Here are the essential concepts you must grasp in order to answer the question correctly.
Atmospheric Layers
The atmosphere is divided into several layers based on temperature gradients and altitude. The main layers include the troposphere, stratosphere, mesosphere, thermosphere, and exosphere. Each layer has distinct characteristics, such as temperature changes and the presence of specific gases, which influence weather patterns and climate.
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Temperature Gradient
The temperature gradient refers to the change in temperature with altitude in the atmosphere. This gradient is crucial for distinguishing between the different atmospheric layers, as each layer exhibits unique temperature behaviors. For instance, the troposphere generally cools with altitude, while the stratosphere warms due to ozone absorption of UV radiation.
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Pressure Variation
Atmospheric pressure decreases with increasing altitude, which is another property used to differentiate the layers of the atmosphere. As one ascends through the layers, the density of air molecules decreases, leading to lower pressure. This variation in pressure is essential for understanding weather phenomena and the behavior of gases in the atmosphere.
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