A) looks at cyclones in two dimensions.
B) has less explanatory power than does the cyclogenesis model.
C) does not account for the comma-shaped cloud pattern often associated with cyclones.
D) focuses on three major flows of air.
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A) favors formation of strong cyclones.
B) is associated with meridional patterns.
C) does not have pronounced vorticity characteristics.
D) is breaking the normal upper-wind flow pattern from east to west.
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A) farther to the north during summer.
B) farther to the south during summer.
C) at higher altitudes during summer.
D) at higher altitudes during winter.
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A) are relatively unaffected by upper-level conditions.
B) are only occasionally affected by upper-level conditions.
C) are strongly affected by upper-level conditions.
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A) Rossby waves.
B) upper level flows.
C) jet streams.
D) all of these
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A) clockwise rotation in the northern hemisphere.
B) clockwise rotation in the southern hemisphere.
C) widespread areas of rising air in the northern hemisphere.
D) widespread areas of rising air in the southern hemisphere.
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A) the surface level and upper level of the troposphere are two distinct layers.
B) the Bjerknes model of cyclogenesis gives the best explanation for the formation and life of mid-latitude cyclones.
C) upper-level divergence has little impact on the surface.
D) the temperature at the surface can affect air flow at upper levels of the atmosphere.
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A) Their widespread sinking motions causes the air to cool.
B) Their widespread rising motions causes the air to cool.
C) Their widespread sinking motions causes the air to warm.
D) Their widespread rising motions causes the air to warm.
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A) warm sector.
B) storm sector.
C) kill sector.
D) chill sector.
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A) localized heating of the air from below.
B) localized cooling of air from below.
C) upper-tropospheric motions.
D) lower-tropospheric motions.
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A) is greatest at the Equator.
B) does not affect absolute vorticity.
C) is a function of latitude.
D) is vorticity relative to the earth's surface.
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A) is not a significant factor in the upper atmosphere.
B) is often detected through examination of the orientation of height contours and isotherms.
C) refers to the vertical movement of warm air.
D) always occurs simultaneously with temperature conduction.
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