
Global Wind Patterns
Presentation
•
Science
•
6th - 8th Grade
•
Hard
Joseph Anderson
FREE Resource
12 Slides • 18 Questions
1
LESSON:
Local Winds and Global,
Jet Streams, and Coriolis Effect
2
I CAN STATEMENT
I can explain the influence of convection,
global winds, and the jet stream on weather
and climatic conditions.
3
LOCAL WINDS
Local winds form due to differences in air pressure caused by the uneven heating of the Earth's surface. Here's how the process works:
UNEVEN HEATING OF LAND AND WATER:
Land heats up and cools down more quickly than water. During the day, the land gets warmer than
the nearby water bodies (like lakes or oceans). At night, the land cools down faster than the water.
DIFFERENCE IN AIR PRESSURE:
- Warm air is less dense and rises, creating an area of low pressure.
- Cool air is denser and sinks, creating an area of high pressure.
AIR MOVEMENT FROM HIGH TO LOW PRESSURE:
Air always moves from areas of high pressure to areas of low pressure. This movement of air
creates wind.
4
Multiple Choice
What causes local winds to form?
Changes in humidity
The Earth's gravitational pull
Differences in air pressure due to uneven heating
The Earth's rotation
5
Multiple Choice
What happens to warm air as it rises?
It creates an area of high pressure
It creates an area of low pressure
It becomes cooler and denser
It forms clouds
6
Multiple Choice
What does cool air do because it is denser than warm air?
It sinks and creates high pressure
It rises and creates low pressure
It expands and creates wind
It absorbs heat from the land
7
Multiple Choice
How does air move in relation to pressure differences?
From warm areas to cool areas
From areas of low pressure to areas of high pressure
From the ocean to the land
From areas of high pressure to areas of low pressure
8
Multiple Choice
How does air move in relation to pressure differences?
From warm areas to cool areas
From areas of low pressure to areas of high pressure
From the ocean to the land
From areas of high pressure to areas of low pressure
9
TYPES OF LOCAL WINDS:
At night, the land cools down faster than the water. The air over the water remains warmer, creating low pressure. Cooler air from the land (which has higher pressure) moves toward the water, creating a land breeze.
During the day, the land heats up faster than the water. Warm air over the land rises, creating low pressure. Cooler air from the ocean (which has higher pressure) moves in to replace the rising warm air, forming a sea breeze.
10
Multiple Choice
During a land breeze, where does the cool air come from?
From the ocean
From the clouds
From the land
From the sun
11
Multiple Choice
What causes a land breeze at night?
The land cools down faster than the water
The water cools down faster than the land
The air over the land becomes warmer than the air over the water
The land heats up faster than the water
12
Multiple Choice
What happens during a sea breeze?
Cool air from the land moves toward the ocean
Warm air from the ocean moves toward the land
Cool air from the ocean moves toward the land
Warm air from the land moves toward the ocean
13
Multiple Choice
Why does a sea breeze occur during the day?
The ocean heats up faster than the land
The land heats up faster than the water
The ocean cools down faster than the land
The air over the land stays cooler than the air over the ocean
14
Global Wind Patterns
Trade Winds flow through the tropics. They steer tropical storms in the ocean.
•Westerlies (originate from the west)move air masses and fronts.
Polar winds or Easterlies( originate from the east) They are cold and dry winds that blow around the north and south poles
15
Explore : Stations rotations
students will work in groups to annotate the picture in the stations.
we have 3 minutes to complete activity
Switch to the next station/activity
To be Graded
16
Labelling
Annotate the picture with the correct label
horse shoe latitude
horse shoe latitude
doldrums
westerlies
trade winds
doldrums
trade winds
polar easterlies
polar easterlies
westerlies
17
CORIOLIS EFFECT
The Coriolis Effect is the apparent deflection of moving objects (like air masses or ocean currents) caused by the rotation of the Earth. It influences wind patterns and ocean currents.
18
How the Coriolis Effect Works:
Earth's Rotation: The Earth rotates on its axis from west to east. This rotation affects how objects move across the surface.
Deflection Direction:
In the Northern Hemisphere, moving objects (including air) are deflected to the right of their direction of travel.
In the Southern Hemisphere, moving objects are deflected to the left of their direction of travel.
Impact of Latitude:
The Coriolis Effect is strongest at the poles and weakest at the equator. At the equator, there is little to no deflection because the rotational speed is highest there.
As you move towards the poles, the Coriolis Effect increases, leading to more significant deflection.
19
Importance of Coriolis Effect
The Coriolis Effect is crucial for understanding weather systems and climate. It helps explain why cyclones rotate in different directions in the two hemispheres: hurricanes in the Northern Hemisphere rotate counterclockwise, while in the Southern Hemisphere, they rotate clockwise.
20
Multiple Choice
What causes the Coriolis Effect?
The gravitational pull of the moon
The Earth's rotation
The uneven heating of the Earth's surface
Changes in atmospheric pressure
21
Multiple Choice
Which of the following best describes the movement of air due to the Coriolis Effect?
Air moves in a straight line from high to low pressure
Air remains stationary
Air moves only vertically
Air is deflected sideways as it moves
22
Multiple Choice
The Coriolis Effect is crucial for understanding which of the following phenomena?
The size of ocean waves
The melting of polar ice caps
The rotation of hurricanes
The temperature of ocean currents
23
Multiple Choice
In which direction are moving objects deflected in the Northern Hemisphere due to the Coriolis Effect?
To the right
To the left
Straight ahead
Circular or rotating
24
WHAT IS A JET STREAM?
A JET STREAM is a fast, narrow, and powerful air current that flows high in the atmosphere, typically at altitudes of around 6 to 12 miles (10 to 20 kilometers) above the Earth's surface. Jet streams are found in the upper levels of the troposphere and lower stratosphere and usually form at the boundaries between large air masses of different temperatures, such as the polar regions and warmer areas closer to the equator.
25
KEY FEATURES OF JET STREAMS
High Speed: Jet streams can travel at speeds of 100 to 200 miles per hour (160 to 320 kilometers per hour) or more.
Narrow Bands: They are relatively narrow, often a few hundred miles wide, but can stretch for thousands of miles around the Earth.
Westerly Winds: In most cases, jet streams flow from west to east due to the rotation of the Earth, but they can shift and meander north and south, which affects weather patterns.
26
TWO MAIN TYPES OF JET STREAMS?
1. POLAR JET STREAM: Found closer to
the poles, this jet stream separates cold polar air from warmer air to the
south. It tends to have stronger winds
and plays a key role in weather systems
in mid-latitude regions.
2. SUBTROPICAL JET STREAM: Located
closer to the equator, this jet stream
forms near the boundary between
tropical and subtropical air masses.
27
Multiple Choice
What causes jet streams to form?
The Earth's gravitational pull
Differences in air pressure near the ocean
The boundaries between large air masses of different temperatures
Changes in humidity levels and convection currents
28
Multiple Choice
In which direction do jet streams typically flow?
North to South
South to North
East to West
West to East
29
Multiple Choice
Where are jet streams typically located in the atmosphere?
In the lower troposphere and the surface of the Earth
In the upper levels of the troposphere and lower stratosphere
Near the Earth's surface
In between the stratosphere and mesosphere
30
Multiple Choice
How can jet streams affect air travel?
Planes flying with a jet stream can move faster
Jet streams always slow planes down
Jet streams cause planes to rise in altitude
Jet streams prevent planes from flying at high altitudes
LESSON:
Local Winds and Global,
Jet Streams, and Coriolis Effect
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