The temperature in the troposphere primarily changes due to the varying absorption of solar radiation and the mixing of air masses. As altitude increases, temperature generally decreases because the Earth's surface absorbs solar energy and radiates it as heat, warming the air closest to it. Additionally, weather phenomena, such as convection currents, cloud cover, and precipitation, can also influence temperature fluctuations within this atmospheric layer. Environmental factors, such as land use and geographic features, further contribute to localized temperature variations.
Air temperature can be measured beyond the troposphere.
The temperature increases with altitude in the troposphere because of the absorption of solar radiation by the Earth's surface, which heats up the air closer to the surface. As you move higher in the troposphere, the air becomes thinner and less able to retain this heat, causing a decrease in temperature.
In general, the temperature in the stratosphere is warmer than in the troposphere because the stratosphere absorbs ultraviolet radiation from the sun. The temperature inversion in the stratosphere creates a stabilizing effect on the atmosphere.
The layer of the atmosphere that has a temperature drop of 6.5 degrees Celsius per kilometer is the troposphere. This temperature change is known as the environmental lapse rate and is a key characteristic of the troposphere, the layer closest to the Earth's surface where weather occurs.
It is -60 Celsius and higher.
Answer question
The air is thinner
it could be the sun and different seasons
dog
In the troposphere, temperature generally decreases as altitude increases. This is due to the decreasing air pressure and the fact that the upper regions of the troposphere are cooler due to their distance from the Earth's surface.
As the altitude increases in the Troposphere, The air temperature decreases. When about 1 kilometer increases in altitude, the air cools about 6.5 degrees Celsius. And at the very top of the Troposphere the air temperature stays the same at around -60 degrees Celsius.
In the troposphere, temperature generally decreases with increasing altitude. This is because the troposphere is heated from the ground up by solar radiation, causing the lower layers to be warmer than the higher layers. This temperature decrease is known as the lapse rate.
As the altitude increases in the Troposphere, The air temperature decreases. When about 1 kilometer increases in altitude, the air cools about 6.5 degrees Celsius. And at the very top of the Troposphere the air temperature stays the same at around -60 degrees Celsius.
As the altitude increases in the Troposphere, The air temperature decreases. When about 1 kilometer increases in altitude, the air cools about 6.5 degrees Celsius. And at the very top of the Troposphere the air temperature stays the same at around -60 degrees Celsius.
As you increase in altitude in the troposphere, the temperature usually decreases. This is because the air becomes less dense with higher altitude, leading to less heat retention and a decrease in temperature.
The temperature of troposphere is not constant. It varies from -51C to 17 Celcius.
Air temperature can be measured beyond the troposphere.