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Winds blow towards the low pressure, and the air rises in the atmosphere where they meet. At any given moment, some areas on the earth’s surface have higher pressure compared to their surroundings, and some have lower pressure Ascending and descending air areas of high and low pressure are caused by ascending and descending air As air warms it ascends, leading to low pressure at the surface
That means they are constantly pushing air away from them into the areas that have lower pressure. The slightly inward moving air in low pressure causes air to converge and since it can’t move downward due to the surface, the air is forced upward, leading to condensation and precipitation as discussed earlier The opposite occurs with high pressure. This outermost layer, extending far into space, experiences an extremely sparse atmosphere, leading to minimal air pressure compared to the denser layers closer to the earth’s surface.
This is called the pressure gradient force. High pressure systems are the controlling factor and determine the direction low pressure systems follow High pressure can push or stop low pressure, but low pressure can never steer or block high pressure even if it is a hurricane. As explained previously, we use an average value of sea level pressure to differentiate between high pressure and low pressure
Because air pressure decreases aloft, the average pressure at any point above the surface is less. Air flows outward from a high pressure center at the surface, leading to sinking motion above the high pressure center This sinking motion is typically associated with clear skies.
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