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Air Masses and Severe Weather. Integrated Science. Air Mass. Huge volumes of air that can cover entire continents or oceans Several types that each have specific characteristics see text p. 689. Atmospheric Lifting. Clouds are indicators of weather

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Presentation Transcript
air mass
Air Mass
  • Huge volumes of air that can cover entire continents or oceans
  • Several types that each have specific characteristics
  • see text p. 689
atmospheric lifting
Atmospheric Lifting
  • Clouds are indicators of weather
  • For clouds to form, air must be lifted
  • Three types of lifting cause clouds.
lifting type 1
Lifting Type #1
  • Convectional Lifting
  • Earth’s surface is heated by the sun, which heats the air mass above it. The heated air will then rise.
convectional lifting1
Convectional Lifting
  • If cooling occurs near the air mass’ saturation temperature, often cumulus clouds may form
convectional lifting2
Convectional Lifting
  • Often happens in the mid-west during summer
atmospheric lifting type 2
Atmospheric Lifting Type #2
  • Orographic Lifting
  • An air mass is pushed upward over an obstacle, such as a mountain range.
atmospheric lifting type 2 orographic
Atmospheric Lifting Type #2Orographic
  • As the air mass is pushed over the obstacle, the air mass will lose moisture in the form of clouds, rain, or snow
atmospheric lifting type 23
Atmospheric Lifting Type #2
  • The clouds dump their load of rain on the windward slope
  • The down slope (leeward) air will be dry = rain shadow
rain shadow
Rain shadow
  • Western Kansas is so dry only certain short grasses can grow; not enough rain for trees
orographic lifting chinook winds
Orographic Lifting – Chinook Winds
  • At the high elevations of the top of a mountain, the air pressure is low.
  • As the air descends the mountain is under more pressure.
  • The increased air pressure heats the air causing warm winds called Chinook Winds
  • Temperatures can rise 20-300 as air moves down the mountain
atmospheric lifting type 3
Atmospheric Lifting Type #3
  • Frontal Lifting
  • This occurs at the mesh point between two different temperature air masses.
  • One air mass (warm) is pushed upward by the other (cold).
  • This can be associated with thunderstorms.
frontal lifting
Frontal Lifting
  • Three types of frontal lifting
  • A) warm front
  • B) cold front
  • C) Stationary front
frontal lifting1
Frontal Lifting
  • Cold Front: When a cold air mass moves into a warm air mass.
  • Cold, denser air forces the warm air up where it cools and condenses, forming clouds
cold front
Cold Front:
  • Warm air is abruptly pushed upward, cooling, condensing moisture into cumulus or cumulonimbus clouds
cold front1
Cold Front
  • Notice how steep the angle is between the two air masses
  • Typically brings sudden, heavy rains and storms
warm front
Warm Front
  • WARM FRONT: when a warm air mass moves into a colder,denser air mass.
  • Warm air rides up and over the colder air
warm front2
Warm Front
  • Notice the angle of slope between the two air masses.
warm front3
Warm Front
  • From the ground, one would observe the following cloud sequence
  • A) cirrus
  • B) cirrostratus
  • C) altostratus
  • D) stratus
  • E) nimbostratus
warm front4
Warm Front
  • The weather during a WARM FRONT starts with cirrus clouds about 24-48 hours before the rain begins
  • Cirrus clouds are “at the front of the front”
warm front5
Warm Front
  • As more warm air is pushed upward, more moisture condenses forming cirrostratus clouds
warm front6
Warm Front
  • As warm more warm air is pushed up, heavier clouds form mid-way up over the cold air
  • Altostratus and stratus
warm front7
Warm Front
  • The final cloud type in a warm front is the nimbostratus
  • “nimbo” = “rain”
warm front8
Warm Front
  • Warm front: rain or snow is steady over several hours or days
quiz t or f
QUIZ: T or F
  • For clouds to form, air must be lifted
  • There are FOUR different types of lifting
  • Orographic lifting refers to air movingup and over a mountain
quiz t or f1
QUIZ: T or F
  • Convectional lifting is the circulation of warm air rising, cold air sinking
  • A rain shadow is caused by WET air descending down the leeward side of a mountain
  • A WARM FRONT means warm air is riding up over cold air
  • A WARM FRONT produces sudden, severe rain and storms
thunderstorms
Thunderstorms
  • Cold Fronts
  • Begins with humid air rising, cooling, and condensing into a single cumulus cloud.
  • Cloud builds as they are “fueled” by warm, moist air from below.
thunderstorms1
Thunderstorms
  • The droplets of water grow larger until they are so big that they fall as rain.
thunderstorms con t
Thunderstorms (con’t)
  • Lightning may be associated with T.storms
  • Hits Earth 100 times per second
  • Over 200 people in the US die each year from lightning.
lightning
Lightning
  • Lightning is the cause of thunder
  • returns nitrogen to the soil
  • may cause fires
  • May have helped start pre-biotic formation of amino acids(?)
lightning formation
Lightning Formation
  • During thunderstorms strong updrafts cause molecules to bump together and their charges to separate
  • Negative charges concentrate at the base of the clouds
lightning formation1
Lightning Formation
  • The ground has lost electrons, giving it a positive (+) charge
  • Opposites attract: The (-) from the cloud base is “pulled” to the (+)
  • First downward movement of (-) is called a leader
lightning formation2
Lightning Formation
  • When the (-) and (+) touch, they create a conductive path to the ground.
  • The other (-) rush down this path = lightning
true or false
TRUE or FALSE?????
  • Cumulonimbus clouds can become thunderstorms
  • Stratus clouds produce sudden, severe thunderstorms and lightning
  • Lightning forms because of unequal charges
tornadoes
Tornadoes
  • A funnel shaped cloud that extends downward from a cumulonimbus cloud.
  • Called a tornado only once it hits the ground.
  • Winds inside travel at up to 800km per hour in counterclockwise direction.
hurricanes
Hurricanes
  • Caused by a warm, vertical wind interacting with an existing storm and causing the storm to turn inward and spiral.
  • Wind speeds of up to 300km per hour.
  • Hurricanes grow as more moist air rises into it.
  • Severe winds rotate around a calm, low pressure zone in the middle, which is the eye of the storm.
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