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Miss Nelson SCIENCE ~ CHAPTER 8 WEATHER
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Air Masses and Fronts SECTION 3
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Which is denser… warm air, or cold air? What do you think happens when warm air and cold air collide? ANTICIPATORY SET
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S 6.4.e – Students know differences in pressure, heat, air movement, and humidity result in change in weather STANDARDS
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What are the major types of air masses in North America, and how do they move? What are the main types of fronts? What type of weather is associated with cyclones and anticyclones? THE BIG IDEA
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Air mass – a huge body of air that has similar temperature, humidity, and air pressure throughout Tropical – a warm air mass that forms in the tropics and has low air pressure Polar – a cold air mass that forms north of 50 degrees latitude or south of 50 degrees latitude and has high air pressure Maritime – a humid air mass that forms over oceans Continental – a dry air mass that forms over land KEY TERMS
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Front – the boundary where unlike air masses meet but do not mix Occluded – cut off, as in a front where warm air mass is caught between two cooler air masses Cyclone – a swirling center of low air pressure Anticyclone – a high-pressure center of dry air KEY TERMS
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Weather can be influenced by air from thousands of kilometers away A huge body of air that has similar temperature, humidity, and air pressure at any given height is called an air mass A single air mass may spread out over millions of square kilometers and be up to 10 kilometers deep AIR MASSES AND FRONTS
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Four major types of air masses influence the weather in North America: Maritime tropical Continental tropical Maritime polar Continental polar TYPES OF AIR MASSES
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The characteristics of an air mass depend on the temperatures and moisture content of the region over which the air mass forms TYPES OF AIR MASSES
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Temperatures affects pressure Cold, dense air has a higher pressure Warm, less dense air has a lower pressure TYPES OF AIR MASSES
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Tropical air masses: Warm air masses Form in the tropics Have low air pressure Polar air masses: Cold air masses Form north of 50° and south of 50° Have high air pressure TYPES OF AIR MASSES
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Whether an air mass is humid or dry depends on whether it forms over water or land TYPES OF AIR MASSES
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Maritime air masses form over water The air can become very humid Continental air masses form over land Have less exposure to moisture from water – are drier TYPES OF AIR MASSES
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Warm, humid air masses form over tropical oceans Gulf of Mexico, Atlantic Ocean In summer time, they bring hot, humid weather Summer showers and thunderstorms In winter, bring heavy rain or snow MARITIME TROPICAL
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Cool, humid air masses form over the icy cold North Pacific and North Atlantic Oceans Affect the west coast more than the east coast Even in summer, they bring fog, rain, and cool temperatures to the west coast MARITIME POLAR
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Hot, dry air masses form mostly in summer over dry areas of the Southwest and northern Mexico Cover a smaller area than other air masses Occasionally move northeast, bringing hot, dry weather to the southern Great Plains CONTINENTAL TROPICAL
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Form over central and northern Canada and Alaska Can bring bitterly cold weather with very low humidity In winter, bring clear, cold, dry air to much of North America In summer, the air mass is milder Storms may occur when continental polar air masses move south and collide with maritime tropical air masses moving north CONTINENTAL POLAR
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Read Types of Air Masses on pages 311- 312 of your textbook TYPES OF AIR MASSES
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In the continental United States, air masses are commonly moved by the prevailing westerlies (winds) and jet streams HOW AIR MASSES MOVE
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The major wind belts over the continental United States Generally push air masses from west to east PREVAILING WESTERLIES
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Embedded within the prevailing westerlies are jet streams Bands of high speed winds about 10 kilometers above Earth’s surface Blow from west to east JET STREAMS
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As huge air masses move across the land and the oceans, they collide with each other They do not easily mix Think about oil and water! Less dense oil floats on top of the denser water Something similar happens when two air masses with different temperatures and humilities collide FRONTS
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The boundary where these air masses meet is called a front Storms and changeable weather often develop along fronts View the picture on page 313 of your textbook FRONTS
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Read How Air Masses Move on page 313 of your textbook HOW AIR MASSES MOVE
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Colliding air masses can form four types of fronts: Cold fronts Warm fronts Stationary fronts Occluded fronts TYPES OF FRONTS
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The type of front that develops depends on the characteristics of the air masses and how they are moving TYPES OF FRONTS
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Cold air is dense and tends to sink Warm air is less dense and tends to rise When a rapidly moving cold air mass runs into a slowly moving warm air mass… The denser cold air slides under the lighter warm air The warm air is pushed upward along the leading edge of the colder air View figure 14 on page 314 of your textbook COLD FRONT
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As the warm air rises, it expands and cools Warm air can hold move water vapor than cool air The rising air reaches the dew point (the temperature at which water vapor in the air condenses into droplets of water) Clouds form If there is a lot of water vapor in the warm air, heavy rain or snow may fall If the warm air mass contains only a little water vapor, then the cold front may be accompanied by only cloudy skies COLD FRONT
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Read Cold Fronts on page 314 of your textbook COLD FRONT
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Clouds and precipitation also accompany warm fronts At a warm front, a fast-moving warm air mass overtakes a slowly moving cold air mass Cold air is denser than warm air, the warm air moves over the cold air If the warm air is humid, light rain or snow falls along the front If the warm air is dry, scattered clouds form Because warm fronts move slowly, the weather may be rainy or cloudy for several days After a warm front passes through an area, the weather is likely to be warm and humid WARM FRONTS
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Read Warm Fronts on page 315 of your textbook WARM FRONTS
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View the diagram on page 315 of your textbook Read Stationary Fronts on page 315 of your textbook STATIONARY FRONTS
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View the diagram on page 315 of your textbook Read Occluded Fronts on page 315 of your textbook OCCLUDED FRONTS
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As air masses collide to form fronts, the boundary between the fronts sometimes becomes distorted Can be caused by surface features such as mountains, strong winds, or jet streams When this happens the air begins to swirl Swirling air can cause a low pressure center to form CYCLONES AND ANTICYCLONES
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When you look at a weather map you will see areas marked with an L Stands for “low” pressure Swirling center of low air pressure is called a cyclone From the Greek word meaning “wheel” Cyclones play a large part in the weather of the United States As air rises in the cyclone, the air cools, forming clouds and precipitation CYCLONES
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Cyclones and decreasing air pressure are associated with clouds, winds, and precipitation CYCLONES
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The opposite of a cyclone High pressure centers of dry air Called “highs” and marked with an H on a weather map Winds spiral outward from the center of an anticyclone, moving toward areas of low pressure ANTICYCLONES
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The descending air in an anticyclone generally causes dry, clear weather ANTICYCLONES
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What two characteristics are used to classify air masses? Of the four types of air masses, which are dry, and which are humid? CHECK FOR UNDERSTANDING
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What two characteristics are used to classify air masses? The two characteristics used to classify air masses are temperature and humidity. Of the four types of air masses, which are dry, and which are humid? Maritime tropical and maritime polar air masses are humid, while continental tropical and continental polar air masses are dry. CHECK FOR UNDERSTANDING
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What type of air mass would form over the northern Atlantic Ocean? What are the four types of fronts? GUIDED PRACTICE
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What type of air mass would form over the northern Atlantic Ocean? The type of air mass that would form over the northern Atlantic Ocean is a maritime polar air mass. What are the four types of fronts? The four types of fronts are cold front, warm front, stationary front, and occluded front. GUIDED PRACTICE
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Complete Weather 8-3 Independent Practice INDEPENDENT PRACTICE
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