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Home > Exam Questions > ATPL - Airline Transport Pilot Licence > Meteorology > In a typical Northern Hemisphere warm-advection situation ahead of a warm front, how does wind direction generally change with increasing height through the surface friction layer and then through the lower and middle troposphere above it?

313 - ATPL Question Bank in English - In a typical Northern Hemisphere warm-advection situation ahead of a warm front, how does wind direction generally change with increasing height through the surface friction layer and then through the lower and middle troposphere above it?

Question 313 - Meteorology - ATPL - Airline Transport Pilot Licence

Veers in the friction layer and backs above the friction layer

Backs in the friction layer and veers above the friction layer

Backs in the friction layer and backs above the friction layer

Veers in the friction layer and veers above the friction layer

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