Introduction to Geophysical Fluid Dynamics

Size: px
Start display at page:

Download "Introduction to Geophysical Fluid Dynamics"

Transcription

1 Introduction to Geophysical Fluid Dynamics BENOIT CUSHMAN-ROISIN Dartmouth College Prentice Hall Prentice Hall, Upper Saddle River, New Jersey 07458

2 Contents Preface xiii PART I FUNDAMENTALS I Introduction 1-1 Objective Importance of Geophysical Fluid Dynamics Distinguishing Attributes of Geophysical Fluid Dynamics Scales of Motion 5

3 1-5 Importance of Rotation Importance of Stratification Important Distinctions between the Atmosphere and Oceans General Remarks on Data Acquisition 12 Problems 13 Suggested Laboratory Demonstration 14 Historical Note: Walsh Cottage 15 The Coriolis Force 2-1 Motivation for the Choice of a Rotating Reference Framework Rotating Frame of Reference Unimportance of the Centrifugal Force Motion of a Free Particle on a Rotating Plane Analogy with a Pendulum Acceleration on a Three-Dimensional Rotating Earth 27 Problems 29 Suggested Laboratory Demonstrations 31 Biography: Gaspard Gustave de Coriolis 32 The Governing Equations 3-1 Momentum Equations Other Governing Equations The Boussinesq Approximation Further Simplifications Recapitulation of the Equations Governing Geophysical Flows The Rossby and Ekman Numbers 44 Problems 45 Biography: Carl-Gustaf Arvid Rossby 47

4 Contents vii PART II ROTATION EFFECTS 4 Geostrophic Flows and Vorticity Dynamics Homogeneous Geostrophic Flows Homogeneous Geostrophic Flows over an Irregular Bottom Generalization to Nongeostrophic Flows Vorticity Dynamics 56 Problems 58 Suggested Laboratory Demonstration 60 Biography: Geoffrey Ingram Taylor 61 5 The Ekman Layer On the Importance of Friction The Bottom Ekman Layer Generalization to Nonuniform Currents The Surface Ekman Layer The Ekman Layer over Uneven Terrain The Ekman Layer in Real Geophysical Flows 72 Problems 74 Suggested Laboratory Demonstration 75 Biography: Vagn Walfrid Ekman 76 6 Linear Barotropic Waves Linear Wave Dynamics The Kelvin Wave Inertia-Gravity Waves (Poincare Waves) Planetary Waves (Rossby Waves) Topographic Waves Analogy between Planetary and Topographic Waves 91

5 VIM Contents Problems 93 Suggested Laboratory Demonstration 94 Biography: William Thomson, Lord Kelvin 95 7 Barotropic Instability Introduction Waves on a Shear Flow Bounds on Wave Speeds and Growth Rates A Simple Example 103 Problems 106 Biography: Louis Norberg Howard Large-Scale Ocean Circulation Some Remarks on the Ocean and Atmosphere A Simple Model of Midlatitude Circulation Sverdrup Transport Westward Intensification Discussion 118 Problems 119 Suggested Laboratory Demonstration 119 Biography: Harald Ulrik Sverdrup 121 Biography: Henry Melson Stommel 122 PART III STRATIFICATION EFFECTS 9 Stratification Introduction Static Stability A Note on Atmospheric Stratification The Importance of Stratification: The Froude Number 129

6 Contents ix 9-5 Combination of Rotation and Stratification 132 Problems 134 Suggested Laboratory Demonstration 134 Biography: David Brunt 135 I 0 Internal Waves From Surface to Internal Waves Internal-Wave Theory Structure of an Internal Wave Lee Waves A Note on Nonlinear Effects A Note on Shear Effects 148 Problems 148 Suggested Laboratory Demonstration 149 Biography: Walter Heinrich Munk 150 I I Turbulence in Stratified Fluids Mixing of Stratified Fluids Instability of a Stratified Shear Flow Turbulence in a Stratified Shear Flow Convection 762 Problems 766 Suggested Laboratory Demonstration 767 Biography: Lewis Fry Richardson 168 PART IV COMBINED ROTATION AND STRATIFICATION EFFECTS I 2. Layered Models From Depth to Density 769 i

7 X Contents 12-2 Potential Vorticity Layered Models 174 Problems 179 Biography: Raymond Braislin Montgomery 180 I 3 Stratified Geostrophic Dynamics Thermal Wind Geostrophic Adjustment Energetics of Geostrophic Adjustment 187 Problems 189 Suggested Laboratory Demonstration 191 Biography: George Veronis Upwelling The Upwelling Process A Simple Model of Coastal Upwelling Finite-Amplitude Upwelling Variability of the Upwelling Front 799 Problems 200 Biography: Kozo Yoshida 203 I 5 Quasi-Geostrophic Dynamics Simplifying Assumption Governing Equation Discussion Energetics Planetary Waves in a Stratified Fluid Some Nonlinear Effects 279 Problems 223 Biography: Jule Gregory Charney 224

8 Contents XI I 6 Barolinic Instability Cause for Instability Linear Theory Heat Transport More-General Criteria 234 Problems 237 Suggested Laboratory Demonstration 237 Biography: Joseph Pedlosky 239 I 7 Fronts, Jets, and Vortices Fronts and Jets Vortices Geostrophic Turbulence 259 Problems 267 Suggested Laboratory Demonstrations 263 Biography: Melvin Ernest Stern 264 Biography: Allan Richard Robinson 265 PART V SPECIAL TOPICS I 8 Climate Dynamics Climate versus Weather Global Heat Budget General Atmospheric Circulation The Ocean as a Regulator Greenhouse Effect 278 Problems 281 Suggested Laboratory Demonstration 282 Biography: Syukuro Manabe 283

