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.
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, the lowest layer of Earth's atmosphere, is heated from below. The troposphere is warmest at the bottom near Earth's surface. The troposphere is coldest at its top, where it meets up with the layer above (the stratosphere) at a boundary region called the tropopause. Temperatures drop as you move upward through the troposphere.Sunlight streams down from space through the atmosphere, striking the ground or ocean beneath. The sunlight heats the surface, and that surface radiates the heat into the adjacent atmosphere. Atmospheric scientists use a concept called a "standard atmosphere" to represent an average atmosphere with variations caused by weather, latitude, season, and so forth, removed. In the standard atmosphere model, the temperature at sea level at the bottom of the troposphere is 15° C (59° F). Higher up in the troposphere, where less heat from the surface warms the air, the temperature drops. Typically, the temperature drops about 6.5° C with each increase in altitude of 1 kilometer (about 3.6° F per 1,000 feet). The rate at which the temperature changes with altitude is called the "lapse rate". In the standard atmosphere, by the time you reach the top of the troposphere the temperature has fallen to a chilly -57° C (-70° F).Of course, the atmosphere is always changing and is never "standard". Temperatures in the troposphere, both at the surface and at various altitudes, do vary based on latitude, season, time of day or night, regional weather conditions, and so on. In some circumstances, the temperature at the top of the troposphere can be as low as -80° C (-110° F). When a weather phenomenon called at "temperature inversion" occurs, temperature in some part of the troposphere gets warmer with increasing altitude, contrary to the normal situation.In the layer above the troposphere, the stratosphere, temperature rises with increasing altitude. In the stratosphere, the air is heated from above by ultraviolet "light" which is absorbed by ozone molecules in the air. The tropopause is the boundary between the troposphere (below) and the stratosphere (above). The tropopause occurs where the temperature stops dropping with increasing altitude (in the troposphere) and begins climbing with increasing altitude (the stratosphere).
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. :)
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.
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.
No, the temperature in the troposphere decreases as the altitude increases.
The stratosphere is the layer above the troposphere (where we live). The ozone layer is found in the lower stratosphere. The stratosphere is the lowest layer where temperature increases with increasing altitude.