Mesoscale refers to atmospheric phenomena that occur at a scale of 2 to 200 kilometers, bridging the gap between microscale events, like turbulence, and large-scale features, such as cyclones. It encompasses various weather patterns and processes, including thunderstorms, sea breezes, and mountain-valley breezes, which can significantly impact local weather and climate. Understanding mesoscale dynamics is crucial for predicting short-term weather events and the behavior of atmospheric systems.
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