9 xii Contents I 9 Equatorial Dynamics Equatorial Beta Plane Linear Wave Theory El Nino 290 Problems 292 Biography: Adrian Edmund Gill 293 Appendix A: Wave Kinematics 294 A-l Wave Number and Wavelength 294 A-2 Frequency, Phase Speed, and Dispersion 296 A-3 Group Velocity and Energy Propagation 299 Problems 301 Suggested Computer Demonstration 302 References 303 Index 313

Contents. Parti Fundamentals. 1. Introduction. 2. The Coriolis Force. Preface Preface of the First Edition

Contents. Parti Fundamentals. 1. Introduction. 2. The Coriolis Force. Preface Preface of the First Edition Foreword Preface Preface of the First Edition xiii xv xvii Parti Fundamentals 1. Introduction 1.1 Objective 3 1.2 Importance of Geophysical Fluid Dynamics 4 1.3 Distinguishing Attributes of Geophysical

More information

ATMOSPHERIC AND OCEANIC FLUID DYNAMICS

ATMOSPHERIC AND OCEANIC FLUID DYNAMICS ATMOSPHERIC AND OCEANIC FLUID DYNAMICS Fundamentals and Large-scale Circulation G E O F F R E Y K. V A L L I S Princeton University, New Jersey CAMBRIDGE UNIVERSITY PRESS An asterisk indicates more advanced

More information

INTERNAL GRAVITY WAVES

INTERNAL GRAVITY WAVES INTERNAL GRAVITY WAVES B. R. Sutherland Departments of Physics and of Earth&Atmospheric Sciences University of Alberta Contents Preface List of Tables vii xi 1 Stratified Fluids and Waves 1 1.1 Introduction

More information

Atmospheric Dynamics Fall 2008

Atmospheric Dynamics Fall 2008 Atmospheric Dynamics Fall 2008 AT601, the first semester of Atmospheric Dynamics, is based on the course notes available over the web and on the highly recommended texts listed below. The course notes

More information

Goals of this Chapter

Goals of this Chapter Waves in the Atmosphere and Oceans Restoring Force Conservation of potential temperature in the presence of positive static stability internal gravity waves Conservation of potential vorticity in the presence

More information

Atmosphere, Ocean and Climate Dynamics Fall 2008

Atmosphere, Ocean and Climate Dynamics Fall 2008 MIT OpenCourseWare http://ocw.mit.edu 12.003 Atmosphere, Ocean and Climate Dynamics Fall 2008 For information about citing these materials or our Terms of Use, visit: http://ocw.mit.edu/terms. Contents

More information

Dynamics and Kinematics

Dynamics and Kinematics Geophysics Fluid Dynamics () Syllabus Course Time Lectures: Tu, Th 09:30-10:50 Discussion: 3315 Croul Hall Text Book J. R. Holton, "An introduction to Dynamic Meteorology", Academic Press (Ch. 1, 2, 3,

More information

Geophysics Fluid Dynamics (ESS228)

Geophysics Fluid Dynamics (ESS228) Geophysics Fluid Dynamics (ESS228) Course Time Lectures: Tu, Th 09:30-10:50 Discussion: 3315 Croul Hall Text Book J. R. Holton, "An introduction to Dynamic Meteorology", Academic Press (Ch. 1, 2, 3, 4,

More information

OCN660 - Ocean Waves. Course Purpose & Outline. Doug Luther. OCN660 - Syllabus. Instructor: x65875

OCN660 - Ocean Waves. Course Purpose & Outline. Doug Luther. OCN660 - Syllabus. Instructor: x65875 OCN660 - Ocean Waves Course Purpose & Outline Instructor: Doug Luther dluther@hawaii.edu x65875 This introductory course has two objectives: to survey the principal types of linear ocean waves; and, to

More information

Synoptic-Dynamic Meteorology in Midlatitudes

Synoptic-Dynamic Meteorology in Midlatitudes Synoptic-Dynamic Meteorology in Midlatitudes VOLUME II Observations and Theory of Weather Systems HOWARD B. BLUESTEIN New York Oxford OXFORD UNIVERSITY PRESS 1993 Contents 1. THE BEHAVIOR OF SYNOPTIC-SCALE,

More information

An Introduction to Atmospheric Physics

An Introduction to Atmospheric Physics An Introduction to Atmospheric Physics David G. Andrews CAMBRIDGE UNIVERSITY PRESS Contents Preface ix 1 Introduction 1 1.1 The atmosphere as a physical System 1 1.2 Atmospheric modeis 4 1.3 Two simple

More information

Gravity Waves. Lecture 5: Waves in Atmosphere. Waves in the Atmosphere and Oceans. Internal Gravity (Buoyancy) Waves 2/9/2017

Gravity Waves. Lecture 5: Waves in Atmosphere. Waves in the Atmosphere and Oceans. Internal Gravity (Buoyancy) Waves 2/9/2017 Lecture 5: Waves in Atmosphere Perturbation Method Properties of Wave Shallow Water Model Gravity Waves Rossby Waves Waves in the Atmosphere and Oceans Restoring Force Conservation of potential temperature

More information

8/21/08. Modeling the General Circulation of the Atmosphere. Topic 4: Equatorial Wave Dynamics. Moisture and Equatorial Waves

8/21/08. Modeling the General Circulation of the Atmosphere. Topic 4: Equatorial Wave Dynamics. Moisture and Equatorial Waves Modeling the General Circulation of the Atmosphere. Topic 4: Equatorial Wave Dynamics D A R G A N M. W. F R I E R S O N U N I V E R S I T Y O F W A S H I N G T O N, D E P A R T M E N T O F A T M O S P

