11: Atmosphere Motion - Dry Processes (DALR) Flashcards
Form of Energy in the Atmosphere (4)
1) Electrical energy (Thunderstorms & lightning) 2) External kinetic energy (Winds) 3) Potential energy (Vertical motion) 4) Work done (Parcels expand as they rise) (Parcels contract as they sink)
Sources of energy available to parcel of air
3
1) Internal (kinetic) energy
2) External energy
(via absorption of UV by O3)
3) External energy
(via surface heating - close to surface)
Define Adiabatic
No external source of energy
Dry Adiabatic Lapse Rate (DALR)
1) Define
2) 1* C
3) 10* C
1) Rate at which temperature changes
(no change of phase)
2) 1* C for every 100 m
3) 10 * C for every 1000 m
Environmental Lapse Rate Depending on the atmosphere, the parcel of air temperature will change. what happens when: 1) Warm 2) Cold 3) Same temp
1) Rise & due to buoyancy will cause unstable conditions
2) Sink - stable conditions
3) It wont move - neutral conditions
What determines atmospheric stability
The temperature of a parcel of air relative to the temperature of its surrounding environment
When does a neutral atmosphere occur
If actual lapse rate is exact equal to DALR
Unstable atmosphere calculation (DALR) 1) Atmosphere 20* C at surface 8* C, at 1 km 2) Parcel of air 20* C at surface 10* C, at 1 km What happens to the parcel of air?
Parcel (dry) warmer than environment & therefor rise
Stable atmosphere calculation (DALR) 1) Atmosphere 20* C at surface 13* C, at 1 km 2) Parcel of air 20* C at surface 10* C, at 1 km What happens to the parcel of air?
Parcel (dry) is cooler than environment & therefor sink
If the environment/actual lapse rate is greater than the DALR then…
Parcel (dry) is warmer than its surrounding environment = unstable conditions
If the environment/actual lapse rate is less than the DALR then…
Parcel (dry) is cooler than its surrounding environment = stable conditions
If the environment/actual lapse rate is equal than the DALR then…
Parcel & environment at the same temperature = neutral conditions