Atmospheric dynamics 1
Background Concepts
Variables, laws
• Basic variables: 6 (7)
• Need 6 (7) physical laws
(3) conservation of momentum
(1) conservation of energy
(1) equation of state
(1) conservation of mass
(1) conservation of mass for composition
u, v, w, p, ρ, T, (q, S)
Concepts
• Continuum hypothesis
- parcel: tiny volume >> such that variables are well defined tiny volume << length scale of variables are varying
• Material derivative
T = T(x, y, z, t)
DT
Dt ≡ ∂T
∂t + u ∂T
∂x + v ∂T
∂y + w ∂T
∂z
Equations
• Momentum equation F = ma
Pressure gradient force
Viscosity
• Thermodynamic energy equation
I = I(α, η, s)
dI = dQ + dW + dC
cp DT
Dt − α Dp
Dt = J
Equations
• Conservation of mass (continuity equation)
• Conservation of mass for composition
∂
∂t ∫V ρ dv = − ∫S ρ v ⃗ ⋅ ⃗s = − ∫V ∇ ⋅ (ρ v )⃗ dv
∂ρ
∂t + ∇ ⋅ (ρ v ⃗) = 0
∂
∂t ∫V ρq dv = − ∫S ρq v ⃗ ⋅ ⃗s = − ∫V ∇ ⋅ (ρq v ⃗) dv
∂q
∂t + ∇ ⋅ (q v ) = 0⃗
Equations
• Conservation of mass for composition
• If q-flux include “downgrading mixing”
∂q
∂t + ∇ ⋅ (q v ) = 0⃗
∂
∂t ∫V ρq dv = − ∫S (ρq v ⃗ − ρκ∇q) ⋅ ⃗s
∂q
∂t + ∇ ⋅ (q v ) =⃗ κ∇2q