Question

In the given figure the direction of wind is from 35° s to 0° and 35° s to 0° Give the Reason

Answer 1

Hey mate,

Here's your answer.. ☺

Explanation :

Generally, the winds from high pressure area are seen to travel towards low pressure region i.e the equator.

• Now we’re getting to the part where wind happens.
• Gases move from high-pressure areas to low-pressure areas.
• And the bigger the difference between the pressures, the faster the air will move from the high to the low pressure.
• That rush of air is the wind we experience.

Reason :

This is something that happens in nature all the time: things always try to even out. It’s called diffusion.

• Warm air rises, creating a low pressure zone; cool air sinks, creating a high pressure zone.
• Air that moves horizontally between high and low pressure zones makes wind.
• The greater the pressure difference between the pressure zones the faster the wind moves.
• Air moving between large high and low pressure systems creates the global wind belts that profoundly affect regional climate.
• Smaller pressure systems create localized winds that affect the weather and climate of a local area.

Hope it helps.. ❤

Answer 2

Explanation :

Generally, the winds from high pressure area are seen to travel towards low pressure region i.e the equator.

Now we’re getting to the part where wind happens.

Gases move from high-pressure areas to low-pressure areas.

And the bigger the difference between the pressures, the faster the air will move from the high to the low pressure.

That rush of air is the wind we experience.

Reason :

This is something that happens in nature all the time: things always try to even out. It’s called diffusion.

Warm air rises, creating a low pressure zone; cool air sinks, creating a high pressure zone.

Air that moves horizontally between high and low pressure zones makes wind.

The greater the pressure difference between the pressure zones the faster the wind moves.

Air moving between large high and low pressure systems creates the global wind belts that profoundly affect regional climate.

Smaller pressure systems create localized winds that affect the weather and climate of a local area.