科学通识与工程精读·英语30篇（1）
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Why Coastal Fog Forms Despite Warm Sea Surface Temperatures
为何暖海面温度下仍形成海岸雾
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Coastal fog commonly develops when moist marine air moves over cooler land or upwelled ocean water—even if the broader sea surface remains warm.沿海雾通常在潮湿的海风流经较冷的陆地或上涌的冷水时形成，即使大范围海表温度仍较高。
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The key driver is not absolute temperature but vertical temperature gradient: advection fog forms when unsaturated air cools below its dew point upon contact with colder surfaces.关键驱动因素并非绝对温度，而是垂直温度梯度：平流雾产生于未饱和空气接触冷表面后冷却至露点以下。
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Along California’s coast, equatorial warm currents coexist with cold subsurface upwelling, creating sharp horizontal thermal contrasts ideal for fog banks.加州海岸既有赤道暖流，又有冷的次表层上升流，形成利于雾带生成的强烈水平热对比。
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Satellite imagery reveals fog corridors aligning precisely with coastal bathymetric ridges that drive localized upwelling—not broad SST anomalies.卫星图像显示，雾带精确沿驱动局地上升流的沿海地形脊线分布，而非由大范围海表温度异常所致。
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Maritime pilots rely on real-time fog forecasts calibrated to near-surface lapse rates, not satellite-derived sea surface averages.海上领航员依赖基于近地层气温直减率校准的实时雾预报，而非卫星反演的海表平均温度。
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Urban heat islands paradoxically intensify fog persistence inland by delaying nocturnal boundary layer mixing that would otherwise disperse it.城市热岛效应反而延缓夜间边界层混合，从而加剧内陆雾的持续时间。
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Climate models show increasing fog frequency in some subtropical coasts despite rising mean SSTs—highlighting the inadequacy of single-variable climate indicators.气候模型显示，部分副热带海岸雾频次增加，尽管平均海表温度上升——凸显单变量气候指标的局限性。
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Aviation authorities treat fog formation as a microscale thermodynamic event, requiring airport-specific dew-point depression thresholds for landing clearance.航空管理部门将雾的形成视为微尺度热力学事件，要求机场按特定露点差阈值批准着陆。
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Fog chemistry differs significantly from continental mist: higher chloride aerosol content accelerates corrosion on offshore infrastructure.沿海雾的化学成分与大陆雾显著不同：更高浓度的氯化物气溶胶加速近海基础设施腐蚀。
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Coastal architects now incorporate fog-resilient material specifications into building codes, referencing ASTM D6329 corrosion testing protocols.沿海建筑师已将抗雾材料技术要求纳入建筑规范，并援引ASTM D6329腐蚀测试标准。
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This phenomenon illustrates how macroclimate trends obscure critical mesoscale processes governing human-scale environmental exposure.这一现象表明，大尺度气候趋势会掩盖调控人类尺度环境暴露的关键中尺度过程。
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Understanding it demands integrating oceanography, boundary-layer meteorology, and materials science—not just atmospheric temperature alone.理解该现象需融合海洋学、边界层气象学和材料科学，而不仅限于大气温度。