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Chapter: The Atmosphere in Motion

Table of Contents. Chapter: The Atmosphere in Motion. Section 3: Air Masses and Fronts. Air Masses and Fronts. 3. A. Air Masses. 1. Weather changes quickly when a different air mass enters an area.

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Chapter: The Atmosphere in Motion

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  1. Table of Contents Chapter: The Atmosphere in Motion Section 3: Air Masses and Fronts

  2. Air Masses and Fronts 3 A. Air Masses 1. Weather changes quickly when a different air mass enters an area. 2. An air mass is a large body of air that develops over a particular region of Earth’s surface.

  3. Air Masses and Fronts 3 B. Types of Air Masses 1. A mass of air that remains over a region for a few days picks up the characteristics of that area. 2. Six major air masses affect North America.

  4. Air Masses and Fronts 3 C. Fronts 1. Where air masses of different temperatures meet, a boundary between them, called a front, is created. Click image to view movie.

  5. Air Masses and Fronts 3 C. Fronts 2. Air does not mix along a front. Because cold air is more dense, it sinks beneath warm air. 3. The warm air is pushed upward and wind develop. Fronts usually bring a change in temperature as they pass, and they always bring a change in wind direction. 4. There are four kinds of fronts – cold, warm, stationary and occluded.

  6. Air Masses and Fronts 3 D. Cold Fronts 1. When a cold air mass advances and pushes under a warm air mass, the warm air is forced to rise. 2. The boundary is known as a cold front. 3. A narrow band of violent storms can result from a cold front.

  7. Air Masses and Fronts 3 E. Warm Fronts 1. If warm air is advancing into a region of colder air, a warm front is formed. 2. As the warm air mass moves upward, it cools. Water vapor condenses and precipitation occurs over a wide area.

  8. Air Masses and Fronts 3 F. Stationary Fronts 1. A stationary front is a front where a warm air mass and a cold air mass meet but neither advances. 2. Cloudiness and precipitation occur along the front.

  9. Air Masses and Fronts 3 G. Occluded Fronts • An occluded front forms when a fast-moving cold front overtakes a slower warm front. • All types of occluded fronts can produce cloudy weather with precipitation.

  10. Air Masses and Fronts 3 H. High- and Low-Pressure Centers • In areas where pressure is high, air sinks. • As it spreads, the Coriolis effect turns the air in a clockwise direction in the northern hemisphere. • Because the air is sinking, air near a high-pressure center is usually dry with few clouds.

  11. Air Masses and Fronts 3 H. High- and Low-Pressure Centers 4. As air flows into a low-pressure center, it rises and cools. 5. Eventually, the air reaches its dew point and the water vapor condenses, forming clouds and precipitation. 6. Air circulates in a counterclockwise direction in the northern hemisphere in a low-pressure center.

  12. Air Masses and Fronts 3 I. Severe Weather—Thunderstorms 1. Thunderstorms develop from cumulonimbus clouds. 2. Falling droplets collide with other droplets and grow bigger. 3. As these larger droplets fall, they cool the surrounding air, creating downdrafts that spread out at the surface.

  13. Air Masses and Fronts 3 I. Severe Weather—Thunderstorms 4. These are the strong winds associated with thunderstorms. 5. Lightning and thunder also are created in cumulonimbus clouds.

  14. Air Masses and Fronts 3 J. Tornadoes • A tornadois a violent, whirling wind that moves in a narrow path over land. • The powerful updrafts into the low pressure in the center of a tornado act like a giant vacuum cleaner, sucking up anything in its path.

  15. Air Masses and Fronts 3 J. Tornadoes

  16. Air Masses and Fronts 3 K. Hurricanes 1. A hurricane is a large storm that begins as an area of low pressure over tropical oceans. 2. The Coriolis effect causes winds to rotate counterclockwise around the center of the storm.

  17. Air Masses and Fronts 3 K. Hurricanes 3. As the storm moves, it pulls in moisture. The heat energy from the moist air is converted to wind. 4. The sustained winds in a hurricane can reach 250 km/h (155 mph)with gusts up to 300 km/h (186 mph). 5. When a hurricane passes over land, high winds, tornadoes, heavy rains, and storm surge pound the affected region.

  18. Air Masses and Fronts 3 K. Hurricanes 6. After the storm begins traveling over land, however, it no longer has the warm, moist air to provide it with energy, and it begins losing power.

  19. Air Masses and Fronts 3 L. Weather Safety • Using technology such as Doppler radar, as well as weather balloons, satellites, and computer, the position and strength of storms are watched constantly. • If the National Weather Service believes conditions are right for severe weather to develop in a particular area, it issues a severe weather watch.

  20. Air Masses and Fronts 3 M. Watches and Warnings • Watches and warnings are issued for severe thunderstorms, tornadoes, tropical storms, hurricanes, blizzards, and floods. • Local radio and television stations announce watches and warnings, along with NOAA (NOH ah) Weather Radio.

  21. Air Masses and Fronts 3 M. Watches and Warnings 3. During a watch, stay tuned to a radio or television station and have a plan of action in case a warning is issued. 4. If the National Weather Service does issue a warning, take immediate action to protect yourself.

  22. Section Check 3 Question 1 Where is a front most likely to occur?

  23. Section Check 3 Question 2 Explain how lightning forms.

  24. Section Check 3 Question 3 If conditions are right for severe weather to develop in a particular area, what will the National Weather Service issue? A. an advisory B. Doppler radar C. a warning D. a watch

  25. Help To advance to the next item or next page click on any of the following keys: mouse, space bar, enter, down or forward arrow. Click on this icon to return to the table of contents Click on this icon to return to the previous slide Click on this icon to move to the next slide Click on this icon to open the resources file. Click on this icon to go to the end of the presentation.

  26. End of Chapter Summary File

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