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1.Fundamental equations and concepts 2.Balanced flow and vortex motion 3.Waves 4.Instabilities 5.Nonlinear phenomena An Introduction to Geophysical Fluid Dynamics YODEN Shigeo Department of Geophysics, Kyoto University The 2nd KAGI-21 INTERNATIONAL SUMMER SCHOOL: Aug. 15-27, 2005
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1. Fundamental equations and concepts 1.1 Fundamental equations for Newtonian fluids
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Continuity equation conservation law of mass advection (Lagrange) form flux form Momentum equation conservation law of momentum (Navie-Stokes Eq.) ~0
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advection vs. diffusion linear advection-diffusion equation (1D) nonlinear advection-diffusion equation: Burgers equation Brownian motion Langevin equation for a particle stochastic motions of a huge ensemble of particles ?
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Energy equation conservation law of total energy (internal + kinetic) 1st law of thermodynamics (dU=ΔW + ΔQ ) entropy conservation of entropy in adiabatic conditions
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Equation of state ideal gas Boussinesq fluid in the buoyancy term, and ρ=constant in the other terms incompressible fluid
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stress tensor momentum equation for continuum Cauchy’s 1st law of motion conservation law of angular momentum Cauchy’s 2nd law of motion for Newtonian fluids p : pressure
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H L Advection of finite fluid elements in a steady 2D flow deformation rate deformation rate tensor strain rate tensor elongation-contraction rate shear strain rate vorticity
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1.2 Fundamental equations in a rotating frame momentum equation in a rotating frame an orthogonal inertial frame with a set of unit vectors a rotating frame with which rotates with a constant angular velocity : position, velocity, and acceleration Coriolis force and centrifugal force CoCe
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inertial oscillation free motion of a particle on a rotating plane without Ce if we put inertial oscillation with a period of 2π/f (=π/Ω) inertial circle with a radius of |W 0 /f |
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momentum equation on the rotating Earth a spherical coordinate + rotation Ω ⇒ (longitude λ, latitude φ, radius r ) traditional approximation (r =a +z ; |z | << a ) conservation of angular momentum?
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2. Balanced flow and vortex motion 2.1 Steady axisymmetric vortex in a rotating frame constant density fluid a cylindrical coordinate (r, θ, z ) 2D motion independent of z + rotation Ω steady axisymmetric motion balance in centrifugal, Coriolis, and pressure grad. forces
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Rossby number Ro = Centrifugal force / Coriolis force = v / (2Ωr ) cyclostrophic-flow balance Ro >> 1 ex. tornado bathtub vortex gradient-flow balance Ro ~ 1 ex. typhoon
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geostrophic-flow balance Ro << 1 ex. circumpolar vortex inertial flow Pressure grad. force ~ 0
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2.2 Circulation and vorticity circulation theorem velocity, vorticity, and circulation Bjerknes’ circulation theorem Kelvin’s circulation theorem (by Stokes’s theorem) (solenoid term) B : baroclinic vector for barotropic fluid: B =0, or ρ = (p )
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vorticity equation momentum equation in a vector invariant form vorticity equation tilting term and stretching term in a rotating system momentum equation and vorticity equation
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2.3 Potential vorticity conservation of potential vorticity –ideal gas potential vorticity potential vorticity equation for inviscid fluid under conservative external forces PV thinking invertibility: P ⇒ other dynamical quantities (u, T, ・・・ ) conserved in Lagrangian motion combination with other conserved quantities: (Θ, q, ・・・ ) s : entropy or potential temperature Θ
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conservation of potential vorticity –shallow water shallow water equations potential vorticity equation
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2.3 Vortex motions Rankin vortex circular vortex patch Contour dynamics evolution of vortex patch ex. elliptic vortex elongated one is unstable
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stratospheric polar vortex point vortex Fujiwara effect Karman vortices Karman vortices around Robinson Crusoe Island DeFelice et al. (2000, BAMS ) McIntyre and Palmer (1983, Nature ) Fujii (2001)
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