fronts where two air masses meet, but do not mix
TRANSCRIPT
FRONTSWHERE TWO AIR MASSES MEET, BUT DO NOT MIX
COLD FRONT
COLD FRONT• Cold air “crashes” into warm air causing the
warm air to rise quickly.• Water Vapor rises quickly, cools condenses
and creates clouds.• Frequently creates cumulonimbus clouds
which cause severe weather (thunderstorms or even tornadoes)
• Quickly moving front
COLD FRONTSYMBOL ON A WEATHER MAP
WARM FRONT
WARM FRONT• Warm air “slowly creeps” over cold air causing
the warm air to rise slowly.• Water Vapor rises slowly, cools condenses and
creates clouds.• Frequently creates stratus or nimbostratus
clouds which cause longer periods of rain or snow.
• Slowly moving front
WARM FRONTSYMBOL ON A WEATHER MAP
STATIONARY FRONT
STATIONARY FRONT• Similar air masses “sit next to each other”
because neither is “strong enough” to rise over or push under the other.
• Water Vapor rises very slowly, cools condenses and creates clouds.
• Frequently creates stratus or nimbostratus clouds which cause very long periods of light rain or snow.
• Very slow moving front
STATIONARY FRONTSYMBOL ON A WEATHER MAP
OCCLUDED FRONT
OCCLUDED FRONT• Starts as a cold front and warm front. The cold
air forces the warm air away from the surface.• Water Vapor rises, cools condenses and creates
clouds.• Depending on the speed that the warm air rises,
it can create stratus or nimbostratus clouds or cumulonimbus clouds.
• Most complex type of front because it involves 3 different air masses.
OCCLUDED FRONTSYMBOL ON A WEATHER MAP