Upload
charlotte-johns
View
222
Download
0
Tags:
Embed Size (px)
Citation preview
Dynamics I
• 23. Nov.: circulation, thermal wind, vorticity
• 30. Nov.: shallow water theory, waves
• 7. December: numerics: diffusion-advection
• 14. December: computer simulations
Fluid dynamics
properties of mass, momentum and energy
in a control volume
Substatial or material derivative
Fluid dynamics
properties of mass, momentum and energy
in a control volume
Substatial or material derivative
To Add: Vorticity !
Scale Analysis
Scale Analysis
Scale Analysis
dominant terms: geostrophy
Scale Analysis
Validity of the geostrophic approximation:
Geostrophic approximation:
Geostrophic balance:
Parallelism between wind velocities
and pressure contours (isobars)
Taylor–Proudman theorem (Taylor, 1923; Proudman, 1953)
gConst.
vertical derivative of the horizontal velocity is zero:
Physically, it means that the horizontal velocity field has no vertical shear and that all particles on the same vertical move in concert. Such vertical rigidity is a fundamental property of rotating homogeneous fluids.
Non-Geostrophic Flows
g still suppose that the fluid is homogeneous and frictionless, no vertical structure
Additional terms
Non-Geostrophic FlowsContinuity equation:
Non-Geostrophic Flows
Surface elevation η = b + h − H:
Continuity equation:
Non-Geostrophic Flows
In the absence of a pressure variation above the fluid surface (e.g., uniform atmospheric pressure over the ocean), this dynamic pressure is
Continuity equation
Shallow Water ModelCase b=0
This is a formulation that we will encounter in layered models !
Vorticity
Vorticity:
Elimination of pressure terms:
Continuity:
d/dt [(f+ zeta)/h] = 0Conservation of potential vorticity
ambient vorticity (f) plus relative vorticity zeta
vorticity vector is strictly vertical
(Volume conservation)
Conservation of volume in an incompressible fluid
This implies that if the parcel is squeezed vertically (decreasing h), it stretches horizontally (increasing ds), and vice versa
Vorticity
horizontal divergence (∂u/∂x + ∂v/∂y > 0) causes widening of the cross-sectional area ds
convergence (∂u/∂x + ∂v/∂y < 0) narrowing of the crosssection.
Kelvin’s theorem
(f + zeta)/h : the potential vorticity, is also conserved.
Kelvin’s theorem
(f + zeta)/h : the potential vorticity, is also conserved.
This product canbe interpreted as the vorticity flux (vorticity integrated over the cross-section) and is therefore the circulation of the parcel.
Two-dimensional flows: Kelvin’s theorem conservation of circulation in inviscid fluids
Circulation of a parcel
(f + zeta)/h : the potential vorticity, is also conserved.
This product can be interpreted as the vorticity flux (vorticity integrated over the cross-section) and is therefore the circulation of the parcel.
Two-dimensional flows: Kelvin’s theorem guarantees conservation of circulation in inviscid fluids
Exercise !
Potential Vorticity
Rapidly rotating flows, in which the Coriolis force dominates. In this case, the Rossby number is much less than unity (Ro = U/L << 1),which implies that the relative vorticity (ζ = ∂v/∂x − ∂u/∂y, scaling as U/L) is negligible in front of the ambient vorticity f. The potential vorticity reduces to q =f/h !
if f is constant – such as in a rotating laboratory tank or for geophysical patterns of modest meridional extent – implies that each fluid column must conserve its height h.
Shallow Water ModelCase b=0
This is a formulation that we will encounter in layered models !
Shallow Water ModelCase b=0
Schrödinger equation: harmonic oscillator
In the one-dimensional harmonic oscillator problem, a particle of mass m is subject to a potential V(x) = (1/2)mω^2 x^2. The Hamiltonian of the particle is:
where x is the position operator, and p is the momentum operator
we must solve the time-independent Schrödinger equation:
Solution
Ladder operator method
a acts on an eigenstate of energy E to produceanother eigenstate of energy
a† acts on an eigenstate of energy E to produce an eigenstate of energy
a "lowering operator", a† "raising operator„
The two operators together are called "ladder operators".
In quantum field theory, a and a† are alternatively called "annihilation" and "creation" operators because they destroy and create particles, which correspond to our quanta of energy.
Operator a and a† have properties:
Graph
Graph
Rossby
Gravity
Kelvin
Yanai, mixed G-R
Homework