When two air masses with different properties meet, a frontal surface forms between them, and near the front, the line where that surface meets the ground, clouds form, rain falls, and the wind and temperature change. At a warm front, warm air rides gently up over cold air and light rain falls over a wide area for a long time; at a cold front, cold air drives sharply under warm air and showers pour down over a narrow area. A mid-latitude cyclone carries these two fronts with it as it moves from west to east with the westerlies, and when the faster cold front catches up with the warm front, it forms an occluded front and the low gradually weakens. In the diagram, switching the type of front compares, in cross-section, how steep the frontal surface is and where the clouds and rain are.
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