The Earth's atmosphere is divided into several layers, each characterized by distinct temperature gradients and compositional differences. Starting from the surface, these layers are the troposphere, where weather occurs and temperatures decrease with altitude; the stratosphere, which contains the ozone layer and has a temperature increase with altitude; the mesosphere, where temperatures again decrease; and the thermosphere, where temperatures rise significantly due to solar radiation. Beyond the thermosphere lies the exosphere, where atmospheric particles are sparse and can escape into space. Each layer plays a crucial role in weather patterns, climate, and the protection of life on Earth.
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