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Volume
THE MASS OF THE MOLECULES
IN A GIVEN VOLUME
IF TOTAL MASS IN A VOLUME
DECREASES, THE DENSITY
DECREASES AND VICE VERSA
THE UNITS OF DENSITY ARE
EXPRESSED IN TERMS OF
MASS PER UNIT VOLUME
Pressure
The force exerted by the moving molecules of the gas/liquid/solid in a given area.
Pressure at a point acts equally in all directions.
Example: A typical value of atmospheric pressure at sea level is 14.7 pounds per square inch (1013.25 millibars, 29.92 inches of mercury).
Gas Law (P/DT=R)
P = pressure
D = density
T = temperature
The ratio of pressure to density and temperature is always the same (BALANCED). If pressure changes, then either density or temperature must also change
Charting Atmospheric Pressure
Pilots pay special attention to the horizontal distribution of atmospheric pressure
These pressure patterns are normally identified through
chart analyses
Sea Level Pressure Patterns
Pressure gradient – difference in pressure over a given distance
Strong pressure gradient = closely spaced isobars
Weak pressure gradient = spaced isobars
Isopleths spacing displays gradients of many parameters
The Pressure Altimeter
Indicated altitude – measured by altimeter
True altitude – height MSL
Absolute altitude – height AGL
Three specific errors caused by nonstandard atmospheric conditions:
Sea level pressure different from 29.92 in. Hg
Temperature warmer or colder than standard
Strong vertical gusts
Pressure Variation Error
Standard atmosphere is based on a fixed pressure (1013.25 mb)
This value provides important reference because different locations vary due to:
Heating and cooling of the earth
Movements of high and low pressure areas
Nonstandard Temperature Error
Temperature variations expand or contract the atmosphere and raise or lower pressure levels that the altimeter senses
On a warm day – pressure level is higher than standard...altimeter indicates lower than actual
On a cold day – pressure level is lower than standard...altimeter
indicates higher than actual
REMEMBER: High to Low, Look out Below!
Vertical Gust Error
• Caused by large and rapid changes in vertical movements of air
• The changes upset the balance of forces or the hydrostatic balance
• These errors can be expected in the extreme updrafts of thunderstorms and in strong mountain waves
Density
Lower atmospheric densities yield LOWER aircraft performance
Fix with special aircraft and power plant designs
Density altitude – pressure altitude corrected for nonstandard temperature
Note: Humid air is less dense than dry air at the same pressure and temperature