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FRONTS (Chapter 11) Figure 11.12
A weather map showing surface-pressure systems, air masses, fronts, and isobars (in millibars) as solid gray lines. Large arrows in color show air flow. (Green-shaded area represents precipitation.) (Chapter 11)
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FIGURE A surface weather map showing surface-pressure systems, air masses, fronts, and isobars (in millibars) as solid gray lines. Large arrows in color show air flow. (Green-shaded area represents rain; pink-shaded area represents freezing rain and sleet; white-shaded area represents snow.)
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Ben Franklin’s Storm (Nov. 2, 1743) 500 mb L Boston L Philadelphia
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Norwegian Cyclone Model
Page: 323 FIGURE 12.1 The idealized life cycle of a mid-latitude cyclone (a through f) in the Northern Hemisphere based on the polar front theory. As the life cycle progresses, the system moves northeastward in a dynamic fashion. The small arrow next to each L shows the direction of storm movement. (pp. 322–324)
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Typical Cold Front Convective precipitation 50–100 mile wide
band along front Page: 308 FIGURE A closer look at the surface weather associated with the cold front situated in the southern United States in Fig (Solid gray lines are isobars. Green-shaded area represents rain; white-shaded area represents snow.)
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Cold Front Cross-Section
Page: 309 FIGURE A vertical view of a model representing the weather across the cold front in Fig along the line X–X´.
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Typical Warm Front “Overrunning” Clouds and precipitation
precede surface front Stratiform clouds starting about 750 miles from front Stratiform precipitation starting about 350 miles from front “Overrunning” Page: 312 FIGURE Surface weather associated with a typical warm front in winter. A vertical view along the dashed line P-P´ is shown in Fig (Green-shaded area represents rain; pink-shaded area represents freezing rain and sleet; white-shaded area represents snow.)
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Warm Front Cross-Section
Figure 11.19 Vertical view of clouds, precipitation, and winds across the warm front in Fig along the line P–P’.
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Warm Front Cross-Section
WARM AIR COLD AIR Figure 11.19 Vertical view of clouds, precipitation, and winds across the warm front in Fig along the line P–P’.
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Page: 312 FIGURE Vertical view of a model illustrating clouds, precipitation, and winds across the warm front in Fig along the line P–P’.
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FIGURE 11. 22 The formation of a cold-occluded front. The
faster-moving cold front (a) catches up to the slower-moving warm front (b) and forces it to rise off the ground (c). (Green-shaded area in (d) represents precipitation.)
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FIGURE 11. 22 The formation of a cold-occluded front. The
faster-moving cold front (a) catches up to the slower-moving warm front (b) and forces it to rise off the ground (c). (Green-shaded area in (d) represents precipitation.)
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FIGURE 11. 22 The formation of a cold-occluded front. The
faster-moving cold front (a) catches up to the slower-moving warm front (b) and forces it to rise off the ground (c). (Green-shaded area in (d) represents precipitation.)
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OCCLUDED FRONTS Heavy precipitation along front
FIGURE The formation of a cold-occluded front. The faster-moving cold front (a) catches up to the slower-moving warm front (b) and forces it to rise off the ground (c). (Green-shaded area in (d) represents precipitation.) OCCLUDED FRONTS Heavy precipitation along front Convective or stratiform Short duration
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FIGURE 11. 22 The formation of a cold-occluded front. The
faster-moving cold front (a) catches up to the slower-moving warm front (b) and forces it to rise off the ground (c). (Green-shaded area in (d) represents precipitation.)
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Occluded Front Cross-Section (“Cold Occlusion”)
FIGURE The formation of a cold-occluded front. The faster-moving cold front (a) catches up to the slower-moving warm front (b) and forces it to rise off the ground (c). (Green-shaded area in (d) represents precipitation.)
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FIGURE 11. 22 The formation of a cold-occluded front. The
faster-moving cold front (a) catches up to the slower-moving warm front (b) and forces it to rise off the ground (c). (Green-shaded area in (d) represents precipitation.)
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“Warm Occlusion” FIGURE (at left) The formation of a warm-type occluded front. The faster-moving cold front in (a) overtakes the slower-moving warm front in (b). The lighter air behind the cold front rises up and over the denser air ahead of the warm front. Diagram (c) shows a surface map of the situation.
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Figure 11.21 The formation of a warm-type occluded front. The faster-moving cold front in (a) overtakes the slower-moving warm front in (b). The lighter air behind the cold front rises up and over the denser air ahead of the warm front. Diagram (c) shows a surface map of the situation.
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Occluded Front Cross-Section (“Warm Occlusion”)
Figure 11.21 The formation of a warm-type occluded front. The faster-moving cold front in (a) overtakes the slower-moving warm front in (b). The lighter air behind the cold front rises up and over the denser air ahead of the warm front. Diagram (c) shows a surface map of the situation.
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“Warm Occlusion” FIGURE (at left) The formation of a warm-type occluded front. The faster-moving cold front in (a) overtakes the slower-moving warm front in (b). The lighter air behind the cold front rises up and over the denser air ahead of the warm front. Diagram (c) shows a surface map of the situation.
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Cold Occlusion Warm Occlusion
FIGURE The formation of a cold-occluded front. The faster-moving cold front (a) catches up to the slower-moving warm front (b) and forces it to rise off the ground (c). (Green-shaded area in (d) represents precipitation.)
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(QUASI-) STATIONARY FRONT
Partly cloudy or cloudy with widespread stratiform precipitation
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Cyclone Family Cold Air Warm Air (pp. 306–319)
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Station Temp SLP trend CC Wind dir Dew point Precip A B C D E F Low
Falling Cirrostratus SE Moderate No B Overcast, (nb)stratus No, chance light drizzle C Overcast, nb-stratus Slightly higher Continuous rain D Lower Falling then rising nb-stratus or c-nimbus NW to W Slightly lower (?) Mod-hvy rain showers E Rising Clearing NW F No clouds Lower, stabilizing
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cP or mP (Atlantic) cP mT
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Clouds
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Precipitation
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