21-24 Flashcards
Coriolis Force
A force acting on objects that are moving when they are moving in a rotating context.
90 right in N
90 Left in S
Equations with coriolis forces
r=
θ =
r (distance in inertial frame of reference) = vΔt
but then at time Δt, world rotated θ
so s = horizontal distance from predicted if not on rotating plane = rθ = 1/2 * a * (Δt)^2 = Ω v((Δt)^2)
where Ω= rotation speed
What is coriolis acceleration?
2Ωv
Coriolis force equation =
f = 2Ωsin(φ)
φ = latitude
Rossby waves
They are inertial waves
- in the context of the atmosphere - they are the meanders in the jet streams caused by the rotation of the earth
- more prominent in polar jet stream
Geostrophic flow
The movement of air parcels down a pressure gradient which is balanced by Coriolis forcing
Adiabatic Lapse Rate
The temperature change of an air parcel per unit time when the elevation change is adiabatic, so no heat transfer and so the parcel expands with altitude or contracts when it sinks
With no condensation = 10 degrees/km
Observed= 7degrees/km
Why is observed lapse rate different?
Because of the latent heat of condensation
Dew point
the saturation of the air, so once past this, the water will condense out