More information

Note that Rossby waves are tranverse waves, that is the particles move perpendicular to the direction of propagation. f up, down (clockwise)

Note that Rossby waves are tranverse waves, that is the particles move perpendicular to the direction of propagation. f up, down (clockwise) Ocean 423 Rossby waves 1 Rossby waves: Restoring force is the north-south gradient of background potential vorticity (f/h). That gradient can be due to either the variation in f with latitude, or to a

More information

Model equations for planetary and synoptic scale atmospheric motions associated with different background stratification

Model equations for planetary and synoptic scale atmospheric motions associated with different background stratification Model equations for planetary and synoptic scale atmospheric motions associated with different background stratification Stamen Dolaptchiev & Rupert Klein Potsdam Institute for Climate Impact Research

More information

Nonlinear Balance on an Equatorial Beta Plane

Nonlinear Balance on an Equatorial Beta Plane Nonlinear Balance on an Equatorial Beta Plane David J. Raymond Physics Department and Geophysical Research Center New Mexico Tech Socorro, NM 87801 April 26, 2009 Summary Extension of the nonlinear balance

More information

Baroclinic Rossby waves in the ocean: normal modes, phase speeds and instability

Baroclinic Rossby waves in the ocean: normal modes, phase speeds and instability Baroclinic Rossby waves in the ocean: normal modes, phase speeds and instability J. H. LaCasce, University of Oslo J. Pedlosky, Woods Hole Oceanographic Institution P. E. Isachsen, Norwegian Meteorological

More information

Ocean Dynamics. The Great Wave off Kanagawa Hokusai

Ocean Dynamics. The Great Wave off Kanagawa Hokusai Ocean Dynamics The Great Wave off Kanagawa Hokusai LO: integrate relevant oceanographic processes with factors influencing survival and growth of fish larvae Physics Determining Ocean Dynamics 1. Conservation

More information

Atmosphere, Ocean, Climate Dynamics: the Ocean Circulation EESS 146B/246B

Atmosphere, Ocean, Climate Dynamics: the Ocean Circulation EESS 146B/246B Atmosphere, Ocean, Climate Dynamics: the Ocean Circulation EESS 146B/246B Instructor: Leif Thomas TA: Gonçalo Zo Zo Gil http://pangea.stanford.edu/courses/eess146bweb/ Course Objectives Identify and characterize

More information

Chapter 9. Geostrophy, Quasi-Geostrophy and the Potential Vorticity Equation

Chapter 9. Geostrophy, Quasi-Geostrophy and the Potential Vorticity Equation Chapter 9 Geostrophy, Quasi-Geostrophy and the Potential Vorticity Equation 9.1 Geostrophy and scaling. We examined in the last chapter some consequences of the dynamical balances for low frequency, nearly

More information

Contents. I Introduction 1. Preface. xiii

Contents. I Introduction 1. Preface. xiii Contents Preface xiii I Introduction 1 1 Continuous matter 3 1.1 Molecules................................ 4 1.2 The continuum approximation.................... 6 1.3 Newtonian mechanics.........................

More information

Symmetric Instability and Rossby Waves

Symmetric Instability and Rossby Waves Chapter 8 Symmetric Instability and Rossby Waves We are now in a position to begin investigating more complex disturbances in a rotating, stratified environment. Most of the disturbances of interest are

More information

Lecture 1 ATS 601. Thomas Birner, CSU. ATS 601 Lecture 1

Lecture 1 ATS 601. Thomas Birner, CSU. ATS 601 Lecture 1 Lecture 1 ATS 601 Thomas Birner, CSU About your Instructor: Thomas Birner Assistant Professor, joined CSU 10/2008 M.Sc. Physics (Condensed Matter Theory), U of Leipzig, Germany Ph.D. Atmospheric Science

More information

Exam Questions & Problems

Exam Questions & Problems 1 Exam Questions & Problems Summer School on Dynamics of the North Indian Ocean National Institute of Oceanography, Dona Paula, Goa General topics that have been considered during this course are indicated

More information

Introduction to Physical Oceanography and Climate Spring 2018 FAS course web page for EPS 131

Introduction to Physical Oceanography and Climate Spring 2018 FAS course web page for EPS 131 Introduction to Physical Oceanography and Climate Spring 2018 FAS course web page for EPS 131 Field trip to the Woods Hole Oceanographic Institution, spring 2018. Instructor: Eli Tziperman, office hours:

More information

Ocean currents: some misconceptions and some dynamics

Ocean currents: some misconceptions and some dynamics Ocean currents: some misconceptions and some dynamics Joe LaCasce Dept. Geosciences October 30, 2012 Where is the Gulf Stream? BBC Weather Center Where is the Gulf Stream? Univ. Bergen news website (2011)

More information

The general circulation: midlatitude storms

The general circulation: midlatitude storms The general circulation: midlatitude storms Motivation for this class Provide understanding basic motions of the atmosphere: Ability to diagnose individual weather systems, and predict how they will change

More information

Inertia-gravity wave generation: a WKB approach. Jonathan Maclean Aspden

Inertia-gravity wave generation: a WKB approach. Jonathan Maclean Aspden Inertia-gravity wave generation: a WKB approach Jonathan Maclean Aspden Doctor of Philosophy University of Edinburgh 2010 Declaration I declare that this thesis was composed by myself and that the work

More information

1/27/2010. With this method, all filed variables are separated into. from the basic state: Assumptions 1: : the basic state variables must

