Cold and warm fronts are associated with different types of pressure systems. A cold front typically advances into an area of warm air, causing the warm air to rise rapidly, often leading to stormy weather and lower pressure. Conversely, a warm front moves into an area of cooler air, resulting in gradual lifting and usually bringing overcast skies and steady precipitation, often associated with higher pressure systems. Both fronts play a crucial role in the dynamics of weather patterns and the movement of air masses.
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