科学素养与生活应用·英语30篇(4)
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How Ocean Currents Distribute Heat Across Earth’s Surface
洋流如何在全球地表分配热量
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Warm surface currents like the Gulf Stream carry tropical heat northward along eastern coastlines.像墨西哥湾暖流这样的表层暖流,将热带热量沿东海岸向北输送。
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Cold deep currents return cooler, denser water toward the equator in a global conveyor belt.寒冷的深层洋流则以全球输送带的形式,将较冷、密度更大的海水带回赤道附近。
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This thermohaline circulation regulates climate—Europe stays milder than Canada at similar latitudes.这种温盐环流调节着气候——同纬度下,欧洲比加拿大更温暖。
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Melting polar ice adds freshwater, lowering salinity and potentially slowing current flow.极地冰盖融化注入淡水,降低海水盐度,可能减缓洋流速度。
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Satellites track sea-surface temperature and color to map current speed and direction.卫星通过监测海表温度和颜色,绘制洋流速度与方向图。
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Marine ecosystems depend on upwelling zones where cold, nutrient-rich water rises near coasts.海洋生态系统依赖上升流区,即寒冷、富含营养的海水在近岸涌升的区域。
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El Niño events temporarily shift Pacific currents, altering rainfall patterns worldwide.厄尔尼诺事件会暂时改变太平洋洋流,进而影响全球降雨格局。
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Ships and submarines use current data to optimize fuel efficiency and navigation routes.船舶与潜艇利用洋流数据优化燃油效率和航行路线。
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Changes in current strength correlate with long-term droughts and intensified monsoon seasons.洋流强度变化与长期干旱及季风增强存在关联。
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Climate models now integrate ocean-atmosphere coupling to improve decade-scale predictions.当前气候模型已整合海洋-大气耦合机制,以提升十年尺度预测精度。