What happens when air masses meet
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What happens when air masses meet? PowerPoint PPT Presentation


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What happens when air masses meet?. What is an air mass?. Large volume of air with uniform temperature and humidity readings Gets its characteristics from where it forms Continental : forms over land (dry) Maritime : forms over water (moist) Tropical : forms near equator (warm)

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What happens when air masses meet?

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What happens when air masses meet?


What is an air mass?

  • Large volume of air with uniform temperature and humidity readings

  • Gets its characteristics from where it forms

  • Continental: forms over land (dry)

  • Maritime: forms over water (moist)

  • Tropical: forms near equator (warm)

  • Polar: forms nearer poles (cold)


Continental Air Masses

Tropical (cT)

Polar (cP)


Maritime Air Masses

Tropical (mT)

Polar (mP)


What happens when different air masses meet?

Boundary between two different air masses is a:

FRONT


Types of Fronts

  • Cold Front

  • Warm Front

  • Stationary Front

  • Occluded Front


What happens in a cold front?


Cold air moves into warmer air


Cold Front

  • Cold air moves in, replaces warm air

  • Cold air is more dense than warm air

  • Cold air pushes warm air up

  • Tall clouds form (cumulus and cumulonimbus)


  • Clouds are right along the front

  • Precipitation is brief, but heavy (thunderstorms)

  • Band of precipitation 75 miles around front

    (about 50 miles ahead and 25 miles behind)


75 miles


  • Air pressure is lowest at front

  • After front passes: colder air mass

    temperature drops

    skies clear

    pressure increases

  • Cold fronts move faster than warm fronts

    (about 30 mph)


Weather map symbol


Warm air moving into cold

Predictions?


Warm air moving in


What happens with a warm front?

  • Warm air mass advances and replaces cold air mass

  • Warm air is less dense than cold

  • Warm air rides above the colder air


Warm Front


  • Clouds start to form 1000 miles ahead of the front

  • Cirrus clouds develop, followed by lower level stratus clouds

  • Belt of precipitation is about 300 miles wide (starting 100-400 miles ahead of the front)


1000 miles


  • Rain (precipitation) is gentle, but may last for a long period (several hours or days)

  • Weather changes slowly (front moves about 20 mph)

  • Warmer air finally replaces the colder air


As the front passes:

  • Temperature increases

  • Skies clear

  • Pressure increases


Weather map symbol


Fronts – boundary that separates 2 air masses with different temperatures


Clouds: altostratus

Warm front


Cold Front


HINT: sudden burst of intense rain over a small area

Cold Front


HINT: this is a squall line

Cold front


Stratus clouds:

warm front


Clouds on Monday

Clouds on Tuesday

Warm front


Another squall line: COLD FRONT

Robin Brueckner 2004


HINT: low gray clouds, long period of light snow

WARM FRONT!!!!!!!!


Cold Front


Cold front

Sharp break between air masses


Stationary Front


Stationary Front

  • A stationary front occurs when the air masses on either side of the front are not moving toward each other.


Stationary Front

  • Neither air mass pushes into the other

  • Generally causes unsettled conditions

    • Rain, clouds, etc…

  • Flooding may occur if front does not pass


OCCLUDED FRONTWarm air mass gets caught between 2 colder air masses and is forced aloft


Formation of an Occluded Front


Occluded Front

  • A cold air mass catches up to another cold air mass

  • Warm air is ‘squeezed’ out in the middle

  • Causes precipitation


Important Vocabulary

  • Air mass

    • (cT, cP, mT, mP, cA)

  • Front

  • Warm front

  • Cold front

  • Occluded front

  • Stationary front


Winds spiral clockwise out of the High and counterclockwise into the LowFronts are low pressure – lousy weatherAfter the front passes – happy weather


Weather in a High

  • Clockwise Rotation

  • Bright, Clear

  • Happy Weather


Hurricanes – counterclockwise low pressure systems (lousy weather)


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