In the stratosphere, the temperature increases with altitude. This is due to the absorption of ultraviolet radiation by the ozone layer, which warms the upper stratosphere. As you ascend, the air becomes less dense, and the increased energy from the ozone causes the temperature to rise, contrasting with the troposphere below, where temperature typically decreases with altitude.
The altitude of the stratosphere increases as you move upward from the Earth's surface. It starts at around 10-13 kilometers (6-8 miles) and extends up to about 50 kilometers (31 miles) above the Earth's surface.
As distance from the Earth's surface increases, the temperature of the stratosphere generally increases. This warming occurs because the stratosphere contains the ozone layer, which absorbs ultraviolet (UV) radiation from the sun, leading to an increase in temperature with altitude. In contrast, the troposphere, which is the layer below the stratosphere, experiences a decrease in temperature with altitude.
as you go higher the air becomes thinner and colder until eventually you reach space where there is no air and it extremely cold
Yes, the temperature in the stratosphere increases with altitude. This warming occurs because the stratosphere contains the ozone layer, which absorbs ultraviolet (UV) radiation from the sun, leading to higher temperatures at greater heights. In contrast to the troposphere, where temperature generally decreases with altitude, the stratosphere exhibits this temperature inversion due to the presence of ozone.
1,700-foot decrease.
The temperature increases like the stratosphere
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.
Temperature decreases with altitude in the mesosphere due to the decrease in atmospheric pressure with height. This is because the mesosphere is above the stratosphere where the ozone layer absorbs incoming solar radiation, leading to a decrease in temperature as altitude increases.
In the stratosphere, the temperature increases with height. This is due to the presence of the ozone layer near the top of the stratosphere. The ozone layer absorbs incoming UV radiation, and thus the temperatures are warmer at the top of the stratosphere than at the bottom.
The altitude of the stratosphere increases as you move upward from the Earth's surface. It starts at around 10-13 kilometers (6-8 miles) and extends up to about 50 kilometers (31 miles) above the Earth's surface.
As distance from the Earth's surface increases, the temperature of the stratosphere generally increases. This warming occurs because the stratosphere contains the ozone layer, which absorbs ultraviolet (UV) radiation from the sun, leading to an increase in temperature with altitude. In contrast, the troposphere, which is the layer below the stratosphere, experiences a decrease in temperature with altitude.
Decrease
The transition into the stratosphere is marked by the tropopause, which is the boundary between the troposphere and the stratosphere. This layer is characterized by a significant change in temperature gradient; while the troposphere experiences a decrease in temperature with altitude, the stratosphere exhibits a temperature increase due to the absorption of ultraviolet radiation by the ozone layer. The tropopause varies in altitude, typically reaching higher elevations at the equator and lower at the poles.
increase the temparature of the reactants
stratosphere and thermosephere -Nikki Gallagher
as you go higher the air becomes thinner and colder until eventually you reach space where there is no air and it extremely cold
B. Stratosphere. In the stratosphere, temperatures generally increase with altitude due to the presence of the ozone layer, which absorbs ultraviolet radiation from the sun and heats the surrounding air.