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The stratosphere is the layer of the atmosphere that is relatively calm and has stable temperatures. This layer is above the troposphere and contains the ozone layer, which helps trap heat in the atmosphere. Temperatures in the stratosphere increase with altitude due to the absorption of ultraviolet radiation by the ozone layer.
The temperature decreases with altitude.
The upper layers of the atmosphere are heated from above, while the lower layers are heated from below, because infrared radiation is given off by the Earth's surface in response to solar heating. The lower troposphere (with its denser molecules and water vapor) receives heat from both re-radiation and convection. The result is that while the atmosphere always gets thinner with altitude, the temperature decreases with altitude in the troposphere, then increases with altitude in the stratosphere. The very high temperatures in the thermosphere are moot because of the low specific heat (energy capacity) of the tenuous gases there.
No. The temperature usually increasesgreatlytowards the interiors ofthe gas giants.
This temperature variation occurs due to the different layers of the atmosphere interacting with solar radiation in varying ways. In the troposphere, temperature decreases with altitude due to the atmosphere's ability to trap heat. In the stratosphere, temperatures increase because of the presence of the ozone layer which absorbs and traps incoming solar radiation. Finally, in the mesosphere, temperatures drop again as the atmosphere becomes less dense and heat is not as efficiently retained.
The troposphere and the lower stratosphere are the two atmospheric layers that can contain air as warm as 25 degrees Celsius. Temperatures in the troposphere decrease with altitude, but can vary depending on location and weather conditions. In the lower stratosphere, temperatures can increase with altitude due to the presence of the ozone layer.
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.
Temperatures in the stratosphere generally increase with altitude due to the absorption of ultraviolet radiation by the ozone layer. This temperature increase is opposite to the trend in the troposphere, where temperature decreases with altitude.
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.
The troposphere is the layer closest to the Earth's surface where weather events occur and temperature decreases with altitude. The stratosphere is above the troposphere and contains the ozone layer that absorbs ultraviolet radiation, causing temperatures to increase with altitude in this layer.
The stratosphere is warmer at the top because it contains the ozone layer, which absorbs and scatters incoming solar radiation, leading to a temperature increase with altitude. In contrast, the troposphere cools with altitude due to the decrease in air pressure, which results in lower temperatures at higher altitudes.
In the troposphere, temperatures decrease with altitude (air pressure), in the effect known as the adiabatic lapse rate (9.8 °C per thousand feet).
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.
The stratosphere and mesosphere are both layers of the Earth's atmosphere located above the troposphere. The stratosphere contains the ozone layer, which absorbs and scatters solar ultraviolet radiation, while the mesosphere is where most meteoroids burn up upon entering the atmosphere. Additionally, temperatures in the stratosphere increase with altitude due to the absorption of solar radiation, whereas temperatures in the mesosphere decrease with altitude.
The stratosphere is the layer of the atmosphere that is relatively calm and has stable temperatures. This layer is above the troposphere and contains the ozone layer, which helps trap heat in the atmosphere. Temperatures in the stratosphere increase with altitude due to the absorption of ultraviolet radiation by the ozone 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.
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.