Air Masses and Fronts Chapter 17 Section 1
![Air Masses and Fronts Chapter 17 Section 1 Air Masses and Fronts Chapter 17 Section 1](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-1.jpg)
![Air Masses and Fronts n Today’s weather can be influence by air from thousands Air Masses and Fronts n Today’s weather can be influence by air from thousands](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-2.jpg)
![Types of Air Masses n Scientists classify air masses according to temperature and humidity Types of Air Masses n Scientists classify air masses according to temperature and humidity](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-3.jpg)
![Types of Air Masses n n Cold, dense air has a high pressure, while Types of Air Masses n n Cold, dense air has a high pressure, while](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-4.jpg)
![Maritime Tropical Warm, humid air masses form over the tropical oceans n In summer, Maritime Tropical Warm, humid air masses form over the tropical oceans n In summer,](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-5.jpg)
![Maritime Polar n Cool, humid air masses form over the icy cold North Pacific Maritime Polar n Cool, humid air masses form over the icy cold North Pacific](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-6.jpg)
![Continental Tropical n Hot, dry air masses form mostly in summer over dry areas Continental Tropical n Hot, dry air masses form mostly in summer over dry areas](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-7.jpg)
![Continental Polar Large continental polar air masses form over central and northern Canada and Continental Polar Large continental polar air masses form over central and northern Canada and](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-8.jpg)
![](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-9.jpg)
![Types of Fronts Air masses are commonly moved by the prevailing westerlies and jet Types of Fronts Air masses are commonly moved by the prevailing westerlies and jet](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-10.jpg)
![Cold Fronts Occurs when a rapidly moving cold air mass runs into a slowly Cold Fronts Occurs when a rapidly moving cold air mass runs into a slowly](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-11.jpg)
![Warm Fronts A fast moving warm air mass takes over a slow moving cold Warm Fronts A fast moving warm air mass takes over a slow moving cold](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-12.jpg)
![Stationary Front Occurs when warm and cold air masses meet, but neither one can Stationary Front Occurs when warm and cold air masses meet, but neither one can](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-13.jpg)
![Occluded Front Most complex weather situation n Warm air mass gets caught between two Occluded Front Most complex weather situation n Warm air mass gets caught between two](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-14.jpg)
![Cyclones The L on a weather map stands for “low” and indicates an area Cyclones The L on a weather map stands for “low” and indicates an area](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-15.jpg)
![Anticyclones n Opposite of a cyclone----high pressure centers of dry air n Marked on Anticyclones n Opposite of a cyclone----high pressure centers of dry air n Marked on](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-16.jpg)
- Slides: 16
![Air Masses and Fronts Chapter 17 Section 1 Air Masses and Fronts Chapter 17 Section 1](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-1.jpg)
Air Masses and Fronts Chapter 17 Section 1
![Air Masses and Fronts n Todays weather can be influence by air from thousands Air Masses and Fronts n Today’s weather can be influence by air from thousands](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-2.jpg)
Air Masses and Fronts n Today’s weather can be influence by air from thousands of kilometers away n A huge body of air that has similar temperature, humidity, and air pressure at any given height is called an air mass n A single air mass may spread over millions of square kilometers and be up to 10 kilometers deep
![Types of Air Masses n Scientists classify air masses according to temperature and humidity Types of Air Masses n Scientists classify air masses according to temperature and humidity](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-3.jpg)
Types of Air Masses n Scientists classify air masses according to temperature and humidity n Four major types of air masses influence the weather in North America: maritime tropical, continental tropical, maritime polar, and continental polar n Recall: Temperature affects air pressure
![Types of Air Masses n n Cold dense air has a high pressure while Types of Air Masses n n Cold, dense air has a high pressure, while](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-4.jpg)
Types of Air Masses n n Cold, dense air has a high pressure, while warm, less dense air has a lower pressure Tropical, or warm, air masses from in the tropics and have low air pressure Polar, or cold, air masses form north of 50° north latitude and south of 50 ° south latitude Maritime air masses form over oceans n n Typically very humid air Continental form over land n Typically drier air
![Maritime Tropical Warm humid air masses form over the tropical oceans n In summer Maritime Tropical Warm, humid air masses form over the tropical oceans n In summer,](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-5.jpg)
