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As a unit of air increases in altitude in the troposphere, the pressure
Conduction
ionosphere
Decreases
stratosphere
Troposphere
Thermosphere
0-30 degrees North and South of the equator
Surface
The densenst part of the atmosphere is in the
Conduction
ionosphere
Decreases
stratosphere
Troposphere
Thermosphere
0-30 degrees North and South of the equator
Surface
CFC's destroy ozone found in the
Conduction
ionosphere
Decreases
stratosphere
Troposphere
Thermosphere
0-30 degrees North and South of the equator
Surface
The layer in the atmosphere where radio signals bounce off of is called the
Conduction
ionosphere
Decreases
stratosphere
Troposphere
Thermosphere
0-30 degrees North and South of the equator
Surface
Energy from the Sun is absorbed mostly by Earth's
Conduction
ionosphere
Decreases
stratosphere
Troposphere
Thermosphere
0-30 degrees North and South of the equator
Surface
A temperature inversion occurs in this layer of the atmosphere
Conduction
ionosphere
Decreases
stratosphere
Troposphere
Thermosphere
0-30 degrees North and South of the equator
Surface
The Trade winds occur at a latitude of
Conduction
ionosphere
Decreases
stratosphere
Troposphere
Thermosphere
0-30 degrees North and South of the equator
Surface
Energy transfer when particles of matter touch each other is called
Conduction
ionosphere
Decreases
stratosphere
Troposphere
Thermosphere
0-30 degrees North and South of the equator
Surface
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