The winds from the north pole and the south pole along with the heat from the south and the cold from the north.
Warm moist air over the equator creates a zone of convection.
Constant heating from the sun causes air to rise, then flow away from the equator. Sinking air in the subtropics spreads out and some of it flows toward the equator. This creates a "cell" (Hadley Cell) of circulation that constantly generates rising air at the equator and therefore low pressure.
Earths Rotation The Coriolis effect
The high pressure subtropical calm belts known as horse latitudes are between 30 degrees north of the equator and 30 degrees south of the equator. This was an area of either high winds are complete calm.
Around the equator there is no noticeable difference to the seasons, compared to what is experienced by parts of Earth that are much further from the equator. At the poles, can you detect a difference?
The winds from the north pole and the south pole along with the heat from the south and the cold from the north.
The winds from the north pole and the south pole along with the heat from the south and the cold from the north.
Warm moist air over the equator creates a zone of convection.
differences between equator and prime meridian
Air is warmed by the sun, especially near the equator, and becomes less dense. Therefore it rises, and creates an area of lower pressure where it left the Earth's surface. Colder, denser air rushes in to equalise that pressure difference, and that is wind.
everything
There is a difference between poles and equator. It is because depletion is minimum at equator.
it is greater at poles than equator
90 degrees of latitude
Kanyakumari is just 8 degrees away from the equator. As equator receives the direct Sun rays, there won't be hardly any difference between the day & night. Where as, Kashmir is 37 degrees away from the equator. So there can be about 5 hrs difference between day & night.
Constant heating from the sun causes air to rise, then flow away from the equator. Sinking air in the subtropics spreads out and some of it flows toward the equator. This creates a "cell" (Hadley Cell) of circulation that constantly generates rising air at the equator and therefore low pressure.
Constant heating from the sun causes air to rise, then flow away from the equator. Sinking air in the subtropics spreads out and some of it flows toward the equator. This creates a "cell" (Hadley Cell) of circulation that constantly generates rising air at the equator and therefore low pressure.