Adiabatic process
Were heat doesn’t enter or leave the system
Dalr
Dry adiabatic lapse rate
Temp of a air parcel that decreases with height
When it is made to ascend adiabatically
Elr
Environmental lapse rate
It is the actual lapse rate existing in atmosphere
In isa it is 6.5 /1km
Salr
Saturated adiabatic lapse rate
It is not constant like dalr
It is when a saturated air parcel is lifted adiabatically
The extra water vapour condenses and latent heat is released.
What is stability and instability and netural
Is the air parcel moves up and sinks back down it is stable
If not and just moves up then it is unstable and if it just stays at the new level of them is it netural
Conditional instability
When dalr> Elr > salr
It is unstable for saturated air and stable for dry air
Latent instability
It is when the stable parcel of air becomes unstable when it is forced to ascend by hidden instability
Real latent
When the energy required is less than the air parcel to rise up
Pseudo Latent
When the force needed to left the air parcel is more than energy released
For potential instability to occur
The RH should be high is low levels and low in higher lvl
Dry air is stable when
Dalr> elr
Saturated air to be stable
Salr> elr
For absolute unstable
Elr > dalr
Absolute stable
Salr> dalr > elr