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Answer :
Final answer:
A low-pressure system is characterized by an ascending mass of air, which leads to cloud formation and precipitation. In the Northern Hemisphere, air flows counterclockwise into these systems. This process is crucial for understanding weather patterns.
Explanation:
Understanding Low-Pressure Systems
A low-pressure system is characterized by an ascending mass of air. This occurs because as air moves into the low-pressure area from the surrounding regions, it converges and is forced upward due to the lower pressure at the surface. This process results in cooling and condensation of moisture, often leading to precipitation and cloudy weather.
In the Northern Hemisphere, air flows in a counterclockwise direction into the center of a low pressure system. This is due to the Coriolis effect, which alters the direction of the wind as it moves. Consequently, low-pressure systems are typically associated with storms and wet weather conditions.
Contrarily, a high-pressure system is characterized by a descending mass of air, which leads to clearer skies and dry weather as the air diverges at the surface.
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