地理漫步·世界地理英语30篇（8）
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Monsoon Winds Drive Seasonal Water Patterns
季风驱动季节性水循环格局
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Monsoon winds blow strongly from ocean to land each summer.每年夏季，季风强劲地从海洋吹向陆地。
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They carry huge amounts of moisture across South and Southeast Asia.它们携带大量水汽横跨南亚和东南亚。
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Rain falls heavily on windward mountain slopes and coastal plains.迎风坡的山区和沿海平原降雨猛烈。
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Dry seasons follow when winds reverse and flow inland from land.当风向逆转、从陆地吹向内陆时，便进入旱季。
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Rivers swell in summer, then shrink during winter months.河流在夏季涨水，冬季则逐渐萎缩。
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Farmers time planting to match monsoon arrival and retreat.农民根据季风的到来与退去安排播种时间。
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Cities like Mumbai and Dhaka face flooding and water shortages.孟买和达卡等城市面临洪涝与缺水问题。
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These winds define regional climate, agriculture, and settlement patterns.这些季风塑造了区域气候、农业及聚落格局。