1/27/2010. With this method, all filed variables are separated into. from the basic state: Assumptions 1: : the basic state variables must Lecture 5: Waves in Atmosphere Perturbation Method With this method, all filed variables are separated into two parts: (a) a basic state part and (b) a deviation from the basic state: Perturbation Method

More information

Lecture 14. Equations of Motion Currents With Friction Sverdrup, Stommel, and Munk Solutions Remember that Ekman's solution for wind-induced transport

Lecture 14. Equations of Motion Currents With Friction Sverdrup, Stommel, and Munk Solutions Remember that Ekman's solution for wind-induced transport Lecture 14. Equations of Motion Currents With Friction Sverdrup, Stommel, and Munk Solutions Remember that Ekman's solution for wind-induced transport is which can also be written as (14.1) i.e., #Q x,y

More information

Eddies, Waves, and Friction: Understanding the Mean Circulation in a Barotropic Ocean Model

Eddies, Waves, and Friction: Understanding the Mean Circulation in a Barotropic Ocean Model Eddies, Waves, and Friction: Understanding the Mean Circulation in a Barotropic Ocean Model Baylor Fox-Kemper Atmospheric and Oceanic Sciences Program, Princeton University and NOAA Climate and Global

More information

Internal boundary layers in the ocean circulation

Internal boundary layers in the ocean circulation Internal boundary layers in the ocean circulation Lecture 9 by Andrew Wells We have so far considered boundary layers adjacent to physical boundaries. However, it is also possible to find boundary layers

More information

ATMOSPHERIC SCIENCE-ATS (ATS)

ATMOSPHERIC SCIENCE-ATS (ATS) Atmospheric Science-ATS (ATS) 1 ATMOSPHERIC SCIENCE-ATS (ATS) Courses ATS 150 Science of Global Climate Change Credits: 3 (3-0-0) Physical basis of climate change. Energy budget of the earth, the greenhouse

More information

Equatorially trapped waves. Shayne McGregor ARC Postdoctoral Fellow CCRC & ARC CSS, UNSW. Climate Change. Research Centre

Equatorially trapped waves. Shayne McGregor ARC Postdoctoral Fellow CCRC & ARC CSS, UNSW. Climate Change. Research Centre Equatorially trapped waves Shayne McGregor ARC Postdoctoral Fellow CCRC & ARC CSS, UNSW Climate Change Research Centre Equatorially trapped waves The linear SWM Equatorial Kelvin waves Other equatorially

More information

Q.1 The most abundant gas in the atmosphere among inert gases is (A) Helium (B) Argon (C) Neon (D) Krypton

Q.1 The most abundant gas in the atmosphere among inert gases is (A) Helium (B) Argon (C) Neon (D) Krypton Q. 1 Q. 9 carry one mark each & Q. 10 Q. 22 carry two marks each. Q.1 The most abundant gas in the atmosphere among inert gases is (A) Helium (B) Argon (C) Neon (D) Krypton Q.2 The pair of variables that

More information

196 7 atmospheric oscillations:

196 7 atmospheric oscillations: 196 7 atmospheric oscillations: 7.4 INTERNAL GRAVITY (BUOYANCY) WAVES We now consider the nature of gravity wave propagation in the atmosphere. Atmospheric gravity waves can only exist when the atmosphere

More information

Jet Formation in the Equatorial Oceans Through Barotropic and Inertial Instabilities. Mark Fruman

Jet Formation in the Equatorial Oceans Through Barotropic and Inertial Instabilities. Mark Fruman p. 1/24 Jet Formation in the Equatorial Oceans Through Barotropic and Inertial Instabilities Mark Fruman Bach Lien Hua, Richard Schopp, Marc d Orgeville, Claire Ménesguen LPO IFREMER, Brest, France IAU

More information

Stability of meridionally-flowing grounded abyssal currents in the ocean

Stability of meridionally-flowing grounded abyssal currents in the ocean Advances in Fluid Mechanics VII 93 Stability of meridionally-flowing grounded abyssal currents in the ocean G. E. Swaters Applied Mathematics Institute, Department of Mathematical & Statistical Sciences

More information

Geostrophic and Quasi-Geostrophic Balances

Geostrophic and Quasi-Geostrophic Balances Geostrophic and Quasi-Geostrophic Balances Qiyu Xiao June 19, 2018 1 Introduction Understanding how the atmosphere and ocean behave is important to our everyday lives. Techniques such as weather forecasting

More information

For example, for values of A x = 0 m /s, f 0 s, and L = 0 km, then E h = 0. and the motion may be influenced by horizontal friction if Corioli

For example, for values of A x = 0 m /s, f 0 s, and L = 0 km, then E h = 0. and the motion may be influenced by horizontal friction if Corioli Lecture. Equations of Motion Scaling, Non-dimensional Numbers, Stability and Mixing We have learned how to express the forces per unit mass that cause acceleration in the ocean, except for the tidal forces

More information

ESCI 343 Atmospheric Dynamics II Lesson 11 - Rossby Waves

ESCI 343 Atmospheric Dynamics II Lesson 11 - Rossby Waves ESCI 343 Atmospheric Dynamics II Lesson 11 - Rossby Waves Reference: An Introduction to Dynamic Meteorology (4 rd edition), J.R. Holton Atmosphere-Ocean Dynamics, A.E. Gill Fundamentals of Atmospheric

More information

Rotating stratified turbulence in the Earth s atmosphere

Rotating stratified turbulence in the Earth s atmosphere Rotating stratified turbulence in the Earth s atmosphere Peter Haynes, Centre for Atmospheric Science, DAMTP, University of Cambridge. Outline 1. Introduction 2. Momentum transport in the atmosphere 3.

