As the altitude increases, the temperature in the troposphere will decrease. The troposphere is the lowest portion of planet's atmosphere.
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 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.
As you move from the troposphere (closest to the surface) to the stratosphere, temperature generally decreases with altitude due to the decreasing density of the air. In the stratosphere, temperature starts to increase with altitude due to the absorption of solar radiation by ozone. Overall, the trend is a decrease in temperature with altitude in the troposphere and an increase in temperature with altitude in the stratosphere.
it is basically nothing.
The temperature changes within the stratosphere with increasing distance from the earth. The temperature increases with altitude, reaching a maximum of about 2 degrees Celsius This is unlike the troposphere, where the temperature decreases with increasing altitude. The heating is caused by the ozone layerbecause as it absorbs solar radiation, the heat around the ozone layer charges the particles in the upper stratosphere as it releases some energy, increasing its temperature. This is also simply known as conduction. Unlike the troposphere, the stratosphere is generally stable, and the warmer air does not cool down and fall like how it does in the troposphere.
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 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 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.
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.
As you move from the troposphere (closest to the surface) to the stratosphere, temperature generally decreases with altitude due to the decreasing density of the air. In the stratosphere, temperature starts to increase with altitude due to the absorption of solar radiation by ozone. Overall, the trend is a decrease in temperature with altitude in the troposphere and an increase in temperature with altitude in the stratosphere.
As you move from the troposphere to the stratosphere, temperature generally increases with altitude due to the absorption of ultraviolet radiation by the ozone layer. Conversely, in the troposphere, temperature decreases with altitude because of the decreasing pressure and density of air. Density also decreases with altitude in both the troposphere and stratosphere, as the air becomes less compressed and thinner at higher elevations. This trend continues through the mesosphere and into the thermosphere, where temperature again rises sharply despite the low density.
In the troposphere, the temperature generally decreases with increasing altitude due to lower air pressure. In the stratosphere, the temperature remains relatively constant then begins to increase due to the absorption of solar radiation by ozone. In the mesosphere and thermosphere, the temperature decreases again as altitude increases due to a decrease in the density of air molecules.
There are four layers of the atmosphere. At the ground is the troposphere, followed by the stratosphere, mesosphere and thermosphere. Temperature decreases with height through the troposphere, increases in the stratosphere, decreases in the mesosphere, then increases again in the thermosphere.
it is basically nothing.
The temperature changes within the stratosphere with increasing distance from the earth. The temperature increases with altitude, reaching a maximum of about 2 degrees Celsius This is unlike the troposphere, where the temperature decreases with increasing altitude. The heating is caused by the ozone layerbecause as it absorbs solar radiation, the heat around the ozone layer charges the particles in the upper stratosphere as it releases some energy, increasing its temperature. This is also simply known as conduction. Unlike the troposphere, the stratosphere is generally stable, and the warmer air does not cool down and fall like how it does in the troposphere.