the State of Baden-Wuerttemberg and
Cruise Report Towed ADCP Bay of Biscay R/V Pelagia cruise 64PE April 2005 Texel - Vigo
Reference: van Haren, H., 2005. Towed ADCP- Bay of Biscay: R/V Pelagia cruise 64PE235, 20-27 April 2005, NIOZ, 15 pp. Cruise Report Towed ADCP Bay of Biscay R/V Pelagia cruise 64PE235 20-27 April 2005
BCCS TECHNICAL REPORT SERIES
BCCS TECHNICAL REPORT SERIES Numerical studies of internal solitary wave trains generated at edges in the topography. Berntsen, J., Mathisen, J.-P. and Furnes, G. REPORT No. 21 April 13, Report on Contract
Surface Wave Processes on the Continental Shelf and Beach
DISTRIBUTION STATEMENT A: Approved for public release; distribution is unlimited. Surface Wave Processes on the Continental Shelf and Beach Thomas H. C. Herbers Department of Oceanography, Code OC/He Naval
GNSS Technology for the Determination of Real-Time Tidal Information
GNSS Technology for the Determination of Real-Time Tidal Information Benjamin Kidder C-Nav Positioning Solutions European region Outline of Topics Covered Introduction to Tides Past and Present Methods
NUMERICAL STUDY OF WIND-GENERATED WAVES IN THE RED SEA
NUMERICAL STUDY OF WIND-GENERATED WAVES IN THE RED SEA NATACHA FERY (1), GERD BRUSS (2), ABDULLAH AL-SUBHI (3) & ROBERTO MAYERLE (4) (1) Research and Technology Centre, Christian Albrechts University,
Wave Transformation Modeling with Bottom Friction Applied to the Southeast Oahu Reefs. Mary A. Cialone and Jane McKee Smith
Wave Transformation Modeling with Bottom Friction Applied to the Southeast Oahu Reefs Mary A. Cialone and Jane McKee Smith Outline Objective Study Area STWAVE Friction Formulations Model Validation Summary
RIVET Satellite Remote Sensing and Small Scale Wave Process Analysis
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. RIVET Satellite Remote Sensing and Small Scale Wave Process Analysis Hans C. Graber RSMAS Department of Ocean Sciences
Coastal Wave Energy Dissipation: Observations and Modeling
Coastal Wave Energy Dissipation: Observations and Modeling Jeffrey L Hanson US Army Corps of Engineers Field Research Facility USACE Field Research Facility Kent K. Hathaway US Army Corps of Engineers
Internal Tide Breaking at Topography
20th Australasian Fluid Mechanics Conference Perth, Australia 5-8 December 2016 Internal Tide Breaking at Topography S. Legg 1 1 Atmospheric and Oceanic Sciences Program Princeton University, Princeton,
Tidal modulation of wave-setup and wave-induced currents on the Aboré coral reef, New Caledonia
18th April 2007 Tidal modulation of wave-setup and wave-induced currents on the Aboré coral reef, New Caledonia Philippe BONNETON, Jean-Pierre LEFEBVRE, Patrice BRETEL, Sylvain OUILLON, Pascal DOUILLET
Prediction of Nearshore Waves and Currents: Model Sensitivity, Confidence and Assimilation
Prediction of Nearshore Waves and Currents: Model Sensitivity, Confidence and Assimilation H. Tuba Özkan-Haller College of Oceanic and Atmospheric Sciences Oregon State University, 104 Ocean Admin Bldg
Internal Tides and Solitary Waves in the Northern South China Sea: A Nonhydrostatic Numerical Investigation
Internal Tides and Solitary Waves in the Northern South China Sea: A Nonhydrostatic Numerical Investigation Ping-Tung Shaw Dept of MEAS, North Carolina State University Box 8208, Raleigh, NC 27695-8208
Island-trapped waves, internal waves, and island circulation
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Island-trapped waves, internal waves, and island circulation T. M. Shaun Johnston Scripps Institution of Oceanography University
13.012: Hydrodynamics for Ocean Engineers
13.012: Hydrodynamics for Ocean Engineers Alexandra H. Techet Dept. of Ocean Engineering 9 September 2004 Lecture 1 What is Hydrodynamics? Hydrodynamics v. Aerodynamics Water is almost 1000 times denser
What is Hydrodynamics?
