Earth Systems Science
A warm front is a boundary that forms when a warm air mass moves into an area occupied by a cooler air mass, causing the warm air to rise over the cooler air. This process leads to a gradual increase in temperature and often results in prolonged precipitation, usually in the form of steady rain or drizzle, as the warm air cools and condenses. Warm fronts are significant because they play a crucial role in shaping weather patterns and phenomena associated with transitioning weather systems.
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