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In the extratropical cyclone’s warm sector (the area between the warm front and the advancing cold front), surface winds are likely to be producing [(cold)(warm)] air advection.

As the cyclone progresses across Earth’s surface, the cold and warm fronts rotate about the center of low pressure. The motion of the storm system has similarities to that of a flying Frisbee®, that is, a Frisbee spins as it sails through the air (simultaneously exhibiting rotational and translational motions). Typically, the cold front rotates about the center of the low faster than the warm front. Consequently, the extent of the warm sector occupied by relatively warm and humid air at the surface [(shrinks)(increases)]

To the north and west of the center of an extratropical cyclone, surface winds are likely to be producing [(cold)(warm)] air advection.

Most cloudiness associated with a warm front develops over a broad area, often hundreds of kilometers wide, [(ahead of)(behind)] the front. From these clouds, light to moderate precipitation may fall for 12 to 24 hours or longer.

The expected continuing advancement of the cold front and the Low would likely cause residents of the center portion of the country to see [(rapidly rising)(small changes in)(rapidly falling)] temperatures over the next day or so.

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