Fronts and Pressure System
Notes of Doom!
Remember what drives our
climate/weather forces!
Another Example of ConvectionAnother Example of Convection
Convection is heat energy moving as aConvection is heat energy moving as a fluidfluid fromfrom hotter tohotter to
coolercooler areasareas..
Warm air at the ground surface rises as a thermal bubbleWarm air at the ground surface rises as a thermal bubble
expands, consumes energy, and hence cools.expands, consumes energy, and hence cools.
Fronts
• Air masses are large pockets/blobs of air
that move over land
• When 2 air masses collide its called front.
• Fronts- are narrow regions between 2 air
masses of different densities.
• Density of air masses depend on
temperature, pressure, and humidity of air
Cold Front
• Cold, dense air displaces the less dense
warm air.
• Precipitation and T-storms are common
Warm Front
• Warm air displaces cold air
• Light precipitation common along warm
fronts.
Stationary Front
• 2 air masses meet but do not advance
• Frequently occur when both air masses have small
temperature and pressure gradients between them.
• Light winds and light precipitation
Occluded Front
• Cold air moves so fast that it overtakes a warm front and pushes the
warm air upwards.
• Cold air from behind warm front will meet up with cold air in front of
warm front.
• Strong winds and heavy precipitation common along occluded
fronts.
Pressure System
• Air will either rise or sink near the Earth’s
surface.
• Air always from an area of high pressure
to an area of low pressure.
• Sinking or rising air with the Coriolis effect,
results in rotating high and low pressure
systems. (Air moves in a circular motion)
Low-pressure system
• Air rises and air coming in from outside spirals inward towards the
center. Then it continues up.
• Spiraling air is due to coriolis effect
• Air rises, cools, and condenses into clouds and precipitation
(usually)
High-pressure system
• Sinking air moves away from the center when it reaches the Earth’s
surface.
• High pressure systems are usually associated with fair weather.

Fronts and pressure system notes of doom!

  • 1.
    Fronts and PressureSystem Notes of Doom!
  • 2.
    Remember what drivesour climate/weather forces!
  • 3.
    Another Example ofConvectionAnother Example of Convection Convection is heat energy moving as aConvection is heat energy moving as a fluidfluid fromfrom hotter tohotter to coolercooler areasareas.. Warm air at the ground surface rises as a thermal bubbleWarm air at the ground surface rises as a thermal bubble expands, consumes energy, and hence cools.expands, consumes energy, and hence cools.
  • 4.
    Fronts • Air massesare large pockets/blobs of air that move over land • When 2 air masses collide its called front. • Fronts- are narrow regions between 2 air masses of different densities. • Density of air masses depend on temperature, pressure, and humidity of air
  • 5.
    Cold Front • Cold,dense air displaces the less dense warm air. • Precipitation and T-storms are common
  • 6.
    Warm Front • Warmair displaces cold air • Light precipitation common along warm fronts.
  • 7.
    Stationary Front • 2air masses meet but do not advance • Frequently occur when both air masses have small temperature and pressure gradients between them. • Light winds and light precipitation
  • 8.
    Occluded Front • Coldair moves so fast that it overtakes a warm front and pushes the warm air upwards. • Cold air from behind warm front will meet up with cold air in front of warm front. • Strong winds and heavy precipitation common along occluded fronts.
  • 9.
    Pressure System • Airwill either rise or sink near the Earth’s surface. • Air always from an area of high pressure to an area of low pressure. • Sinking or rising air with the Coriolis effect, results in rotating high and low pressure systems. (Air moves in a circular motion)
  • 10.
    Low-pressure system • Airrises and air coming in from outside spirals inward towards the center. Then it continues up. • Spiraling air is due to coriolis effect • Air rises, cools, and condenses into clouds and precipitation (usually)
  • 11.
    High-pressure system • Sinkingair moves away from the center when it reaches the Earth’s surface. • High pressure systems are usually associated with fair weather.