13.012: Hydrodynamics for Ocean Engineers Alexandra H. Techet Dept. of Ocean Engineering 9 September 2004 Lecture 1 What is Hydrodynamics? Hydrodynamics v. Aerodynamics Water is almost 1000 times denser
Louisiana s 2012 Coastal Master Plan BARRIER SHORELINE MORPHOLOGY MODEL
Louisiana Coastal Protection & Restorat coastal.louisiana.gov Louisiana s 2012 Coastal Master Plan PREDICTIVE MODELING: committed to our coast BARRIER SHORELINE MORPHOLOGY MODEL Dallon Weathers, University
JCOMM Wind Waves and Storm Surge Programme
9 th International Workshop on Wave Hindcasting and Forecasting Victoria, Canada, September 24-29, 2006 JCOMM Wind Waves and Storm Surge Programme Alice Soares Scientific Officer, Ocean Affairs Division
Tidal analysis and prediction of the flow characteristics around Abu Dhabi Island
Tidal analysis and prediction of the flow characteristics around Abu Dhabi Island K.A. Mohamed & M.E. El-Dahshan Research Center, Abu Dhabi Water and Electricity Authority Abstract In coastal seas and
RIP CURRENTS. Award # N
RIP CURRENTS Graham Symonds School of Geography and Oceanography University College, University of New South Wales, Australian Defence Force Academy, Canberra, 2600 AUSTRALIA Phone: 61-6-2688289 Fax: 61-6-2688313
An Atlas of Oceanic Internal Solitary Waves (February 2004) by Global Ocean Associates Prepared for Office of Naval Research Code 322 PO
Overview covers approximately 2200 km of coast from Kenya to the tip of Somalia (approximately 39 o E, 4 o S to 51 o E, 12 o N)(Figure 1). Internal wave activity has been observed in the area the near
Chapter - Oceans and Coasts
Chapter - Oceans and Coasts Discussion: What do oceans contribute to the environment of Earth? How do Earth s major systems relate to the oceans? Oceans and Coasts Oceans are important - Thermal regulation
LONG WAVE EFFECTS ON BREAKING WAVES OVER FRINGING REEFS
LONG WAVE EFFECTS ON BREAKING WAVES OVER FRINGING REEFS John T. Goertz 1, James M. Kaihatu, Alex Sheremet 3, Ernest R. Smith 4 and Jane M. Smith 5 Modeling of wave energy transformation and breaking on
Wave Modeling and Applications
Wave Modeling and Applications Hellenic Naval Academy Section of Mathematics Joint work with - Hellenic Navy Hydrographic Service - Atmospheric Modeling Group, Department of Physics, University of Athens,
David Wolcott Lijuan Huang Stephen Gill. Center for Operational Oceanographic Products and Services National Ocean Service/ NOAA Silver Spring, MD
Establishing Tide Control in an Area with Insufficient Observational Water Level Data: A Case Study of the Kuskokwim River, AK David Wolcott Lijuan Huang Stephen Gill Center for Operational Oceanographic
Wave research at Department of Oceanography, University of Hawai i
Wave research at Department of Oceanography, University of Hawai i Hawaii wave climate. Directional waverider buoys around Hawaii. Past and present wave-related research projects. Effect of tides on wave
Monitoring tidal movements in Cook Inlet, Alaska, using the integration of remote sensing data, GIS, and inundation models
Monitoring tidal movements in Cook Inlet, Alaska, using the integration of remote sensing data, GIS, and inundation models Hua Liu Department of political Science and Geography Old Dominion University
Hydrologic Feasibility of Storm Surge Barriers
Hydrologic Feasibility of Storm Surge Barriers Malcolm J. Bowman, School of Marine and Atmospheric Sciences State University of New York, Stony Brook, NY. Presented at Against the Deluge: Storm Surge Barriers
PhD student, January 2010-December 2013
Numerical modeling of wave current interactions ata a local scaleand and studyof turbulence closuremodel effects MARIA JOÃO TELES PhD student, January 2010-December 2013 Supervisor: António Pires-Silva,
ABSTRACT. KEY WORDS: coral reef, storm waves, infragravity waves, power plant, cooling water, field observation. INTRODUCTION FIELD OBSERVATION
M.W.L. Fluctuations Inside a Cooling Water Tank Set Inside a Coral Reef Julio Monroy Department of Civil Engineering, Kagoshima University -2-4 Korimoto, Kagoshima-shi, Japan 89-65 Ryuchiro Nishi, Michio
