Where does this occur?
Wind current on a…
1. Local scale.
2. Global scale
WINDS ARE NAMED FROM WHERE THEY COME FROM!
SEA BREEZE Mountain BREEZE Prevailing
Westerlies
NE Trade
Winds
Polar
EasterliesLand BREEZE Valley BREEZE
LOCALIZED WINDS GLOBAL WINDS
Global Winds
• Wind currents that develop
on a GLOBAL SCALE over
long distances.
• Still a result of temperature
and pressure differences.
• Air moves
between the
warm equator
and the cold
poles.
Global
Winds
Global Temperature Patterns
So Air tries to move between the poles from a high to low
pressure = Global Winds
Strong Direct Sunlight!
Warm
Rising air = LOW
pressure
Weaker Indirect
Sunlight!
COLD
Sinking air = HIGH
Pressure
The Coriolis Effect
• Air does not
move in a
straight line
because of
Earth’s rotation.
Coriolis
Effect
Earth spin makes the wind curve
instead of traveling in a straight line.
Curve to the RIGHT in the
NORTHERN HEMISPHERE.
Curve to the LEFT in the
SOUTHERN HEMISPHERE.
Global Winds
LOW PRESSURE
HIGH PRESSURE LOW PRESSURE
HIGH PRESSURE
LOW PRESSURE
HIGH PRESSURE LOW PRESSURE
HIGH PRESSURE
Northern
Hemisphere
Southern
Hemisphere
POLAR EASTERLIES
Prevailing Westerlies
Easterly Trade Winds
Hadley
Cells.
Global Winds
60°
S
30°
S
0°
30°
N
60°
N
Prevailing Westerlies
- From 30°N to
60°N
- Deflected to right
Easterly Trade Winds
- From 30°N to O°
- Deflected to right
Polar Easterlies
- From 90°N to
60°N
- Deflected to right
Easterly Trade Winds
- From 30°S to 0°
- Deflected to left
Prevailing Westerlies
- From 30°S to
60°S
- Deflected to left
Polar Easterlies
- From 90°S to
60°S
- Deflected to left
Doldrums
Remember, winds are
named from where
they come.

Global Wind Patterns

  • 1.
    Where does thisoccur? Wind current on a… 1. Local scale. 2. Global scale WINDS ARE NAMED FROM WHERE THEY COME FROM! SEA BREEZE Mountain BREEZE Prevailing Westerlies NE Trade Winds Polar EasterliesLand BREEZE Valley BREEZE LOCALIZED WINDS GLOBAL WINDS
  • 2.
    Global Winds • Windcurrents that develop on a GLOBAL SCALE over long distances. • Still a result of temperature and pressure differences. • Air moves between the warm equator and the cold poles. Global Winds
  • 3.
    Global Temperature Patterns SoAir tries to move between the poles from a high to low pressure = Global Winds Strong Direct Sunlight! Warm Rising air = LOW pressure Weaker Indirect Sunlight! COLD Sinking air = HIGH Pressure
  • 4.
    The Coriolis Effect •Air does not move in a straight line because of Earth’s rotation. Coriolis Effect Earth spin makes the wind curve instead of traveling in a straight line.
  • 5.
    Curve to theRIGHT in the NORTHERN HEMISPHERE. Curve to the LEFT in the SOUTHERN HEMISPHERE.
  • 7.
    Global Winds LOW PRESSURE HIGHPRESSURE LOW PRESSURE HIGH PRESSURE LOW PRESSURE HIGH PRESSURE LOW PRESSURE HIGH PRESSURE Northern Hemisphere Southern Hemisphere
  • 9.
  • 10.
    Global Winds 60° S 30° S 0° 30° N 60° N Prevailing Westerlies -From 30°N to 60°N - Deflected to right Easterly Trade Winds - From 30°N to O° - Deflected to right Polar Easterlies - From 90°N to 60°N - Deflected to right Easterly Trade Winds - From 30°S to 0° - Deflected to left Prevailing Westerlies - From 30°S to 60°S - Deflected to left Polar Easterlies - From 90°S to 60°S - Deflected to left Doldrums Remember, winds are named from where they come.