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Fronts Chapter 17 Section 1 Pages 560-566
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Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

Dec 13, 2015

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Page 1: Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

FrontsFrontsChapter 17 Section 1

Pages 560-566

Chapter 17 Section 1

Pages 560-566

Page 2: Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

• The Prevailing Westerlies (a major global wind belt) generally push air masses from west to east in the United States.

How Air Masses Move

Page 3: Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

• The area where air masses meet and do not mix.

• Causes storms and changeable weather.

• Four types.• Determined by the

characteristics of the air masses and how they are moving.

Fronts

Page 4: Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

• A moving warm air mass collides with a slower moving cold air mass.

• Warm air moves over cold air. (warm air is less dense)

• Weather-– Clouds, storms and rain.– If humid air, light rain forms.– If dry- scattered clouds form.– After it passes, it is likely to be warm and

humid.

Warm Fronts

Page 5: Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

Warm Fronts

Page 6: Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

• Cold air is very dense and tends to sink.• Warm (less dense) air is pushed up.• As it rises it cools and forms clouds,

may bring heavy rain or snow.• Move very quickly, can cause abrupt

weather changes including violent T-storms.

• After it moves through, brings cool, dry air with clear skies and cooler temps.

Cold Fronts

Page 7: Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

Cold Fronts

Page 8: Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

• Occurs when cold and warm air masses meet, but neither can force the other to move.

• Water vapor in the warm air condenses into rain, snow, fog or clouds.

• If it stalls over an area, it can bring these conditions for several days.

Stationary Fronts

Page 9: Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

Stationary Fronts

Page 10: Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

• A complex situation that occurs when a cold front catches up with a warm front.

• Pushes warm air up over colder air, cutting the warm air off from the ground.

• Weather-– Ground temp= cool– Brings rain or snowy weather.

Occluded Fronts

Page 11: Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

Occluded Fronts

Page 12: Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

Surface Map

Page 13: Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

Surface Map

Page 14: Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

Surface Map

Page 15: Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

• Cyclone is Greek- meaning “wheel”

• A swirling center of low pressure.– Spin counter-clockwise (due to coriolis effect

winds are turned to the right in the NH)

• L is short for Low Pressure– Air is moving towards the low– Air is rising, forming clouds and precip.– Bring LOUSY Weather

Cyclones

Page 16: Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

• Are areas of high pressure centers

• Winds spiral out from the center towards areas of lower pressure.

– Spin clockwise (due to coriolis effect winds are turned to the right in the NH)

• H= short for High Pressure– Air is moving away from the high.– Cool air is sinking, and warms as it falls.– Clear, dry weather. (Brings HAPPY weather)

Anti-Cyclones

Page 17: Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

Mid-Latitude Cyclones

Page 18: Fronts Chapter 17 Section 1 Pages 560-566 Chapter 17 Section 1 Pages 560-566.

Mid-Latitude Cyclones