Reinisch_ASD85.515_Chap#71 Chapter 7. Atmospheric Oscillations Linear Perturbation Theory.

Slides:



Advertisements
Similar presentations
Parameterization of orographic related momentum
Advertisements

Chapter 1: What is the Mesoscale? Mesoscale energy sources.
Please return your tests to me at the end of the peroid. I will return them Friday with a printout of all your scores and your current grade. Test scores.
The pulse wave.
Section 5: Kelvin waves 1.Introduction 2.Shallow water theory 3.Observation 4.Representation in GCM 5.Summary.
Physics 1251 The Science and Technology of Musical Sound Unit 1 Session 8 Harmonic Series Unit 1 Session 8 Harmonic Series.
Chapter 15 - Waves Traveling Waves –Types –Classification –Harmonic Waves –Definitions –Direction of Travel Speed of Waves Energy of a Wave Standing Waves.
Chapter 4 Waves in Plasmas 4.1 Representation of Waves 4.2 Group velocity 4.3 Plasma Oscillations 4.4 Electron Plasma Waves 4.5 Sound Waves 4.6 Ion Waves.
Physics 110G Waves TOC 1 Transverse Waves in Space Transverse Waves in Time Longitudinal Waves in Space Longitudinal Waves in Time.
Gravity Waves. Kayak Surfing on ocean gravity waves Oregon Coast.
Chapter 1: What is the Mesoscale? Mesoscale energy sources.
Phase Difference = Phase Difference = 0.05.
Waves on a string THIS LECTURE Standing waves Standing waves Dispersive and non-dispersive waves Dispersive and non-dispersive waves.
This lecture A wide variety of waves
Phy 212: General Physics II Chapter 16: Waves I Lecture Notes.
5.6 Energy Dispersion – Group Velocity. Non-dispersive waves (movie) Wave 1: K1, C1 Wave 2: K2, C2 K2=1.4*k1 C2=C1 The phase shift between the two waves.
Chapter 10 Ocean Waves Part 1 ftp://ucsbuxa.ucsb.edu/opl/tommy/Geog3awinter2011/
Gravity Waves Geraint Vaughan University of Manchester, UK
Presentation Slides for Chapter 4 of Fundamentals of Atmospheric Modeling 2 nd Edition Mark Z. Jacobson Department of Civil & Environmental Engineering.
Fluid Mechanics Fluid Statics Fluid Dynamics LectureParticleTotalMidTW/VivaGTU ExTotal 325 hr
Applied NWP [1.2] “Once the initialization problem was resolved in the 1960s, models based on the primitive equations gradually supplanted those based.
Associate Professor: C. H.L IAO. Contents:  3.1 Introduction 99  3.2 Simple Harmonic Oscillator 100  3.3 Harmonic Oscillations in Two Dimensions 104.
16-6 Wave Speed on a Stretched String
Richard Rotunno National Center for Atmospheric Research, USA Dynamic Mesoscale Mountain Meteorology Lecture 3: Mountain Waves.
Prof. dr. A. Achterberg, Astronomical Dept., IMAPP, Radboud Universiteit.
Basic properties of waves One-dimensional wave t=0 t circular wave-number wave-number angular frequency frequency phase speed phase measures the position.
Sound speed in air: C Ｓ ∝ [T] 1/2 T[K] C Ｓ [m/s] Conv. Div. tendency of pressure & density >0
11/20/2015 Fourier Series Chapter /20/2015 Fourier Series Chapter 6 2.
Signals and Systems Using MATLAB Luis F. Chaparro
Internal Wave Interactions with Time-Dependent Critical Levels Brian Casaday and J. C. Vanderhoff Department of Mechanical Engineering Brigham Young University,
Copyright © 2011 Pearson, Inc. 4.6 Graphs of Composite Trigonometric Functions.
Gravity waves derivation ATM Fall, Introduction Gravity waves describe how environment responds to disturbances, such as by oscillating parcels.
12/2/2015 Fourier Series - Supplemental Notes A Fourier series is a sum of sine and cosine harmonic functions that approximates a repetitive (periodic)
EVAT 554 OCEAN-ATMOSPHERE DYNAMICS TIME-DEPENDENT DYNAMICS; WAVE DISTURBANCES LECTURE 21.
Chapter 19 Physics A First Course Vibrations, Waves, and Sound.
Physical Conditions 9/16-9/ including Hurricane Isabel inches Hg ft (MLLW) knots inches Atmospheric Pressure.
Wave Equation II and Solution. Length of the curved element.
V 0 =g/f  /  x div.conv.div. Phase propagation Rossby Wave Physics (planetary  -effect)
PHYSICAL CHEMISTRY - ADVANCED MATERIALS Particles and Waves Two opposing concepts Particle theory Field theory Quantum Mechanics Position, mass, velocity,
Ellipsometry: finding n,  or thicknesses, roughness… Wikipedia /ellipsometers/l116sf.htm starts linear, angle.
How do we describe this? 10. Wave Motion. An initial shape… …so can we just let the normal modes oscillate at  n ? No! Because that initial shape can.
Chapter Twenty-Three: Waves  23.1 Harmonic Motion  23.2 Properties of Waves  23.3 Wave Motion.
Light and Matter Tim Freegarde School of Physics & Astronomy University of Southampton Wave mechanics.
The Spectrum n Jean Baptiste Fourier ( ) discovered a fundamental tenet of wave theory.
10//3015PHY 711 Fall Lecture 261 PHY 711 Classical Mechanics and Mathematical Methods 10-10:50 AM MWF Olin 103 Plan for Lecture 26: Chap. 9 of.
The Frequency Domain Digital Image Processing – Chapter 8.
Atmospheric Gravity Waves
Chapter 6 Quasi-geostrophic waves. Balanced stateElastostatic (compressible) HydrostaticGeostrophicSverdrup Result of disturbing it Acoustic oscillations.
Chapter 11 More on wave motions, filtering.  Consider a homogeneous layer of inviscid fluid on an f-plane confined between rigid horizontal boundaries.
Fourier analysis Periodic function: Any (“reasonable”) periodic function, can be written as a series of sines and cosines “vibrations”, whose frequencies.
Geostrophic adjustment
ATMOSPHERIC WAVES.
Damped Inertial oscillations
Waves Chapter 16: Traveling waves
Basic properties of waves
Chapter-3 Standing Waves and the Overtone Series
Phase Velocity & Group Velocity.
♠ ♠ ♠ ♠ الاصوات والموسيقا مجلس أبوظبي للتعليم منطقة العين التعليمية
Physics A First Course Vibrations, Waves, and Sound Chapter 19.
Theory of solar and stellar oscillations - I
Digital Signal Processing
Graphs of Composite Trigonometric Functions
Low frequency radiation from a duct exhausting a hot gas
PHY 711 Classical Mechanics and Mathematical Methods
Ay 123 Lecture 9 - Helioseismology
SWBAT model harmonic motion using graphs.
PHY 711 Classical Mechanics and Mathematical Methods
Week 2: can you? Understand terms in the Equations of Motion of the atmosphere: Acceleration Pressure gradient Coriolis force. Be able to describe and.
Solving a System of Linear Equations
Chapter Twenty-Three: Waves
Presentation transcript:

