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Monsoon Winds Bring Rain to Half the World
季风将雨水带给世界一半地区
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Monsoon winds shift direction with seasons across tropical and subtropical Asia.季风在热带和亚热带亚洲随季节改变风向。
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Warm ocean air carries moisture inland, then drops heavy rain on mountains.温暖的海洋空气将水汽带入内陆，随后在山区形成强降雨。
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Rice farms depend on summer monsoon rains for planting and growth.水稻种植依赖夏季季风雨进行播种和生长。
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Dry winter monsoons bring cool, clear air from northern continents.干燥的冬季季风从北方大陆带来凉爽晴朗的空气。
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Cities near coasts face flooding during intense monsoon downpours.沿海城市在强季风暴雨期间面临洪涝风险。
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Forests on windward mountain slopes get more rain than dry leeward valleys.迎风坡森林比背风坡干旱河谷降水更多。
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Monsoon timing affects river flow, hydropower, and drinking water supply.季风时间变化影响河流流量、水力发电及饮用水供应。
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Scientists track monsoon strength to predict drought or flood risks yearly.科学家通过监测季风强度来预测年度旱涝风险。