A surface low-pressure center could continue to exist if the divergence of air aloft occurred at a rate equal to the inflow of air below. An place where the atmospheric pressure is lower than that of the nearby areas is known as a low-pressure area, low area, or low in meteorology.
High-pressure areas are connected to calmer winds and clearer sky, while low-pressure areas are frequently connected to unfavorable weather . Due to opposing Coriolis forces, winds circle lows in the northern hemisphere counterclockwise and clockwise, respectively. Areas of wind divergence that occur in the upper inflow regions of the atmosphere are where low-pressure systems emerge.
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