Maritime Tropical Warm, humid air masses form over the tropical oceans n In summer, typically bring hot, humid weather n Many summer showers and thunderstorms in Eastern United States caused by this n In winter, humid air mass can bring heavy rain/snow n
![Maritime Polar n Cool humid air masses form over the icy cold North Pacific Maritime Polar n Cool, humid air masses form over the icy cold North Pacific](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-6.jpg)
Maritime Polar n Cool, humid air masses form over the icy cold North Pacific and North Atlantic oceans n Affect West Coast more than East coast n Typically bring fog, rain and cool temperatures to the West in summer
![Continental Tropical n Hot dry air masses form mostly in summer over dry areas Continental Tropical n Hot, dry air masses form mostly in summer over dry areas](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-7.jpg)
Continental Tropical n Hot, dry air masses form mostly in summer over dry areas of the Southwest and Northern Mexico n Cover a smaller area than other air masses n Move Northeast bringing hot, dry air to the Great Plains
![Continental Polar Large continental polar air masses form over central and northern Canada and Continental Polar Large continental polar air masses form over central and northern Canada and](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-8.jpg)
Continental Polar Large continental polar air masses form over central and northern Canada and Alaska n Bring bitterly cold weather with very low humidity n Bring cold, clear, dry air to much of North America in the winter n Storms may occur when continental polar air masses move south and collide with maritime tropical air masses moving north n
![](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-9.jpg)
![Types of Fronts Air masses are commonly moved by the prevailing westerlies and jet Types of Fronts Air masses are commonly moved by the prevailing westerlies and jet](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-10.jpg)
Types of Fronts Air masses are commonly moved by the prevailing westerlies and jet streams in the US n Colliding air masses can form four types of fronts: cold fronts, warm fronts, stationary fronts, and occluded fronts n Type is determined by the characteristic of the air masses and how they are moving n
![Cold Fronts Occurs when a rapidly moving cold air mass runs into a slowly Cold Fronts Occurs when a rapidly moving cold air mass runs into a slowly](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-11.jpg)
Cold Fronts Occurs when a rapidly moving cold air mass runs into a slowly moving warm air mass n Since cold fronts move quickly, they can cause abrupt weather changes, including thunderstorms, clouds, and precipitation n After a cold front moves through, colder, drier air often moves in along with clear skies, a shift in wind, and lower temperatures n
![Warm Fronts A fast moving warm air mass takes over a slow moving cold Warm Fronts A fast moving warm air mass takes over a slow moving cold](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-12.jpg)
Warm Fronts A fast moving warm air mass takes over a slow moving cold air mass n If warm air is humid, light rain or snow will fall n If warm air is dry, scattered clouds form n B/c warm fronts move slowly, it may be rainy or cloudy for several days n After a warm front moves through, the weather is likely to be warm and humid n
![Stationary Front Occurs when warm and cold air masses meet but neither one can Stationary Front Occurs when warm and cold air masses meet, but neither one can](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-13.jpg)
Stationary Front Occurs when warm and cold air masses meet, but neither one can move the other n Where the warm and cool air meet, water vapor in the warm air condenses into rain, snow, fog, or clouds n If it stays stalled over an area, it may bring many days of clouds and precipitation n
![Occluded Front Most complex weather situation n Warm air mass gets caught between two Occluded Front Most complex weather situation n Warm air mass gets caught between two](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-14.jpg)
Occluded Front Most complex weather situation n Warm air mass gets caught between two cold air masses n Two cold air masses mix and the warm air mass is cut off n Becomes cooler or cold on the ground n
![Cyclones The L on a weather map stands for low and indicates an area Cyclones The L on a weather map stands for “low” and indicates an area](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-15.jpg)
Cyclones The L on a weather map stands for “low” and indicates an area of relatively low air pressure n A swirling center of low air pressure is called a cyclone n Cyclones play a large part in the weather of the US n Cyclones and decreasing air pressure associated with clouds, wind, and precipitation n
![Anticyclones n Opposite of a cyclonehigh pressure centers of dry air n Marked on Anticyclones n Opposite of a cyclone----high pressure centers of dry air n Marked on](https://slidetodoc.com/presentation_image/ab25872532734a292eb214eb743fe146/image-16.jpg)
Anticyclones n Opposite of a cyclone----high pressure centers of dry air n Marked on a weather map with an H n The descending air in an anticyclone generally causes dry, clear weather
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