More information

BALANCED FLOW: EXAMPLES (PHH lecture 3) Potential Vorticity in the real atmosphere. Potential temperature θ. Rossby Ertel potential vorticity

BALANCED FLOW: EXAMPLES (PHH lecture 3) Potential Vorticity in the real atmosphere. Potential temperature θ. Rossby Ertel potential vorticity BALANCED FLOW: EXAMPLES (PHH lecture 3) Potential Vorticity in the real atmosphere Need to introduce a new measure of the buoyancy Potential temperature θ In a compressible fluid, the relevant measure

More information

SAMPLE CHAPTERS UNESCO EOLSS WAVES IN THE OCEANS. Wolfgang Fennel Institut für Ostseeforschung Warnemünde (IOW) an der Universität Rostock,Germany

SAMPLE CHAPTERS UNESCO EOLSS WAVES IN THE OCEANS. Wolfgang Fennel Institut für Ostseeforschung Warnemünde (IOW) an der Universität Rostock,Germany WAVES IN THE OCEANS Wolfgang Fennel Institut für Ostseeforschung Warnemünde (IOW) an der Universität Rostock,Germany Keywords: Wind waves, dispersion, internal waves, inertial oscillations, inertial waves,

More information

OCN/ATM/ESS 587. The wind-driven ocean circulation. Friction and stress. The Ekman layer, top and bottom. Ekman pumping, Ekman suction

OCN/ATM/ESS 587. The wind-driven ocean circulation. Friction and stress. The Ekman layer, top and bottom. Ekman pumping, Ekman suction OCN/ATM/ESS 587 The wind-driven ocean circulation. Friction and stress The Ekman layer, top and bottom Ekman pumping, Ekman suction Westward intensification The wind-driven ocean. The major ocean gyres

More information

The Martian Climate Revisited

The Martian Climate Revisited Peter L. Read and Stephen R. Lewis The Martian Climate Revisited Atmosphere and Environment of a Desert Planet Springer Published in association with Praxis Publishing Chichester, UK Contents Preface Abbreviations

More information

2. Baroclinic Instability and Midlatitude Dynamics

2. Baroclinic Instability and Midlatitude Dynamics 2. Baroclinic Instability and Midlatitude Dynamics Midlatitude Jet Stream Climatology (Atlantic and Pacific) Copyright 26 Emily Shuckburgh, University of Cambridge. Not to be quoted or reproduced without

More information

The Planetary Circulation System

The Planetary Circulation System 12 The Planetary Circulation System Learning Goals After studying this chapter, students should be able to: 1. describe and account for the global patterns of pressure, wind patterns and ocean currents

More information

Prototype Instabilities

Prototype Instabilities Prototype Instabilities David Randall Introduction Broadly speaking, a growing atmospheric disturbance can draw its kinetic energy from two possible sources: the kinetic and available potential energies

More information

( ) (9.1.1) Chapter 9. Geostrophy, Quasi-Geostrophy and the Potential Vorticity Equation. 9.1 Geostrophy and scaling.

( ) (9.1.1) Chapter 9. Geostrophy, Quasi-Geostrophy and the Potential Vorticity Equation. 9.1 Geostrophy and scaling. Chapter 9 Geostrophy, Quasi-Geostrophy and the Potential Vorticity Equation 9.1 Geostrophy and scaling. We examined in the last chapter some consequences of the dynamical balances for low frequency, nearly

More information

Joseph Pedlosky Senior Scientist Emeritus Department of Physical Oceanography Woods Hole Oceanographic Institution. Education

Joseph Pedlosky Senior Scientist Emeritus Department of Physical Oceanography Woods Hole Oceanographic Institution. Education Joseph Pedlosky Senior Scientist Emeritus Department of Physical Oceanography Woods Hole Oceanographic Institution Education B.Sc., Massachusetts Institute of Technology, 1960 M.Sc., Massachusetts Institute

More information

Stratospheric Dynamics and Coupling with Troposphere and Mesosphere

Stratospheric Dynamics and Coupling with Troposphere and Mesosphere WDS'13 Proceedings of Contributed Papers, Part III, 6 66, 13. ISBN 978-8-7378-5-8 MATFYZPRESS Stratospheric Dynamics and Coupling with Troposphere and Mesosphere P. Šácha Charles University in Prague,

More information

7 Balanced Motion. 7.1 Return of the...scale analysis for hydrostatic balance! CSU ATS601 Fall 2015

7 Balanced Motion. 7.1 Return of the...scale analysis for hydrostatic balance! CSU ATS601 Fall 2015 7 Balanced Motion We previously discussed the concept of balance earlier, in the context of hydrostatic balance. Recall that the balanced condition means no accelerations (balance of forces). That is,

More information

ESCI 110: 2 s.h. Introduction to Earth Sciences Programs ESCI 322: 3 s.h. Environmental Hydrology ESCI 241: 4 s.h. Meteorology (G2, L)

ESCI 110: 2 s.h. Introduction to Earth Sciences Programs ESCI 322: 3 s.h. Environmental Hydrology ESCI 241: 4 s.h. Meteorology (G2, L) ESCI 110: 2 s.h. Introduction to Earth Sciences Programs General introduction to each of the earth sciences disciplines and to college life. 2 hrs. lec. Offered in fall. Restricted to earth sciences majors.

