Subsidence in the context of the atmosphere refers to the gradual downward movement of air in the atmosphere. This phenomenon is typically associated with high-pressure systems, where air masses are forced to sink due to various factors, including cooling, gravitational forces, and the loss of buoyancy. When air descends, it becomes compressed, which can lead to warming and drying of the air mass. This process can have significant impacts on weather and climate, often resulting in clear skies and dry conditions.
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