NYS Coastal Waters. Water Resources of NYS: THE NATURE of the COASTAL ZONE. NYS Coastal Waters. NYS Coastal Atlas. Coastal Zone Management 10/10/2014
Water Resources of NYS: THE NATURE of the COASTAL ZONE NYS Coastal Waters NYS is the only state to border the Atlantic Ocean and the Great Lakes (Lakes Erie and Ontario). Great Lakes shoreline: 577 miles
CALCULATIONS OF THE MOTIONS OF A SHIP MOORED WITH MOORMASTER UNITS
CALCULATIONS OF THE MOTIONS OF A SHIP MOORED WITH MOORMASTER UNITS By J. de Bont 1, W. van der Molen 2, J. van der Lem 3, H. Ligteringen 4, D. Mühlestein 5 and M. Howie 6 ABSTRACT Container ships should
Wave Energy Research and Applications
Wave Energy Research and Applications Shoreline and Shallows conference East Lansing, MI March 7, 2019 Photo: Dave Sanford Waves Background 1. Types of Waves 2. Good and Bad Waves 3. Restoration Impacts
The impacts of explicitly simulated gravity waves on large-scale circulation in the
The impacts of explicitly simulated gravity waves on large-scale circulation in the Southern Hemisphere. Linda Mudoni Department of Geological and Atmospheric Sciences October 2003 Introduction In the
Unit 11 Lesson 2 How Does Ocean Water Move? Copyright Houghton Mifflin Harcourt Publishing Company
Unit 11 Lesson 2 How Does Ocean Water Move? Catch a Wave A wave is the up-and-down movement of surface water. Catch a Wave Catch a Wave (wave effects) Surface waves are caused by wind pushing against
The Ike Dike. A Coastal Barrier Protecting the. Hurricane Storm Surge. Protecting the Houston/Galveston Region from Hurricane Storm Surge
The Ike Dike A Coastal Barrier Protecting the Houston/Galveston A Coastal Barrier Region from Hurricane Storm Surge Protecting the Houston/Galveston Region from Hurricane Storm Surge The Houston/Galveston
Chapter 10 Lecture Outline. The Restless Oceans
Chapter 10 Lecture Outline The Restless Oceans Focus Question 10.1 How does the Coriolis effect influence ocean currents? The Ocean s Surface Circulation Ocean currents Masses of water that flow from one
Theory and Application Introductory Oceanography Ray Rector: Instructor
OCEAN TIDES Theory and Application Introductory Oceanography Ray Rector: Instructor Tidal Concepts Tides are extremely swift, very long-wavelength, shallow-water waves Tides are periodic short-term changes
The Storm Surge Hazard 2018 TS-8 Tropical Meteorology 2
The Storm Surge Hazard 2018 TS-8 Tropical Meteorology 2 Daniel Noah National Weather Service Tampa Bay daniel.noah@noaa.gov Tropical Cyclone Storm Surge Is a large dome of water, often 50 to 100 miles
Evaluation of Unstructured WAVEWATCH III for Nearshore Application
Evaluation of Unstructured WAVEWATCH III for Nearshore Application Jane McKee Smith, Tyler Hesser, Mary Anderson Bryant USACE Research and Development Center, Coastal and Hydraulics Lab Aron Roland BGS
OCN 201 Tides. Tsunamis, Tides and other long waves
OCN 201 Tides Tsunamis, Tides and other long waves Storm surges Caused by winds and low atmospheric pressure associated with large storms Can raise sea surface by up to 25 ft, bottom contours magnify effect
INTRODUCTION TO COASTAL ENGINEERING
The University of the West Indies Organization of American States PROFESSIONAL DEVELOPMENT PROGRAMME: COASTAL INFRASTRUCTURE DESIGN, CONSTRUCTION AND MAINTENANCE A COURSE IN COASTAL DEFENSE SYSTEMS I CHAPTER
SCIENCE OF TSUNAMI HAZARDS
SCIENCE OF TSUNAMI HAZARDS ISSN 8755-6839 Journal of Tsunami Society International Volume 29 Number 3 2010 ESTIMATION OF EXPECTED MAXIMUM WATER LEVEL DUE TO TIDE AND TSUNAMI INTERACTION ALONG THE COASTAL
Equilibrium Model of Tides
Tides Outline Equilibrium Theory of Tides diurnal, semidiurnal and mixed semidiurnal tides spring and neap tides Dynamic Theory of Tides rotary tidal motion larger tidal ranges in coastal versus open-ocean
SCOUR AROUND OFFSHORE STRUCTURES - ANALYSIS OF FIELD MEASUREMENTS
SCOUR AROUND OFFSHORE STRUCTURES - ANALYSIS OF FIELD MEASUREMENTS D. RUDOLPH, K.J. BOS, A.P. LUIJENDIJK WL Delft Hydraulics, P.O. Box 177 2600 MH Delft, The Netherlands K. RIETEMA AJS V.o.F., Radarweg