FAA PPL Handbook of Aeronautical Knowledge 2003 Chap 10-12

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Whether preparing for a local flight or a long

cross-country, flight-planning decisions based on

weather can dramatically affect the safety of the flight.

A solid understanding of weather theory provides the

tools necessary to understand the reports and forecasts

obtained from a Flight Service Station weather

specialist and other aviation weather services.

This chapter is designed to help pilots acquire the

background knowledge of weather principles necessary

to develop sound decision making skills relating to

weather. It is important to note, however, that there is

no substitute for experience.

NATURE OF THE ATMOSPHERE

The atmosphere is a mixture of gases that surround the

Earth. This blanket of gases provides protection from

ultraviolet rays as well as supporting human, animal,

and plant life on the planet. Nitrogen accounts for 78

percent of the gases that comprise the atmosphere,

while oxygen makes up 21 percent. Argon, carbon

dioxide, and traces of other gases make up the remaining

1 percent. [Figure 10-1]

Within this envelope of gases, there are several

recognizable layers of the atmosphere that are defined

not only by altitude, but also by the specific

characteristics of that level. [Figure 10-2]

The first layer, known as the troposphere, extends

from sea level up to 20,000 feet (8 km) over the

northern and southern poles and up to 48,000 feet (14.5

km) over the equatorial regions. The vast majority of

weather, clouds, storms, and temperature variances

1% Trace Gases

21% Oxygen

78% Nitrogen

Figure 10-1. Composition of the atmosphere.

Troposphere-The layer of the atmosphere extending from the surface

to a height of 20,000 to 60,000 feet depending on latitude.

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occur within this first layer of the atmosphere. Inside

the troposphere, the temperature decreases at a rate of

about 2° Celsius every 1,000 feet of altitude gain, and

the pressure decreases at a rate of about 1 inch per

1,000 feet of altitude gain. At the top of the troposphere

is a boundary known as the tropopause, which traps

moisture, and the associated weather, in the

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