Published in the July
1998 issue of Continental,
Continental Airlines' in-flight magazine
How High Are We Flying?
By Dave Esser
Have you ever wondered what keeps pilots "on track" in
the sky? A pilot must know how high a plane is flying
as well as its direction of travel. Key in measuring altitude,
or the plane's elevation, is the altimeter, since the
aircraft must maintain a safe distance from terrain and
other obstacles. How does the altimeter function and how
does the information it provides help the pilot safely
conduct the flight?
Depending on the reference point used, there are several
types of altitude. The most commonly used is true altitude,
or an aircraft's height above mean sea level. Height "above
ground level" (AGL) is, quite simply, the absolute or
actual altitude of an aircraft. Pressure altitude, also
used in flight planning, represents the height of the
aircraft above standard sea level pressure. Aircraft flying
above 18,000 feet use "flight levels" (FL), which represent
pressure altitude in hundreds of feet. For example, FL
210 represents a pressure altitude of 21,000 feet, FL
240 is 24,000 feet, and so on.
The pressure at sea level, about 15 pounds per square
inch, is caused by the weight of the atmosphere. As altitude
increases, the associated pressure decreases, although
not in a linear manner; decreases occur in smaller and
smaller amounts. Atmospheric pressure decreases by one-half
for every 20,000-foot rise in altitude. At 20,000 feet
the pressure is about half of that at sea level, so at
40,000 feet (cruise altitude) the pressure is approximately
one-quarter of that at sea level. The height of the aircraft
can be determined by measuring this decrease in pressure.
As high and low pressure systems move overhead, changes
occur in the pressure at sea level. So why is the altimeter
not tricked by these constant changes? The pilot is able
to set the altimeter to the existing sea level pressure;
the altimeter then indicates how high the aircraft is
above this pressure level. Air traffic controllers are
constantly monitoring the changing barometric pressure
and relaying this information to pilots.
The aneroid altimeter is very similar to a barometer.
Inside, sealed wafers expand as the pressure around them
decreases. The pressure inside the altimeter is vented
to a static port on the outer surface of the aircraft
so that it can measure the outside pressure.
A highly accurate device known as a radar altimeter is
used when the aircraft is close to the ground. A radar
signal is bounced off the terrain below to determine the
aircraft's AGL height. This information is used in a ground
proximity warning system that alerts the pilot before
the altitude becomes dangerously low. Future systems will
benefit from the global positioning satellite system (GPS)
because an airborne GPS receiver can determine position
as well as altitude. A computer database that is part
of the system stores the elevation of terrain and obstacles
and constantly monitors the safe separation of the aircraft.
Because maintaining a safe distance from obstacles is
of utmost importance to aviation safety, jet transport
systems use three independent altimeter systems. Altitude
information is backed up by a radar altimeter and ground
proximity alerting system. Even though the current system
is incredibly safe, future innovations using satellites
and computers will undoubtedly enhance air safety even
further.
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