What Happens if Wind and Air Molecules Converge at High Pressure?
The higher the air pressure, the less the mass or amount of air molecules is in its system, which means air pressure has thinned out. As the winds spiral around the thin air pressure at high temperature, it can deflect the pressure’s upward movement into a downward movement, and its inward spinning motion into a counter-clockwise or outward spinning direction. It becomes a mass of descending and less dense air, spreading out through the Earth’s atmospheric layer, and stabilizes the atmospheric condition. It can cool down the Earth’s temperature, thus preventing too much heat transfer that causes water to vaporize and air molecules to rise. The Earth’s populace then experiences fair weather conditions, under a blue and less cloudy sky. However, if this condition persists for an abnormally long period of time, it can also result in a dry-spell. Most of the water stays in the vast ocean instead of vaporizing and precipitating into rain, as a way of distributing water on land. In other par
