1.Looking down on a Northern Hemisphere extratropical cyclone, surface winds blow [(clockwise and outward)(counterclockwise and inward)] about the center. [ ]c|ockwise and outward [ ]counterclockwise and inward 2.The speci?c track of an extratropical cyclone?s low-pressure center across Earth?s surface is largely determined by large-scale horizontal winds blowing [(near Earth?s surface)(in the middle and upper troposphere)]. [ ]near Earth?s surface [ ]in the middle and upper troposphere 3.As a cyclone advances, the system typically progresses through a life cycle. As a cyclone develops, the central pressure of the system [(rises)(falls)] and surface winds strengthen. At maturity, clouds cover a broad area about the low center and associated precipitation is widespread. [ ]rises [ ]falls 4.|n 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. [ ]cold [ ]warm 5.To the north and west of the center of an extratropical cyclone, surface winds are likely to be producing [(cold)(warm)] air advection. [ ]cold [ ]warm 6.Dewpoints are likely to be relatively high to the [(southeast)(northwest)] of the cyclone?s center. [ ]southeast [ ]northwest 7.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 ?ying 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)]. [ ]shrinks
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