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For more on marking an answer as the "Best Answer", please visit our FAQ.The lowest level of the earth�s atmosphere is known as the troposphere. This extends to about 7 or 8 miles (about 12 km). It is within this layer that all of the world�s weather variations take place. As you ascend through this layer generally temperature drops by about one degree Centigrade for each 1,000 feet (300m) until a minimum of around minus 60 degrees Centigrade is encountered. (These are general figures and will vary according to individual local conditions). Some commercial flights provide in-flight data for their passengers and it is not unusual to see outside temperatures of -50 degrees at 35,000 feet.
The reason for this is that atmospheric pressure drops rapidly in these first few miles (85% of the earth�s atmosphere is contained in the troposphere) so there is less air to retain the Sun�s heat.
Above the troposphere is the stratosphere. Here the temperature stabilises and then begins to rise with altitude as the effect of the Sun's radiation takes a hold. Above the stratosphere (c. 50 km) is the mesosphere where the temperature again declines.Above about 85 km comes the thermosphere, where temperature begins to rise again.