How Do Cold and Warm Fronts Form and Affect Weather?

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A front is the boundary between two distinct air masses, with cold fronts displacing warm air and vice versa. This movement is primarily driven by wind, which results from pressure systems in temperate latitudes, such as the Icelandic Low and Azores High. Air flows from high to low pressure, creating vortices known as (anti-)cyclones. A cold front occurs when a cyclone drags a cold air mass equatorward, while a warm front happens when a warm air mass is pulled poleward. The key distinction between cold and warm fronts lies in which air mass is advancing and displacing the other. Understanding these dynamics is essential for interpreting weather patterns.
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On the Weather Channel you hear all about how a Cold Front is moving in and how there will be a lot of wind...etc. But does anyone know how the cold/wram fronts work? Where they originate? What causes them? Their effect?
 
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Did you already look at the wikipedia articles?

In the simplest terms, a front is simply the imaginary boundary line between two distinct air masses. If a cold front is "moving in" on a region, it means that a mass of colder air is in the process of displacing a mass of warmer air, and vice versa. The usual reason for such movement is, almost by definition, wind. Wind, in turn, has a variety of causes.

In the temperate latitudes, the most commonplace are transient or semi-permanent pressure systems - Europeans, say, will be familiar with the "Icelandic Low" and "Azores High" as examples of the latter type. Air flow follows the density gradient, i.e. it streams into a low pressure system and out of a high pressure system. Because of the Coriolis_effect, the streamlines curl one way or the other, depending on the nature of the pressure system and the hemisphere, so instead of a simple sink or source one gets a vortex. Technically, these are known as (anti-)cyclones, just like the tropical storms with which that term is more closely associated in common usage - the basic mechanism is the same. If the cyclone picks up a cold air mass along its polarward edge and drags it along, around its Eastern or Western edge, we have a cold front moving equatorwards. Vice versa, if it picks up a warm air mass along its equatorward edge and drags that along, we have a warm front moving polarwards.
 
Notice that since every "front" involves cold and warm air masses, the distinction between a "cold front" and a "warm front" is which one is moving and pushing the other one away.
 
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