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FRONTS

FRONTS. (Chapter 11, pp. 306–319). Fronts occur in the boundary zone between polar and tropical air masses. World War I Aerial Photograph. “ No man ’ s land ”. trenches. trenches. Ben Franklin ’ s Storm (Nov. 2, 1743). 500 mb. Boston. L. L. Philadelphia. Norwegian Cyclone Model.

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FRONTS

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  1. FRONTS (Chapter 11, pp. 306–319)

  2. Fronts occur in the boundary zone between polar and tropical air masses.

  3. World War I Aerial Photograph “No man’s land” trenches trenches

  4. Ben Franklin’s Storm (Nov. 2, 1743) 500 mb Boston L L Philadelphia

  5. Norwegian Cyclone Model polar/tropical air mass boundary waves form along fluid density boundaries cold front moves faster than warm front (pp. 322–324) cold front catches warm front warm air is pinched upward storm dies

  6. Typical Cold Front • Convective precipitation • 50–100 mile wide • band along front

  7. Cold Front Cross-Section Cold fronts are rapidly advancing cold (dense) air wedges. Warm (often moist) air is forced upward along and ahead of the surface front.

  8. Typical Warm Front • Clouds and precipitation • precede surface front • Stratiform clouds starting • about 750 miles from front • Stratiform precipitation starting • about 350 miles from front “Overrunning”

  9. Warm Front Cross-Section Warm fronts are receding cold (dense) air wedges. Warm air gradually fills in the space vacated by the cold air.

  10. WARM AIR Warm Front Cross-Section COLD AIR

  11. Occluded Front

  12. OCCLUDED FRONTS • Heavy precipitation along front • Convective or stratiform • Short duration

  13. Occluded Front Cross-Section (“Cold Occlusion”)

  14. “Warm Occlusion”

  15. Occluded Front Cross-Section (“Warm Occlusion”)

  16. “Warm Occlusion”

  17. Cold Occlusion Warm Occlusion coldest air is behind cold front coldest air is ahead of warm front

  18. (QUASI-) STATIONARY FRONT Partly cloudy or cloudy with widespread stratiform precipitation

  19. Cyclone Family Cold Air Warm Air (pp. 306–319)

  20. Quick Summary—Fronts (Chapter 11): • Fronts are boundary zones between polar and tropical air masses. • Fronts are stable—the colder, denser air is close to the surface and warmer, less dense air is above it. • Cold front weather: cumuliform clouds, showery, convective precipitation along the front. • Warm front weather: stratiform clouds and precipitation in the cold air well ahead of the front. • Occluded front weather: very heavy precipitation of short duration in the vicinity of the front.

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