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A dry season is a period of extended rainless weather that causes a significant water imbalance. This is a key characteristic of the tropical wet-dry climate, abbreviated as Aw in the Köppen classification system. In these climates, temperatures remain high year-round, but there is a noticeable difference between the wet and dry periods. Most precipitation occurs during the high-sun, or summer, season, while the dry season lengthens as one moves away from the equator. The dry season is caused by the shift in tropical circulation, where the subtropical anticyclone brings dry, stable air. Signs of drought include crop damage, reduced water levels, increased soil erosion, and a higher risk of wildfires.12

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