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Published byJanel Harris Modified over 8 years ago
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Chapter 3
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3.1 Air Mass – large volume of air in which temperature and humidity are nearly the same in different locations at the same altitude Front – is a boundary between air masses High Pressure system – is formed when air moves all the way around a high pressure center. Low pressure system – is a large weather system that surrounds a center of low pressure
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The weather changes when a new air mass moves into your area An air mass is a large volume of air in which temps and humidity are nearly the same in different locations at the same altitude Can cover thousands of square kilometer
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There are different characteristics of air masses Characteristics depend on region where is located Characteristics of air masses are classified into categories according to the characteristics of the regions
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First word of an air mass category name tells whether the air mass formed over dry land or water Describes the moisture of the air mass Continental – formed over land. Air is dry because moisture is pulled to dry land below it Maritime – formed over water. Air becomes moist as water is pulled from the water below
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The second category tells whether air mass formed close to the equator. Describes air mass temp Tropical – Form near the equator. Air becomes warm as it gains energy from warm land or water Polar – Form far from equator. Air becomes cool as t loses energy to cold land or water Combination of words gives the characteristics. Ex: Maritime tropical – moist and warm Continental polar mass – dry and cold
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Air masses can travel away from originated regions Move with global pattern of winds In US, generally move west to east Can move along with jet stream in more complex and changing patterns When moving to new region, takes characteristics with it While moving over earths surface, surface characteristics begin to change the air mass Can take weeks or days to change entire air mass If air mass moves quickly, it may not change much
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Fronts and Weather Different types of fronts produce different patterns of weather Cold Front – moves into regions quickly. Mass of cold and dense air moves forward and warmer air is pushed upward. Produce tall cumulonimbus clouds and precipitation. Brief heavy storms likely. Cool and clear air after
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Warm fronts – move more slowly than cold fronts. Warm air moves gradually up and over cold dense air. Moisture in warm air condenses along front producing clouds. When approaching, high cirrus clods, then high stratus clouds, and then lower and lower stratus clouds appear
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Stationary Fronts – occur when air masses first meet or when a cold or warm front stops moving For a while, boundary between masses stays in same location Each one can move sideways or upward Upward may produced clouds that cover sky for days at a time When movement begins, will become a warm or cold front
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High Pressure system Letter H on a map Air sinks slowly down Near the ground, spreads out toward areas of lower pressure In Northern Hemisphere, Coriolis effect makes air turn clockwise as it moves outward Formed when air moves all the way around a high pressure center Large and change slowly Air mass may form if in one location for a while and can be warm or cold Generally brings clear skies and calm air Sinking air evaporates clouds
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Low Pressure System Begins as air moves around and inward toward the lowest pressure and then up to higher altitudes Upward motion lowers the air pressure, moves faster Rising air produces stormy weather In Northern Hemisphere, LPS circles counterclockwise Can develop wherever there is a center of low pressure Often happens along a boundary of warm and cold air masses Larger systems such as LPS generally move with global winds, west to east
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Section 3.2 Low pressure Systems can become storms Tropical Storms – is a LPS that starts near the equator and has winds that blow at 65 kilometers/hour or more Hurricane – a tropical LPS with winds blowing at speeds of 120 kilometers/hour or more(74 mph) Storm surge – huge masses of ocean water pushed into a costal area by a hurricane Blizzard – blinding snowstorms with winds of at least 56 kilometers per hour (35mph) and low temps usually below 7ºC (20ºF)
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Hurricanes form over warm water At the equator, warm water provides energy to turn LPS into violent storms Energy makes warm air rise faster Clouds and strong winds develop Wind blow from different directions into the LPS The Coriolis effect then bends their paths into a spiral Winds blow faster and faster around the LPS center and this becomes the storm center Hurricanes are called typhoons or cyclones when formed over Indian ocean or western pacific ocean
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Formation of Hurricanes In US, Hurricanes occur most often between August and October Energy from warm water is necessary for LPS center to build into a hurricane Waters are warm enough only near the end of summer Hurricanes and TS generally move westward with trade winds Near land, they move north, south or back east As long as water is warm, storm will grow Cool waters and moving over land will decrease winds which cause the storm to shrink
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Center of the hurricane is a small area of clear weather Called the eye Air moves downward Air moves quickly around and upward along the eye Forms a tall ring of cumulonimbus clouds Ring produces heavy rains and winds
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Effects of Hurricanes Lift cars, uproot trees and tear off building roofs Can produce tornadoes Flooding Storm surges in coastal areas
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Storm surges Sea levels rise several meters Back up rivers Flooding shores Can be deadly and destructive Large waves add to destruction Damage can take weeks or months to clean up
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National Hurricane Center Helps people know when to prepare for hurricanes Puts out TS or hurricane watch within a 36 hour period Helps people evacuate or moved away to safety areas Issues warnings within a 24 hour or less period Warning stays in effect until danger has passed
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Winter Storms Produce Snow and Ice Not caused by LPS Occur when two air masses collide National Weather Service will alert within 48 hours of storm Warning means conditions are already present or will affect an area shortly
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Blizzards Storms where wind blows snow into so it is difficult to see Occur in many parts of the northern and central US Can knock down trees and powerlines Without heat, buildings can become cold, water pipes freeze and roofs can cave in
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Lake-Effect Snowstorms Some of the heaviest snowfall is in the Great Lakes area Cold air rom NW gains moisture and warmth as it passes over the great lakes Over cold land, it cools and releases moisture as snow. Can cover areas downward of GL with clouds and snow even when the rest of the region is clear
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Ice Storms Rain freezes as it is touching the ground and other surfaces Ice covered roads are slippery and dangerous Branches or even whole trees will begin to break Can shut down entire cities
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Section 3.3 Vertical air motion can cause Severe Storms Thunderstorm – a storm with lightning and thunder Tornado – a violently rotating column of air stretching from a cloud to the ground
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Thunderstorms for from rising moist air
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