It begins to get warmer from the sun's radiation.
In the stratosphere, temperature increases with altitude due to the absorption of ultraviolet (UV) radiation by the ozone layer, which is concentrated in this atmospheric layer. As altitude increases, the ozone absorbs more UV radiation, leading to a rise in temperature. This contrasts with the troposphere below, where temperature typically decreases with altitude. The temperature inversion in the stratosphere creates a stable atmospheric layer, preventing vertical mixing.
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 temperature in the stratosphere typically rises with altitude due to the absorption of ultraviolet radiation by ozone molecules, which increases the temperature of the surrounding air.
The temperature does not fall in the stratosphere. The temperature rises considerably once you reach this part of the atmosphere. This is because this is where most of the sun's rays are collected before hitting the surface of the earth.
A temperature of 95°C would most likely occur in the stratosphere, particularly in the upper regions where temperatures can rise due to the absorption of ultraviolet radiation by the ozone layer. The stratosphere extends from about 10 to 50 kilometers above the Earth's surface, and temperatures typically increase with altitude in this layer.
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 temperature already rise as you climb up in the stratosphere.
The temperature in the stratosphere typically rises with altitude due to the absorption of ultraviolet radiation by ozone molecules, which increases the temperature of the surrounding air.
Stratosphere. This is because the stratosphere is above the troposphere and contains the ozone layer, which absorbs UV radiation from the sun, causing temperatures to increase with altitude.
In the troposphere, temperatures typically decrease with altitude due to the decrease in air pressure with height. This is known as the lapse rate, with temperatures normally decreasing by about 6.5°C per kilometer. This temperature trend is reversed in the stratosphere where temperatures rise with altitude due to the absorption of solar radiation by ozone.
The temperature typically rises in the stratosphere because of the absorption of ultraviolet solar radiation by ozone molecules. This absorption leads to the heating of the stratosphere, creating a temperature inversion where it gets warmer with altitude.
The stratosphere is primarily heated by the absorption of UV radiation by ozone molecules, leading to an increase in temperature with altitude. This absorption causes the temperature to rise in the lower stratosphere but decreases with altitude due to the decreasing concentration of ozone.
The temperature does not fall in the stratosphere. The temperature rises considerably once you reach this part of the atmosphere. This is because this is where most of the sun's rays are collected before hitting the surface of the earth.
The higher you go - the lower the temperature.
The temperature in the stratosphere rises because it absorbs ultraviolet radiation from the Sun. This radiation heats up the ozone layer in the stratosphere, causing the temperature to increase with altitude.
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.
As the temperature increases, the viscosity of the liquid will decrease.