Weather Changes as Air Masses Move

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Presentation transcript:

Weather Changes as Air Masses Move Chapter 3 section 1 Notes

Air masses are large bodies of air. An air mass is a large volume of air in which the temperature and humidity are nearly the same throughout. An air mass can cover many thousands of square kilometers. The air gradually takes on the characteristics of the land or water below it.

What air masses bring as they move As an air mass moves, it brings its temperature and moisture to new locations. When an air mass moves to a new region, it carries along its characteristic moisture and temperature.

How Weather Systems move from Place to Place (Air Masses Video) http://player.discoveryeducation.com/index.cfm?guidAssetId=5CDF74DF-97DC-4BA1-996A-C13E68455E0E&blnFromSearch=1&productcode=US (c. 3:54 Min.)

Weather changes where air masses meet. Warm and cold air masses don’t mix together, they stay separate from each other A front is a boundary between air masses. The weather near a front can differ from the weather inside the rest of an air mass.

Fronts and Weather Different types of fronts produce different patterns of weather. When a cold, dense air mass pushes warmer air, it produces a cold front. When a warm air mass pushes colder air, it produces a warm front. A Cold front Photo

Cold Fronts Cold fronts can move into a region quickly. Cold fronts often produce tall cumulonimbus clouds and precipitation. Brief heavy storms are likely. Strong thunderstorms can develop and form tornadoes.

Cold Fronts & Weather After the storms, the air is cooler and often very clear. Triangles show the direction that a cold front moves. Draw a cold front symbol here!

Warm Fronts Warm fronts move more slowly than cold fronts.                                                                                                                                                                                                                  Warm fronts move more slowly than cold fronts. Warm air moves gradually up and over a mass of denser and colder air. Moisture in the warm air condenses all along the sloping front, producing cloud-covered skies.

A warm front approaches As a warm front approaches, you may first see high cirrus clouds, then high stratus clouds, then lower and lower stratus clouds.

Cloud progression of a warm front 2 1 3 4

Warm Fronts & Weather Often, a warm front brings many hours of steady rain or snow. After the front passes, the air is usually warmer. Semicircles show the direction that a warm front moves. Draw a warm front symbol here!

Stationary Fronts Stationary fronts occur when air masses first meet or when a cold or warm front stops moving. For a while, the boundary between the air masses stays in the same location – it stays stationary. The air along the front can still move sideways or upward.

Stationary Fronts Continued The upward air motion may produce clouds that cover the sky, sometimes for days at a time. (This can produce severe flooding.) When the front starts moving, it becomes a warm front if the warm air advances and pushes the cold air. Alternating triangles and semicircles show a stationary front. Draw a stationary front symbol here!

Weather Fronts Video http://player.discoveryeducation.com/index.cfm?guidAssetId=5CDF74DF-97DC-4BA1-996A-C13E68455E0E&blnFromSearch=1&productcode=US (C. 3:03 Min.)

High and Low Pressure Systems H = center of High Pressure System L = center of a Low pressure system.

High Pressure Systems At a high-pressure center, air sinks slowly down. As the air nears the ground, it spreads out toward areas of lower pressure. In the Northern Hemisphere, the Coriolis effect makes the air turn clockwise as it moves outward. http://www.bom.gov.au/lam/Students_Teachers/pressure.shtml

High Pressure Systems Continued A high-pressure system is formed when air moves all the way around a high-pressure center. A high-pressure system generally brings clear skies and calm air or gentle breezes.

Low-pressure Systems A low-pressure system is a large weather system that surrounds a center of low pressure. It begins as air moves around and inward toward the lowest pressure and then up to higher altitudes. The rising air produces stormy weather.

Low-pressure Systems Continued The rising air produces stormy weather. In the Northern Hemisphere, the air in a low-pressure system circles in a counterclockwise direction.

Cold Fronts go with High-pressure Systems & Thunderstorms This video shows a thunderstorm formed along a cold front (Thunderstorms 7:30 Min) http://player.discoveryeducation.com/index.cfm?guidAssetId=3CE03830-3031-4DFC-928B-84E8B80CBDC7&blnFromSearch=1&productcode=US

Warm fronts go with Low-pressure Systems Rain Shower Blizzard Tropical Storm Hurricane Andrew

Weather Changes as Air Masses Move Knowing how to identify different types of fronts, low and high pressure systems, and the weather associated with them, will help you prepare for whatever weather lies ahead.