More information

Lecture 8. Lecture 1. Wind-driven gyres. Ekman transport and Ekman pumping in a typical ocean basin. VEk

Lecture 8. Lecture 1. Wind-driven gyres. Ekman transport and Ekman pumping in a typical ocean basin. VEk Lecture 8 Lecture 1 Wind-driven gyres Ekman transport and Ekman pumping in a typical ocean basin. VEk wek > 0 VEk wek < 0 VEk 1 8.1 Vorticity and circulation The vorticity of a parcel is a measure of its

More information

Boundary Layers: Homogeneous Ocean Circulation

Boundary Layers: Homogeneous Ocean Circulation Boundary Layers: Homogeneous Ocean irculation Lecture 7 by Angel Ruiz-Angulo The first explanation for the western intensification of the wind-driven ocean circulation was provided by Henry Stommel (948).

More information

SIO 210: Dynamics VI (Potential vorticity) L. Talley Fall, 2014 (Section 2: including some derivations) (this lecture was not given in 2015)

SIO 210: Dynamics VI (Potential vorticity) L. Talley Fall, 2014 (Section 2: including some derivations) (this lecture was not given in 2015) SIO 210: Dynamics VI (Potential vorticity) L. Talley Fall, 2014 (Section 2: including some derivations) (this lecture was not given in 2015) Variation of Coriolis with latitude: β Vorticity Potential vorticity

More information

4 (1973, Rossby), 1962, (American Mete2. orological Society), ( Rayleigh),

4 (1973, Rossby), 1962, (American Mete2. orological Society), ( Rayleigh), 64 4 2 0 0 6 8 ACTA METEOROLO GICA SIN ICA Vol. 64 No. 4 August 2006 Ξ 1 2 3 4 1 210093 2 230026 3 210044 4 100081 2006 5 6 91 70 : 6 1 4 (1973 1979 1986 1992 1915 2 7 ) 1979 1929 1937 ( ) 1945 Rossby

More information

Lecture 9: Tidal Rectification, Stratification and Mixing

Lecture 9: Tidal Rectification, Stratification and Mixing Lecture 9: Tidal Rectification, Stratification and Mixing Chris Garrett 1 Additional Notes on Tidal Rectification This lecture continues the discussion of long-wavelength tidal flow over comparatively

More information

2.5 Shallow water equations, quasigeostrophic filtering, and filtering of inertia-gravity waves

2.5 Shallow water equations, quasigeostrophic filtering, and filtering of inertia-gravity waves Chapter. The continuous equations φ=gh Φ=gH φ s =gh s Fig..5: Schematic of the shallow water model, a hydrostatic, incompressible fluid with a rigid bottom h s (x,y), a free surface h(x,y,t), and horizontal

More information

Turbulence. 2. Reynolds number is an indicator for turbulence in a fluid stream

Turbulence. 2. Reynolds number is an indicator for turbulence in a fluid stream Turbulence injection of a water jet into a water tank Reynolds number EF$ 1. There is no clear definition and range of turbulence (multi-scale phenomena) 2. Reynolds number is an indicator for turbulence

More information

Measurement of Rotation. Circulation. Example. Lecture 4: Circulation and Vorticity 1/31/2017

Measurement of Rotation. Circulation. Example. Lecture 4: Circulation and Vorticity 1/31/2017 Lecture 4: Circulation and Vorticity Measurement of Rotation Circulation Bjerknes Circulation Theorem Vorticity Potential Vorticity Conservation of Potential Vorticity Circulation and vorticity are the

More information

Fundamentals of Weather and Climate

Fundamentals of Weather and Climate Fundamentals of Weather and Climate ROBIN McILVEEN Environmental Science Division Institute of Environmental and Biological Sciences Lancaster University CHAPMAN & HALL London Glasgow Weinheim New York

More information

Ocean dynamics: the wind-driven circulation

Ocean dynamics: the wind-driven circulation Ocean dynamics: the wind-driven circulation Weston Anderson March 13, 2017 Contents 1 Introduction 1 2 The wind driven circulation (Ekman Transport) 3 3 Sverdrup flow 5 4 Western boundary currents (western

More information

2/15/2012. Earth System Science II EES 717 Spring 2012

2/15/2012. Earth System Science II EES 717 Spring 2012 Earth System Science II EES 717 Spring 2012 1. The Earth Interior Mantle Convection & Plate Tectonics 2. The Atmosphere - Climate Models, Climate Change and Feedback Processes 3. The Oceans Circulation;

More information

Thermohaline and wind-driven circulation

Thermohaline and wind-driven circulation Thermohaline and wind-driven circulation Annalisa Bracco Georgia Institute of Technology School of Earth and Atmospheric Sciences NCAR ASP Colloquium: Carbon climate connections in the Earth System Tracer

More information

Transformed Eulerian Mean

Transformed Eulerian Mean Chapter 15 Transformed Eulerian Mean In the last few lectures we introduced some fundamental ideas on 1) the properties of turbulent flows in rotating stratified environments, like the ocean and the atmosphere,

More information

The Eady problem of baroclinic instability described in section 19a was shown to

The Eady problem of baroclinic instability described in section 19a was shown to 0. The Charney-Stern Theorem The Eady problem of baroclinic instability described in section 19a was shown to be remarkably similar to the Rayleigh instability of barotropic flow described in Chapter 18.

