Download Air Masses

Survey
yes no Was this document useful for you?
   Thank you for your participation!

* Your assessment is very important for improving the work of artificial intelligence, which forms the content of this project

Document related concepts
no text concepts found
Transcript
Fronts
Interface (Boundary) between 2 air masses
Colder air mass begins to wedge under the
warmer air mass
Fronts are always a sign of a change in the
weather
Fronts are always associated with LOW
pressure
On a weather map, fronts extend from the
Center of the Low
Low pressure L
Warm front
cP
mT
Cold front
Cold Front
cP air mass
mT air mass
• Cold air is MORE dense than warm air so cold
air displaces warm air
• Steep slope
• Moves quickly
• Showery precipitation (doesn’t last long)
Conditions before a cold front
• Warm
humid
• More ______________
southerly
• Winds usually from ______________
direction
• Pressure ____________
decreases
Conditions after the cold front
• cold
drier
• Air is more_____
North west
• Winds usually from ______________
direction
• Pressure ____________
increases
Vertical clouds
Cumulonimbus
(thunderstorm)
Towering Cumulus
Cumulus
Warm Front
mT
cP
• Warm air is LESS dense than cooler air so
warm air rises up and over the cool air
• Gentle slope
• Extended hours of precipitation
Conditions before a warm front
• cool
easterly
• Winds usually from ______________
direction
Conditions after a warm front
• warm
southerly
• Winds usually from ______________
direction
High level clouds
Cirrus
Cirrostratus
Cirrocumulus
Mid-level clouds
Altostratus
Altocumulus
Low-Level Clouds
Stratus
Nimbostratus
Occluded Front
• Faster, colder air overtakes slower, warm
air
• Warm air is forced up off the ground
• Extended hours of precipitation
Stationary Front
• Neither air mass is moving
• Cold and warm air
• Precipitation similar to warm front
cP
mT
COLD FRONT
WARM FRONT