Reinisch_ASD85.515_Chap#71 Chapter 7. Atmospheric Oscillations Linear Perturbation Theory

Reinisch_ASD85.515_Chap# Perturbation Method

Reinisch_ASD85.515_Chap# Properties of Waves

Reinisch_ASD85.515_Chap#74 Sinusoidal oscillations and waves

Reinisch_ASD85.515_Chap#75 Phase velocity

Reinisch_ASD85.515_Chap# Fourier Series

Reinisch_ASD85.515_Chap# Dispersion and Group Velocity

Reinisch_ASD85.515_Chap# Acoustic (Sound) Waves

Reinisch_ASD85.515_Chap#79

10

Reinisch_ASD85.515_Chap#711

Reinisch_ASD85.515_Chap# Shallow-Water Gravity Wave

Reinisch_ASD85.515_Chap#713 =0

Reinisch_ASD85.515_Chap#714 Internal Gravity (or Buoyancy) Waves

Reinisch_ASD85.515_Chap#715 Two-dimensional Internal Gravity Waves

Reinisch_ASD85.515_Chap#716 Perturbation - Linearization

Reinisch_ASD85.515_Chap#717

Reinisch_ASD85.515_Chap#718

Reinisch_ASD85.515_Chap#719

Reinisch_ASD85.515_Chap#720

Reinisch_ASD85.515_Chap#721 Dispersion relation

Reinisch_ASD85.515_Chap#722 LzLz  =kx+mz=const    z x  LxLx

Reinisch_ASD85.515_Chap#723

Reinisch_ASD85.515_Chap#724

Reinisch_ASD85.515_Chap# Topographic Waves

Reinisch_ASD85.515_Chap#726

Reinisch_ASD85.515_Chap#727 Topographic example

Reinisch_ASD85.515_Chap#728

Reinisch_ASD85.515_Chap# Inertial Oscillation

Reinisch_ASD85.515_Chap# Inertio-gravity Waves

Reinisch_ASD85.515_Chap#731

Reinisch_ASD85.515_Chap# Rossby Waves

Reinisch_ASD85.515_Chap#733

Reinisch_ASD85.515_Chap#734

Reinisch_ASD85.515_Chap#735 Phase speed of Rossby waves

Reinisch_ASD85.515_Chap#736

Feedback: Privacy Policy Feedback
Do Not Sell My Personal Information
About project: SlidePlayer Terms of Service

© 2024 SlidePlayer.com Inc. All rights reserved.