More information

The general circulation of the atmosphere

The general circulation of the atmosphere Lecture Summer term 2015 The general circulation of the atmosphere Prof. Dr. Volkmar Wirth, Zi. 426, Tel.: 39-22868, vwirth@uni-mainz.de Lecture: 2 Stunden pro Woche Recommended reading Hartmann, D. L.,

More information

Dynamics in the Earth s core. Philippe Cardin, ISTerre, Université Grenoble Alpes et CNRS

Dynamics in the Earth s core. Philippe Cardin, ISTerre, Université Grenoble Alpes et CNRS Dynamics in the Earth s core Philippe Cardin, ISTerre, Université Grenoble Alpes et CNRS Doctoral training on internal Earth, Barcelonnette, oct 2016 Sources of motions inside the core Core cooling and

More information

Modeling the atmosphere of Jupiter

Modeling the atmosphere of Jupiter Modeling the atmosphere of Jupiter Bruce Turkington UMass Amherst Collaborators: Richard S. Ellis (UMass Professor) Andrew Majda (NYU Professor) Mark DiBattista (NYU Postdoc) Kyle Haven (UMass PhD Student)

More information

Dynamics of the Extratropical Response to Tropical Heating

Dynamics of the Extratropical Response to Tropical Heating Regional and Local Climate Modeling and Analysis Research Group R e L o C l i m Dynamics of the Extratropical Response to Tropical Heating (1) Wegener Center for Climate and Global Change (WegCenter) and

More information

Asymmetric inertial instability

Asymmetric inertial instability Asymmetric inertial instability V. Zeitlin Institut Universitaire de France 2 Laboratory of Dynamical Meteorology, University P. and M. Curie, Paris, France UCL, December 2 Instabilities of jets Motivations,

More information

6 Two-layer shallow water theory.

6 Two-layer shallow water theory. 6 Two-layer shallow water theory. Wewillnowgoontolookatashallowwatersystemthathastwolayersofdifferent density. This is the next level of complexity and a simple starting point for understanding the behaviour

More information

Eliassen-Palm Theory

Eliassen-Palm Theory Eliassen-Palm Theory David Painemal MPO611 April 2007 I. Introduction The separation of the flow into its zonal average and the deviations therefrom has been a dominant paradigm for analyses of the general

More information

Tilting Shear Layers in Coastal Flows

Tilting Shear Layers in Coastal Flows DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Tilting Shear Layers in Coastal Flows Karl R. Helfrich Department of Physical Oceanography, MS-21 Woods Hole Oceanographic

More information

Chapter 9. Barotropic Instability. 9.1 Linearized governing equations

Chapter 9. Barotropic Instability. 9.1 Linearized governing equations Chapter 9 Barotropic Instability The ossby wave is the building block of low ossby number geophysical fluid dynamics. In this chapter we learn how ossby waves can interact with each other to produce a

More information

Wind-driven Western Boundary Ocean Currents in Terran and Superterran Exoplanets

Wind-driven Western Boundary Ocean Currents in Terran and Superterran Exoplanets Wind-driven Western Boundary Ocean Currents in Terran and Superterran Exoplanets By Edwin Alfonso-Sosa, Ph.D. Ocean Physics Education, Inc. 10-Jul-2014 Introduction Simple models of oceanic general circulation

More information

Finite Elements for the Quasi-Geostrophic Equations of the Ocean

Finite Elements for the Quasi-Geostrophic Equations of the Ocean Finite Elements for the Quasi-Geostrophic Equations of the Ocean Erich L Foster Dissertation submitted to the Faculty of the Virginia Polytechnic Institute and State University in partial fulfillment of

More information

The General Circulation of the Oceans

The General Circulation of the Oceans The General Circulation of the Oceans In previous classes we discussed local balances (Inertial otion, Ekman Transport, Geostrophic Flows, etc.), but can we eplain the large-scale general circulation of

More information

Reduction of the usable wind work on the general circulation by forced symmetric instability

Reduction of the usable wind work on the general circulation by forced symmetric instability GEOPHYSICAL RESEARCH LETTERS, VOL. 37,, doi:10.1029/2010gl044680, 2010 Reduction of the usable wind work on the general circulation by forced symmetric instability L. N. Thomas 1 and J. R. Taylor 2 Received

More information

EART164: PLANETARY ATMOSPHERES

EART164: PLANETARY ATMOSPHERES EART164: PLANETARY ATMOSPHERES Francis Nimmo Last Week Radiative Transfer Black body radiation, Planck function, Wien s law Absorption, emission, opacity, optical depth Intensity, flux Radiative diffusion,

More information

Can a Simple Two-Layer Model Capture the Structure of Easterly Waves?

Can a Simple Two-Layer Model Capture the Structure of Easterly Waves? Can a Simple Two-Layer Model Capture the Structure of Easterly Waves? Cheryl L. Lacotta 1 Introduction Most tropical storms in the Atlantic, and even many in the eastern Pacific, are due to disturbances

More information

10 Shallow Water Models

10 Shallow Water Models 10 Shallow Water Models So far, we have studied the effects due to rotation and stratification in isolation. We then looked at the effects of rotation in a barotropic model, but what about if we add stratification

More information

The Quasi-Biennial Oscillation Analysis of the Resolved Wave Forcing

The Quasi-Biennial Oscillation Analysis of the Resolved Wave Forcing The Quasi-Biennial Oscillation Analysis of the Resolved Wave Forcing Thomas Krismer, Marco Giorgetta Max Planck Institute for Meteorology Hamburg Introduction 1) The Quasi Biennial Oscillation is driven

More information

2. Conservation laws and basic equations

2. Conservation laws and basic equations 2. Conservation laws and basic equations Equatorial region is mapped well by cylindrical (Mercator) projection: eastward, northward, upward (local Cartesian) coordinates:,, velocity vector:,,,, material

More information

Chapter 5. Shallow Water Equations. 5.1 Derivation of shallow water equations

Chapter 5. Shallow Water Equations. 5.1 Derivation of shallow water equations Chapter 5 Shallow Water Equations So far we have concentrated on the dynamics of small-scale disturbances in the atmosphere and ocean with relatively simple background flows. In these analyses we have

More information

Notes and Correspondence Higher-order corrections for Rossby waves in a zonal channel on the β-plane

