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The temperature in the atmosphere decreases as altitude increases. The reason for this is there is less warmth from the surface of the earth reaching the higher altitudes because there are fewer particles of the atmosphere to transfer the heat. The temperature begins to increase, however, around 100km in altitude because of the heat and radiation from the sun.
the umber of collisions increases
Air density decreases with altitude, warmer temp and moisture
it decreses as you go up. At the stratopause the temp is +4C, and at mesopause it is - 90C.
its located in the stratosphere its temp averages -60°C. But temp. rises as alitiude increases in the stratosphere. This happens because the ozone in the stratosphere absorbs ultraviolet radiation from the sun, which warms the air.I got my info fromHolt Science & TechnologyWeather and ClimateHolt, Rinehart and WinstonA Hardcourt Education CompanyOrlando- Austin- New York- San Diego-Toronto- London
The temperature of the Troposphere generally decreases as altitude increases.
The temperature in the atmosphere decreases as altitude increases. The reason for this is there is less warmth from the surface of the earth reaching the higher altitudes because there are fewer particles of the atmosphere to transfer the heat. The temperature begins to increase, however, around 100km in altitude because of the heat and radiation from the sun.
as altitude increases in the troposphere the temp. decreases. on average for every 1 kilometer increase in altitude the air gets about 6.5 Celsius degrees cool.
the temp stays the same
The temp rises
the umber of collisions increases
Air density decreases with altitude, warmer temp and moisture
it decreses as you go up. At the stratopause the temp is +4C, and at mesopause it is - 90C.
It is 3.6 Fahrenheit degrees.
Air pressure decreases as you move away from the earth into the atmosphere. Think of it as the air above you pushes down on you. The farther up you go, the less air is above you to push down. Air temp also decreases as you go up.
The temp in the atmosphere approaches -90C at an altitude of 80 kilometers.
Temperature (rate increases with temp increase) Pressure (rate again increases with press increase) Concentration (rate increases with concentration increase) Particle size (rate increases with smaller particles) Catalyst increases rate.