How do low-pressure systems typically affect weather?

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Low-pressure systems are characterized by rising air, which leads to the cooling and condensing of moisture in the atmosphere. This process results in the formation of clouds and precipitation, often creating unstable and stormy weather conditions. When air rises in a low-pressure system, it tends to draw in surrounding air, promoting more cloud development and potential thunderstorms. Thus, regions under the influence of a low-pressure system are typically marked by overcast skies, rain, or even severe weather events.

In contrast, the options that speak to clear skies, stable weather, and increased sunshine are more indicative of high-pressure systems, which promote sinking air and generally lead to fair weather. The notion that low-pressure systems have no significant impact on weather contradicts their fundamental role in driving various meteorological phenomena, including rain and storms. This understanding aligns with standard meteorological principles that describe how atmospheric pressure influences weather patterns.

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