Notes and Correspondence Higher-order corrections for Rossby waves in a zonal channel on the β-plane QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY Q. J. R. Meteorol. Soc. 33: 893 898 (7 Published online 4 October 7 in Wiley InterScience (www.interscience.wiley.com DOI:./qj.44 Notes and Correspondence

More information

The Physics of Fluids and Plasmas

The Physics of Fluids and Plasmas The Physics of Fluids and Plasmas An Introduction for Astrophysicists ARNAB RAI CHOUDHURI CAMBRIDGE UNIVERSITY PRESS Preface Acknowledgements xiii xvii Introduction 1 1. 3 1.1 Fluids and plasmas in the

More information

MT Dynamic Meteorology II MWF Spring :00 a.m. - 8:50 a.m. Dr. Jim Koermer Boyd 306 DYNAMIC METEOROLOGY II SYLLABUS

MT Dynamic Meteorology II MWF Spring :00 a.m. - 8:50 a.m. Dr. Jim Koermer Boyd 306 DYNAMIC METEOROLOGY II SYLLABUS MT5320.01 - Dynamic Meteorology II MWF Spring 2011 8:00 a.m. - 8:50 a.m. Dr. Jim Koermer Boyd 306 DYNAMIC METEOROLOGY II SYLLABUS COURSE DESCRIPTION: Dynamic Meteorology II involves the application of

More information

Joseph Pedlosky Senior Scientist Emeritus Geophysical Fluid Dynamicist Department of Physical Oceanography Woods Hole Oceanographic Institution

Joseph Pedlosky Senior Scientist Emeritus Geophysical Fluid Dynamicist Department of Physical Oceanography Woods Hole Oceanographic Institution Joseph Pedlosky Senior Scientist Emeritus Geophysical Fluid Dynamicist Department of Physical Oceanography Woods Hole Oceanographic Institution Education B.Sc., Massachusetts Institute of Technology, 1960

More information

Dynamics of Upper-Level Waves

Dynamics of Upper-Level Waves Dynamics of Upper-Level Waves Atmos 5110 Synoptic Dynamic Meteorology I Instructor: Jim Steenburgh jim.steenburgh@utah.edu 801-581-8727 Suite 480/Office 488 INSCC Suggested reading: Lackman (2011) section

More information

Impact of atmospheric CO 2 doubling on the North Pacific Subtropical Mode Water

Impact of atmospheric CO 2 doubling on the North Pacific Subtropical Mode Water GEOPHYSICAL RESEARCH LETTERS, VOL. 36, L06602, doi:10.1029/2008gl037075, 2009 Impact of atmospheric CO 2 doubling on the North Pacific Subtropical Mode Water Hyun-Chul Lee 1,2 Received 19 December 2008;

More information

centrifugal acceleration, whose magnitude is r cos, is zero at the poles and maximum at the equator. This distribution of the centrifugal acceleration

centrifugal acceleration, whose magnitude is r cos, is zero at the poles and maximum at the equator. This distribution of the centrifugal acceleration Lecture 10. Equations of Motion Centripetal Acceleration, Gravitation and Gravity The centripetal acceleration of a body located on the Earth's surface at a distance from the center is the force (per unit

More information

Internal inertio-gravity waves in the laboratory: Mechanisms, properties, and impacts

Internal inertio-gravity waves in the laboratory: Mechanisms, properties, and impacts Internal inertio-gravity waves in the laboratory: Mechanisms, properties, and impacts Abstract Paul Williams Department of Meteorology, University of Reading, UK p.d.williams@reading.ac.uk This paper describes

More information

Author or co-author of about 116 refereed publications. December, 2001

Author or co-author of about 116 refereed publications. December, 2001 Joseph Pedlosky Senior Scientist Doherty Professor of Oceanography Geophysical Fluid Dynamicist Department of Physical Oceanography Woods Hole Oceanographic Institution Birth: April 7, 1938 B.Sc., Massachusetts

More information

9 Rossby Waves. 9.1 Non-divergent barotropic vorticity equation. CSU ATS601 Fall (Holton Chapter 7, Vallis Chapter 5)

9 Rossby Waves. 9.1 Non-divergent barotropic vorticity equation. CSU ATS601 Fall (Holton Chapter 7, Vallis Chapter 5) 9 Rossby Waves (Holton Chapter 7, Vallis Chapter 5) 9.1 Non-divergent barotropic vorticity equation We are now at a point that we can discuss our first fundamental application of the equations of motion:

More information

d v 2 v = d v d t i n where "in" and "rot" denote the inertial (absolute) and rotating frames. Equation of motion F =

d v 2 v = d v d t i n where in and rot denote the inertial (absolute) and rotating frames. Equation of motion F = Governing equations of fluid dynamics under the influence of Earth rotation (Navier-Stokes Equations in rotating frame) Recap: From kinematic consideration, d v i n d t i n = d v rot d t r o t 2 v rot

More information

An Introduction to Coupled Models of the Atmosphere Ocean System

An Introduction to Coupled Models of the Atmosphere Ocean System An Introduction to Coupled Models of the Atmosphere Ocean System Jonathon S. Wright jswright@tsinghua.edu.cn Atmosphere Ocean Coupling 1. Important to climate on a wide range of time scales Diurnal to

More information

PHYSFLU - Physics of Fluids

PHYSFLU - Physics of Fluids Coordinating unit: 230 - ETSETB - Barcelona School of Telecommunications Engineering Teaching unit: 748 - FIS - Department of Physics Academic year: Degree: 2018 BACHELOR'S DEGREE IN ENGINEERING PHYSICS

More information