CLIMATE/EARTH 401�Geophysical Fluid Dynamics�Dynamical Meteorology
Mass Conservation: Continuity
Conservation of Mass
Remember our particle of atmosphere, our parcel
Δx
Δy
Δz
ρ ≡ density =
mass per unit volume (ΔV)
ΔV = ΔxΔyΔz
m = ρΔxΔyΔz
-------------------------------------
p ≡ pressure =
force per unit area
acting on the particle of
atmosphere
The Eulerian point of view our parcel is a fixed volume and the fluid flows through it.
Δx
Δy
Δz
Introduce mass flux, ρu
.
Δx
Δy
Δz
(x, y, z)
x
Introduce mass flux, ρu
.
Δx
Δy
Δz
(x, y, z)
x
What is the change of mass inside the fixed volume?
The change of mass in the box is equal to the mass that flows into the box minus the mass that flows out of the box = (flux) x (area)
Mass out right (downstream) face
Mass in left (upstream) face
Extend to 3-Dimensions
The change of mass in the box is equal to the mass that flows into the box minus the mass that flows out of the box = (flux) x (area)
Note: this is change in mass per unit volume.
Recognizing the definition of divergence
Eulerian Form of the Continuity Equation
Δx
Δy
Δz
In the Eulerian point of view, our parcel is a fixed volume and the fluid flows through it.
The Lagrangian point of view is that the parcel is moving.
Δx
Δy
Δz
And it changes shape…
Homework Exercise: Derive the Lagrangian Form
�
Lagrangian Form of the Continuity Equation
The change in mass (density) following the motion is equal to the divergence
Convergence = increase in density (compression)
Divergence = decrease in density (expansion)
The Lagrangian point of view is that the parcel is moving.
Δx
Δy
Δz
And it changes shape…
End: Mass Conservation: Continuity