Foehn wind
 

Can anyone explain why the rate of dry warming jumps to 2 degrees per 200m at 2800m?

Isn't the dry adiabatic lapse rate a consistent 1.33c per 200m?

The DALR is 2º/200m. 1.33º/200m is the 'standard' lapse rate.

So why does it increase at a rate of 1º/200m from the top on the right 4400m? Surely this is the DLR as well (since the air is dry) and the DLR should remain consistent?

What he said ^^^^

Your last thread had the lapse rates in imperial, studying in both will not help, keep to what the exams are in (I presume they are not in both!).

Altitude in feet, speed in knots, distance in nautical miles, runway length in metres, temp in Celsius? And C of G calculations?

When I said not in both I really meant for any particular subject, yes conversions are actually part of the sylabus, but I would think lapse rates are only tested in one regime!

Thanks foxmoth. The bit I hadn't realised was that it is still saturated for a while on the leeward side!

I wasn't looking to study in both, but I wanted a video to help understand, and that was the measurement they used.

Correct, though of course containing less moisture as it has dropped some as precipitation as it goes over the mountains and is why it is a "warm" wind.