
Tutorial
2(c). Atmosphere
![]() |
|
|
Warm Air |
Cold Air |
Altitudinal variations need to also be monitored by the pilot before and during
flight. Normally in the troposphere temperature decreases as the altitude increases.
This is known as the lapse rate. The average temperature decrease (or average
lapse rate) in the troposphere is usually given as 2.0 Celsius per 1,000 feet.
Remember this is just an average! There are times when the temperature actually
increases with height. This increase in temperature with an increase in altitude
is known as an inversion. That is, the lapse rate is inverted or moves opposite
to what is expected. Inversions can occur at any altitude if conditions are
conducive to their development. See the two examples below for a description
of such conditions.
Ground-based
inversion: occurs near the ground on cold, clear nights. Since the ground radiates and cools much faster than the
air above it, air in contact to the ground becomes cold while just a few hundred feet above it that temperature
has changed very little. This can trap fog or smoke close to the ground and decrease visibility.
Inversion
aloft: Occurs a little higher in the atmosphere than ground-based inversions. A current of warm air overruns a
large patch of cold air trapping it next to the Earth's surface. If rain clouds in the warm air current drop rain,
it will pass through the colder air and freeze. This can develop into icing on an aircraft's wings drastically
reducing the aircraft's lift force.