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On the average, cold fronts are about twice as steep as warm fronts and travel slower than warm fronts.
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False
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Precipitation associated with a cold front usually occurs along a narrow zone.
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True
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Midlatitude cyclones that form east of the Rockies have a tendancy to northeastward path.
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True
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Cyclones form along fronts and proceed through a generally predictable life cycle.
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True
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On a weather map, occluded fronts are shown with blue triangular points on one side of a line and red semicircles on the other side of the line.
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False
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The most useful model of how a midlatitude cyclone developes is known as the polar-front theory.
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True
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When compared to cold fronts, warm fronts have a greater slope and produce heavier precipitation over a larger area.
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False
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Fronts are boundary surfaces that seperate air masses of different densities.
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True
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The first sign of an approaching warm front is often the appearance of nimbostratus clouds.
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False
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In a midlatitude cyclone, low pressure is centered at the apex of the "wave" where the fronts connect.
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True
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More often than not, the formation of a cyclone is initiated by the flow aloft in the vicinity of the midlatitude jet stream.
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True
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In the classic polar-front model, cyclogenesis occurs when cP air clashes with mT air along a front.
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True
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Cyclogenesis is closely related to convergence aloft.
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False
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When a rapidly moving cold front overtakes a warm front, an occluded front is likely to form.
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True
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Surface airflow in a Southern Hemisphere midlatitude cyclone is counterclockwise.
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False
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