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Convection currents cause the air to rise when heated. This causes the air pressure to become lower on the surface, which then pulls in air from nearby regions, which is felt as wind.
Air pressure is the type of energy that causes all winds and breezes. When horizontal differences in parcels of air occur, it generates wind. The flow of the air travels from areas of higher pressure to areas of lower pressure.
The curved paths of global winds and surface currents are caused by warm air near the equator.
There is more water vapor present in the air when it is warmer because it is hotter and it causes more evaporating to occur and the liquid is turning into a gas.
Little wind and much afternoon rain occur in the doldrums because near the equator, the Sun heats the air and causes it to rise, creating low pressure and little wind. The rising air then cools, causing rain.
Convection
Convection currents
I am guessing yes. Because seikuken means air sphere which is the range of your motions. so, if you can train to analyze the 'range' of your arms in a circular motion then it's highly possible.
It is the weight of the air itself that causes air pressure. Fluctuations occur due to changes in wind and temperature. We live in air pressure of about 15 pounds per square inch.
When you do fast motions you push the air and it producers vibrations.
It is from differing temperatures of air above it that causes currents to flow in the water.
Eddy - a circular movement of water, counter to a main current twinkle- a circular movement of air
Conventional cells are the large circular patterns that travel in air.
you breathe in and out or you would die!!!! <><><> The movement of the diaphragm is what causes the air to go in and out of your lungs.
Air moves in large, circular patterns called convection cells.
It is during the spring that there are may collisions between warm air and cold air. This causes thunderstorms which in turn can produce tornadoes.
Convection currents cause the air to rise when heated. This causes the air pressure to become lower on the surface, which then pulls in air from nearby regions, which is felt as wind.