Weather patterns are mostly limited to the troposphere.
radiation because it can
The troposphere is the section of the atmosphere in which 95% of weather occurs. the troposphere is where 99% of clouds are and is also the thinnest layer of the atmosphere. the troposphere is thicker in more tropical areas. This is because of the more heat.
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Temperature and altitude are inversely proportional in the troposphere. This means that as one increases, the other decreases. Approximately 165 meters up in the troposphere is equivalent to a 1 degree Celsius drop.
Weather patterns are mostly limited to the troposphere.
the ozone layer in the mesosphere and thermosphere
radiation because it can
Infrared heat rises from the surface of the earth into the troposphere (the lowest level of the atmosphere). It is captured there by greenhouse gases, so the troposphere warms. This is called the greenhouse effect, and too much greenhouse gas means global warming.
cfc's and the ozone layer have no connection with the issue of global warming or with weather events.
Yes they do share the same effect. Global warming is caused by greenhouse gases. These greenhouse gases block the temperature to troposphere. Thus heat cannot escape to Stratosphere.No
nope there are other layers that make up the atmosphere the troposphere is not the only thing.
Stratosphere is affected by global warming. Ozone layer is depleting day by day.
warming up
Infrared heat rises from the surface of the earth into the troposphere (the lowest level of the atmosphere). It is captured there by greenhouse gases, so the troposphere warms. This is called the greenhouse effect, and too much greenhouse gas means global warming.
15 at the surface and up to negative 55 at the tropopause. Temprature decreases by higher altitude (only in troposphere).
The troposphere is the section of the atmosphere in which 95% of weather occurs. the troposphere is where 99% of clouds are and is also the thinnest layer of the atmosphere. the troposphere is thicker in more tropical areas. This is because of the more heat.