The troposphere does not get hotter with increasing altitude because of the way temperature and pressure interact in the atmosphere. As altitude increases, air pressure decreases, leading to a decrease in temperature — a phenomenon known as the environmental lapse rate. The troposphere is heated from below by the Earth's surface, which absorbs solar radiation and warms the air directly in contact with it. Therefore, while the surface is warm, the upper layers of the troposphere remain cooler.
The troposphere does not get hotter with increasing altitude primarily due to the decrease in atmospheric pressure and density, which leads to lower temperatures at higher elevations. Instead, temperature decreases with altitude because the Earth's surface absorbs solar energy and warms the air directly above it. As you ascend, the air becomes less dense and can hold less heat. Additionally, the processes of convection and the cooling effect of rising air contribute to the overall temperature drop with increasing altitude in 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 the troposphere, temperature generally decreases with increasing altitude. On average, the temperature drops about 6.5 degrees Celsius for every kilometer (or about 1.98 degrees Fahrenheit per 1,000 feet) ascended. This decrease occurs because the troposphere is heated primarily by the Earth's surface, which absorbs solar radiation and then radiates heat upward. As altitude increases, the distance from this heat source results in lower temperatures.
The steady decrease in temperature with altitude in the troposphere is called the environmental lapse rate. This is due to the decreasing pressure and density of the air as altitude increases.
The layer of the atmosphere that contains weather is the troposphere. It is the lowest layer of the atmosphere where temperature decreases with increasing altitude and where most weather phenomena occur, including clouds, precipitation, and wind.
The troposphere does not get hotter with increasing altitude primarily due to the decrease in atmospheric pressure and density, which leads to lower temperatures at higher elevations. Instead, temperature decreases with altitude because the Earth's surface absorbs solar energy and warms the air directly above it. As you ascend, the air becomes less dense and can hold less heat. Additionally, the processes of convection and the cooling effect of rising air contribute to the overall temperature drop with increasing altitude in the troposphere.
The troposphere is the layer of the atmosphere that extends to an average altitude of about 12 km. This is where most weather phenomena occur and where temperature generally decreases with increasing altitude.
In the troposphere, temperature typically decreases with increasing altitude due to the adiabatic cooling effect. In the mesosphere, temperature increases with altitude due to absorption of solar radiation by ozone molecules.
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.
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.
it is basically nothing.
in any altitude in the troposphere. :)
In the Earth's atmosphere, temperature decreases with increasing altitude in the troposphere. This is the lowest layer, where weather phenomena occur, and it extends from the surface up to about 8 to 15 kilometers high, depending on location. As altitude increases, the air becomes less dense, leading to a decrease in temperature. Above the troposphere, in the stratosphere, temperature begins to increase with altitude due to the absorption of ultraviolet radiation by the ozone layer.
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.
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.
In the troposphere, temperature generally decreases with increasing altitude. On average, the temperature drops about 6.5 degrees Celsius for every kilometer (or about 1.98 degrees Fahrenheit per 1,000 feet) ascended. This decrease occurs because the troposphere is heated primarily by the Earth's surface, which absorbs solar radiation and then radiates heat upward. As altitude increases, the distance from this heat source results in lower temperatures.
The troposphere is typically colder as you go higher in altitude. On average, the temperature decreases by about 6.5°C for every kilometer increase in altitude within the troposphere.