The reason the temperature increases with increasing altitude is because of what temperature is measured by: the speed of molecules. In the stratosphere, there is very little gas, and molecules can move very quickly because they are not bouncing off of each other (and other factors). Therefore, by the strict definition of 'temperature', the stratosphere is hotter.
However, due to the low amount of gas at that level of the atmosphere, if YOU were to be there (with a gas mask) you would feel terribly cold (aside from feeling like you're being sucked apart by the partial vacuum). The reason for this is that though the 'temperature' is high, there are very very few molecules flying around bouncing into you and warming you. Therefore your body would receive very little heat from the surroundings--BUT you would radiate away a bunch of heat, causing you to be very very cold very quickly. That is also why astronauts need to be careful about the 'cold temperature' of space. But that's a different story.
The stratosphere's temperature increases as altitude increases. The mesosphere's temperature decreases as it's altitude increases. This is helpful
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.
In the atmosphere, temperatures increase with altitude in the stratosphere. This layer, which lies above the troposphere, contains the ozone layer that absorbs and scatters ultraviolet solar radiation, leading to a warming effect as altitude increases. Consequently, the stratosphere experiences a temperature inversion, contrasting with the troposphere, where temperatures typically decrease with altitude.
As a jet ascends from Earth's surface into the stratosphere, the exterior temperature typically decreases initially due to the troposphere's temperature gradient, which generally cools with altitude. However, once the jet reaches the stratosphere, the temperature begins to stabilize and can even increase slightly with altitude due to the absorption of ultraviolet radiation by the ozone layer. This transition leads to a more stable temperature profile in the stratosphere compared to the cooler, turbulent conditions of the troposphere.
The layers of the atmosphere, starting from the Earth’s surface, are the troposphere, stratosphere, mesosphere, thermosphere, and exosphere. In the troposphere, temperature generally decreases with altitude. However, in the stratosphere, temperature starts to increase with altitude due to the absorption of ultraviolet radiation by the ozone layer. In the mesosphere, temperatures again decrease with altitude, while in the thermosphere, temperatures rise dramatically as altitude increases.
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.
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.
stratosphere and thermosephere -Nikki Gallagher
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.
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 stratosphere's temperature increases as altitude increases. The mesosphere's temperature decreases as it's altitude increases. This is helpful
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.
In the stratosphere, the temperature generally remains constant or may even slightly increase with increasing altitude. This is due to the absorption of ultraviolet radiation by the ozone layer, which warms the stratosphere.
The temperature in the stratosphere increases with altitude, a phenomenon known as temperature inversion. This occurs due to the absorption of ultraviolet (UV) radiation by ozone, which warms the stratosphere. As a result, the stratosphere is characterized by warmer temperatures at higher altitudes, differing from the troposphere below it, where temperature generally decreases with altitude. This temperature structure plays a crucial role in atmospheric dynamics and weather patterns.
The temperature of the stratosphere increases primarily due to the absorption of ultraviolet (UV) radiation by ozone molecules. As UV radiation from the sun is absorbed, it causes the ozone layer to warm up, leading to an increase in temperature in the stratosphere. This temperature inversion is a key characteristic of the stratosphere, contrasting with the troposphere below, where temperature typically decreases 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.