Physical Oceanography

Slides:



Advertisements
Similar presentations
INTERNAL WAVE GENERATION, BREAKING, MIXING AND MODEL VALIDATION ALAN DAVIES (POL) JIUXING XING (POL) JARLE BERNTSEN (BERGEN)
Advertisements

Prof. dr. A. Achterberg, Astronomical Dept., IMAPP, Radboud Universiteit.
Physical Oceanography
EarthComm Fluids Pages Oceans of the World There are 4 large oceans on Earth (Atlantic, Pacific, Indian, Antarctic) All oceans have land borders.
Lithospheric Plates The lithosphere can be defined thermally by an isotherm at the base of the lithosphere which should be around 1350 o C. Mantle rocks.
Surface Gravity Waves-1 Knauss (1997), chapter-9, p Descriptive view (wave characteristics) Balance of forces, wave equation Dispersion relation.
Fluid Pumping Apparatuses Powered By Waves Or Flowing Currents
EE535: Renewable Energy: Systems, Technology & Economics Tidal (1)
9.2 Ocean Waves, Tides and Currents
Coastal Ocean Dynamics Baltic Sea Research Warnemünde
ORBITAL ELEMENTS. LaGrangian Points L2 Earth-Sun.
World’s largest meromictic basin. Strongly stratified. Deep waters do not mix with the surface. Buoyant fresh water caps the surface. Fresh water from.
Tsunamis and Tsunami Detection Systems December 1, 2010 Physical Oceanography Presentation Jeana Drake.
Physics of Tsunamis Part 3: Energy of Tsunamis. Review from last week  Energy: potential, kinetic, mechanical?  What kind of energy is originally created.
INTRODUCTION TO GENERAL OCEANOGRAPHY (GEOL 1033) “Few people stand at the edge of the sea without feeling awed by its size and power, and without wondering.
SIO 210: Eddies and mixing L. Talley Fall, 2014
Jiuxing Xing and Alan M. Davies
Converting Kinetic Energy Of Fluid Currents Into Electricity
Antarctic Circumpolar Current
The Cromwell Current and its effects on the Galapagos Islands
Weather. Climate Average weather conditions over time.
Alternative derivation of Sverdrup Relation Construct vorticity equation from geostrophic balance (1) (2)  Integrating over the whole ocean depth, we.
Waves and Water Dynamics
FIGURE 3.1 Values of density  t (curved lines) and the loci of maximum density and freezing point (at atmospheric pressure) for seawater as functions.
OCEN 201 Introduction to Ocean & Coastal Engineering Ocean Environment &Waves Jun Zhang
Physical Oceanography. RAP Barrier Island Major Oceans The three major oceans are : 1._______-largest, deepest, coldest, least salty. 2.__________-
Anatomy of a Wave A wave is the motion of a form that carries energy from one place to another The form is what moves, the material that the wave moves.
Internal Tide Generation Over a Continental Shelf Summer 2008 internship Gaёlle Faivre Flavien Gouillon, Alexandra Bozec Pr. Eric P. Chassignet.
Internal Gravity Waves
Internal Wave Interactions with Time-Dependent Critical Levels Brian Casaday and J. C. Vanderhoff Department of Mechanical Engineering Brigham Young University,
GG450 April 1, 2008 Huygen’s Principle and Snell’s Law.
Typical Mean Dynamic Balances in Estuaries Along-Estuary Component 1. Barotropic pressure gradient vs. friction Steady state, linear motion, no rotation,
Physical Oceanography Chapter 15. Major Oceans The three major oceans are : 1._______-largest, deepest, coldest, least salty. 2.__________- second largest,
Internal tides Seim, Edwards, Shay, Werner Some background SAB – generation site? Shelf observations Towards a climatology?
GEOGRAPHY OF THE OCEANS – from Knauss Chapter 1 Oceans cover ~70% of the surface area of the earth. The horizontal extent of ocean basins is huge in comparison.
Contributions to SST Anomalies in the Atlantic Ocean [Ocean Control of Air-Sea Heat Fluxes] Kathie Kelly Suzanne Dickinson and LuAnne Thompson University.
Oceanography 24 & 25 Ocean Zones TidesOcean Water Elements Grab bag
Oceanography. How much of the Earth’s surface is water?
LEO PAN PHYSICS 420 OUTREACH PROGRAM DEPARTMENT OF PHYSICS AND ASTRONOMY UNIVERSITY OF B.C. An Introduction to Tsunami.
OEAS 604: Introduction to Physical Oceanography Conservation of Mass Chapter 4 – Knauss Chapter 5 – Talley et al. 1.
Physical and Chemical Oceanography Part 1: Chemistry.
The acc and Primary production in the southern ocean
Earth and Space Grade 10 ST What is the Hydrosphere? The Hydrosphere is the Earth’s outer layer of water- including water in its solid, liquid and.
Earth and Space Grade 10 ST What is the Hydrosphere? The Hydrosphere is the Earth’s outer layer of water- including water in its solid, liquid and.
Ocean Waves Scripps Classroom Connection Scripps GK-12 Classroom Connection.
Physical Oceanography Surface Gravity Waves Properties Dispersion Refraction & Diffraction Group velocity Generation Assignment: Read Chapter 16 of Stewart:
1 Oscillating motions in the stable atmosphere of a deep valley Y. Largeron 1, C. Staquet 1 and C. Chemel 2 1. LEGI, Grenoble, France 2. NCAS-Weather,
Antarctic Circumpolar Current (ACC) By: Marie McCrary.
Thermocline & Pycnocline
Reynolds Number (Re) Viscosity: resistance of a liquid to change of form. Inertia: resistance of an object (body) to a change in its state of motion.
Estuarine Variability
Waves and Water Dynamics
Check for Understanding
MEE …. WAVE PROPAGATION IN SOLIDS
Waves.
Tsunamis and Tsunami Detection Systems
Waves Page 49 in Notebook.
Wave Energy.
Waves, Currents, and Tides (S6E.3.d)
Phase Velocity & Group Velocity.
Waves in the Ocean.
Section 3: Ocean Movements
Values of density st (curved lines) and the loci of maximum density and freezing point (at atmospheric pressure) for seawater as functions of temperature.
Oceanography.
Nonlinear effects in internal waves
Ocean Movements 15.3.
Unit 5 Review Earth Science
Waves and Tides Earth Science 6th Grade.
Oceanography.
Physical Oceanography
Presentation transcript:

Physical Oceanography Internal Waves http://myweb.dal.ca/kelley/SLEIWEX/gallery/ISW_large.jpg Mike Brown Physical Oceanography Fall 2014

Waves form at the interface between fluids of different densities. Tank demo: note the slow speed and large amplitude of the internal wave. https://www.youtube.com/watch?v=TxdiU3LJlZ8

Long wave approximation: (similar to shallow waves). Internal waves typically have slow velocities and large amplitudes. Density Depth Karp-Boss et al. (2009)

Frequency is bounded by f and N (horizontal/vertical group velocity). When the ocean is continuously stratified, the direction of wave propagation is dependent on frequency. Frequency is bounded by f and N (horizontal/vertical group velocity). Group velocity can be in a different direction than phase velocity. Density Depth Knauss (2005)

A dominant source of ocean mixing. Generated primarily by 1) tidal flow over seafloor topography, 2) wind. A dominant source of ocean mixing. Jayne et al. (2004)

Internal waves can be detected at the sea surface. Knauss (2005) http://earthobservatory.nasa.gov/IOTD/view.php?id=44567

References: Alford, M. H., MacKinnon, J. A., Zhao, Z., Pinkel, R., Klymak, J., & Peacock, T. (2007). Internal waves across the Pacific. Geophysical Research Letters, 34(24). Franks, P. J., & Franks, S. E. (2009). Hands-on oceanography: Mix it up, mix it down: Intriguing implications of ocean layering. Oceanography, 22(1), 228. Jayne, S. R., Laurent, L. C. S., & Gille, S. T. (2004). Connections Between Ocean Bottom Topography and Earth’s Climate. Oceanography, 17(1). Karp-Boss, L., Boss, E., Weller, H., Loftin, J., & Albright, J. (2009). Teaching Physical Concepts in Oceanography: An Inquiry Based Approach. Oceanography, 22(3). Knauss, J. A. (2005). Introduction to physical oceanography. Waveland Press, Inc.. Kundu, P. K. (1990). Fluid Mechanics. Academic Press, Inc.. St Laurent, L., Alford, M. H., & Paluszkiewicz, T. (2012). An introduction to the special issue on internal waves. Oceanography, 25(2), 15-19. http://myweb.dal.ca/kelley/SLEIWEX/gallery/ISW_large.jpg http://earthobservatory.nasa.gov/IOTD/view.php?id=44567 https://www.youtube.com/watch?v=TxdiU3LJlZ8