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Section 12.2 – Weather Systems. 8 th Grade Earth and Space Science Class Notes. Global Wind Systems. Cold, dense air sinks towards the surface and moves to the tropics where the cold air forces warm air to rise, cool and flow back to the poles (convection current).

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Section 12.2 – Weather Systems


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section 12 2 weather systems

Section 12.2 – Weather Systems

8th Grade Earth and Space Science

Class Notes

global wind systems
Global Wind Systems
  • Cold, dense air sinks towards the surface and moves to the tropics where the cold air forces warm air to rise, cool and flow back to the poles (convection current).
  • Since the Earth spins, moving air curves to the right in the northern hemisphere and to the left in the southern hemisphere.
    • This curving is known as the Coriolis effect
polar easterlies
Polar Easterlies
  • Wind zones between 60 N latitude and the north pole and 60 S latitude and the south pole.
  • Cold, dense air is

deflected in the

eastern direction from

each pole.

  • Ends at a polar front

which causes an area of

stormy weather.

prevailing westerlies
Prevailing Westerlies
  • Located between 30 N and 60 N and 30 S and 60 S.
  • Surface winds move

west toward each pole.

  • Steady winds that move

much of the weather in

the US and Canada.

trade winds
Trade Winds
  • Between 30 N and 30 S
  • Air sinks, warms, and moves toward the equator in and then rises and moves back toward 30 N and 30 S
trade winds horse latitudes
Trade Winds – Horse Latitudes
  • Near 30 N and 30 S, sinking air creates an area of high pressure
  • The Earth’s major deserts are under these high pressure areas
trade winds intertropical convergence zone itcz
Trade Winds – Intertropical Convergence Zone (ITCZ)
  • Near the equator, air is forced upward and creates an area of low pressure
  • Drifts north and south as

seasons change – directly

over equator in Sept. and

March

  • Has bands of cloudiness and

thunderstorms and delivers

moisture to the tropical rain

forests

jet streams
Jet Streams
  • Narrow band of fast wind – can reach up to 185 km/h
  • Position can vary with the seasons
  • Generally located in the region of strongest temperature differences on a line from the equator to a pole
types of jet streams
Types of Jet Streams
  • Major jet streams – called the polar streams; separate polar easterlies from prevailing westerlies and move west to east
  • Minor jet streams – subtropical streams; occur where westerlies meet trade winds
jet streams and weather systems
Jet Streams and Weather Systems
  • Storms form along jet streams and create large-scale weather systems
  • Transport cold surface air to tropics and warm surface air to poles
  • Weather systems

basically follow jet

streams

fronts
Fronts
  • A narrow region between two air masses of different densities
  • Four types:
    • Cold
    • Warm
    • Stationary
    • Occluded
cold front
Cold Front
  • When cold, dense air forces warm, less dense air up a steep slope
  • Causes intense precipitation and thunderstorms
  • Blue line with triangles
    • Triangles point to direction

of the front’s movement

warm front
Warm Front
  • Warm air displaces cold air along a gentle slope
  • Causes widespread, light precipitation
  • Indicated by red line with semicircles

pointing in the direction

of the front’s movement

stationary front
Stationary Front
  • When air masses meet but neither advances
  • Usually occurs between two fronts with small temperature and pressure differences
  • Cause light winds and precipitation
  • Indicated by evenly

spaced, alternating cold

and warm front symbols

occluded front
Occluded Front
  • Rapidly moving cold air mass overtakes a warm front and forces it upward then collides with another cold front
  • Causes strong winds and heavy precipitation
  • Indicated by line with

alternating purple

triangles and semicircles

pointing in the direction

of its movement.

pressure systems
Pressure Systems
  • Air flows from high pressure to low pressure
  • Sinking or rising air in combination with the Coriolis effect causes the formation of rotating high and low pressure systems
  • Air moves in a circular motion around a high or low pressure center
low pressure systems
Low-Pressure Systems
  • Air rises and air from outside spirals in
  • In northern hemisphere, air moves in counterclockwise direction (opposite in southern hemisphere)
  • Causes cloudy weather

and precipitation

high pressure system
High-Pressure System
  • Air sinks and spirals out
  • In northern hemisphere, air moves clockwise (opposite in southern hemisphere)
  • Brings fair weather