The sun does not have an atmosphere. In the earth, the temperature in the different layers is not evenly distributed.
Temperature is the property used to distinguish the layers of the atmosphere
In the atmosphere, vertical mixing processes like convection and turbulence help distribute heat by transferring warm air from the surface to higher altitudes and bringing cooler air downwards. This mixing contributes to the overall temperature balance in the atmosphere by equalizing temperature differences between different layers of the atmosphere.
It depends on their position and the way solar energy is absorbed.
The layers of the atmosphere are classified based on changes in temperature with altitude. These layers include the troposphere, where temperature decreases with height, the stratosphere, where temperature increases due to ozone absorption of UV radiation, the mesosphere, where temperature again decreases, and the thermosphere, which experiences a rise in temperature due to solar activity. Each layer plays a distinct role in Earth's climate and weather patterns.
Why are there so many layers in the atmosphere
Temperature is the property used to distinguish the layers of the atmosphere
In the atmosphere, vertical mixing processes like convection and turbulence help distribute heat by transferring warm air from the surface to higher altitudes and bringing cooler air downwards. This mixing contributes to the overall temperature balance in the atmosphere by equalizing temperature differences between different layers of the atmosphere.
The variable that is used to separate the atmosphere into four layers is temperature. The four layers are the troposphere, stratosphere, mesosphere, and thermosphere, and each layer is defined by changes in temperature with altitude.
The property that separates the Earth's atmosphere into layers is temperature. As you move higher up in the atmosphere, the temperature changes due to the absorption of sunlight and the presence of different gases. This leads to the formation of distinct layers such as the troposphere, stratosphere, mesosphere, thermosphere, and exosphere.
The division of the Earth's atmosphere into layers is based on how temperature changes with altitude. These layers are the troposphere, stratosphere, mesosphere, thermosphere, and exosphere. Each layer has distinct characteristics and plays a specific role in Earth's atmosphere.
temperature
Based on temperature differences.
The division of Earth's atmosphere into layers is based primarily on changes in temperature with altitude. The layers are the troposphere, stratosphere, mesosphere, thermosphere, and exosphere, with each layer characterized by its unique temperature profile and composition. These layers are determined by the balance between the absorption of solar radiation and the emission of infrared radiation by gases in the atmosphere.
it is because all the layers have tempatures that are either cold or hot
it is the ozone layer in the atmosphere because it is what keeps the atmosphere in check of what is happening in the atmosphere.
temperature differences
Based on temperature differences.