True or False: Cold fronts produce a narrow band of weather in front of the front itself.

Cold fronts are characterized by a swift transition from warmer air to cooler air, which results in a narrow band of weather, often depicted as a line of thunderstorms and heavy precipitation. As the cold front advances, the cold air pushes underneath the warm air, causing the warm air to rise rapidly. This lifting action can lead to the formation of cumulonimbus clouds, which typically accompany severe weather such as heavy rain, gusty winds, and sometimes hail or tornadoes. The narrow nature of the weather associated with cold fronts is due to the steep slopes of the frontal boundary, which often results in fast-moving and intense weather phenomena along the frontal line.

While the intensity and specific weather events can vary based on geographic location and seasonal factors, the key characteristic remains that a cold front usually generates concentrated weather activity in a relatively narrow area immediately in front of the frontal boundary. Thus, the statement is true.