The way the layer interacts with solar radiation.
The layer of the atmosphere with the lowest temperature is the mesosphere. Temperatures in this layer can drop as low as -90 degrees Celsius (-130 degrees Fahrenheit).
In the third layer of the atmosphere, known as the mesosphere, temperature decreases with altitude due to the decreasing concentration of ozone molecules. This layer is located above the stratosphere and below the thermosphere in the Earth's atmosphere.
The temperature zone layer of Earth's atmosphere shown in the cross-section is the stratosphere. This layer is characterized by an increase in temperature with altitude due to the presence of the ozone layer, which absorbs and scatters UV radiation from the sun.
The stratosphere has a relatively constant temperature because it contains the ozone layer, which absorbs and traps solar radiation, leading to a stable temperature profile in this layer of the atmosphere.
Layers in Earth's atmosphere are primarily separated based on temperature variations caused by differences in altitude and composition. The troposphere is the layer closest to the Earth's surface, where temperature generally decreases with altitude. Above that is the stratosphere, where temperature begins to increase due to the presence of the ozone layer.
A layer in the atmosphere in which temperature increases with altitude.
The layer of the atmosphere with the lowest temperature is the mesosphere. Temperatures in this layer can drop as low as -90 degrees Celsius (-130 degrees Fahrenheit).
thermosphere
The way the layer interacts with solar radiation.
In the third layer of the atmosphere, known as the mesosphere, temperature decreases with altitude due to the decreasing concentration of ozone molecules. This layer is located above the stratosphere and below the thermosphere in the Earth's atmosphere.
thermosphere
The stratosphere is the layer of the atmosphere where temperature increases with altitude. This is due to the absorption of ultraviolet radiation by the ozone layer, which heats up the surrounding air.
The temperature zone layer of Earth's atmosphere shown in the cross-section is the stratosphere. This layer is characterized by an increase in temperature with altitude due to the presence of the ozone layer, which absorbs and scatters UV radiation from the sun.
The stratosphere has a relatively constant temperature because it contains the ozone layer, which absorbs and traps solar radiation, leading to a stable temperature profile in this layer of the atmosphere.
temperature change
No, you cannot generalize that the higher the layer of the atmosphere, the hotter the temperature. In the troposphere, temperature decreases with altitude due to the decreasing pressure and density of air. However, in the stratosphere, temperature actually increases with altitude because of the absorption of ultraviolet radiation by the ozone layer. Thus, temperature variations in the atmosphere depend on specific layers and their characteristics.
Layers in Earth's atmosphere are primarily separated based on temperature variations caused by differences in altitude and composition. The troposphere is the layer closest to the Earth's surface, where temperature generally decreases with altitude. Above that is the stratosphere, where temperature begins to increase due to the presence of the ozone layer.