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How Fog Forms When Warm Air Meets Cold Ground
雾为何在暖空气接触冷地面时形成?
精读先不看文字,完整听一遍。
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Fog forms when moist air cools rapidly near the ground overnight.雾在夜间近地面的潮湿空气迅速冷却时形成。
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As temperatures drop, water vapor condenses into tiny liquid droplets suspended in air.随着气温下降,水蒸气凝结成悬浮于空气中的微小液滴。
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This process requires high humidity and a surface that loses heat quickly after sunset.这一过程需要高湿度,以及日落后能快速散热的地表。
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Radiation fog is most common in calm, clear nights with little wind or cloud cover.辐射雾最常出现在无风、晴朗、少云的静稳夜晚。
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Unlike clouds, fog develops at ground level where cooling is strongest and most direct.与云不同,雾在地表形成,因为此处冷却最强烈、最直接。
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Dew point temperature must be reached for condensation to begin visibly.只有当气温降至露点,才能开始肉眼可见的凝结。
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Urban areas often see less radiation fog due to heat retention from buildings and roads.城市地区因建筑和道路蓄热,辐射雾往往较少。
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Farmers monitor fog forecasts carefully because it can delay morning fieldwork safely.农民密切关注雾的预报,因为它可能安全延后清晨田间作业。
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Fog usually lifts by mid-morning as sunlight warms the surface and evaporates droplets.日出后地表受热,雾滴蒸发,通常到上午中段消散。
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Its density depends on moisture content, cooling rate, and atmospheric stability.雾的浓密程度取决于水汽含量、冷却速率和大气稳定性。
精读 · 大约 10 分钟
听 → 读 → 学表达 → 懂 → 今天会说这一句 → 跟读录音 → 自己说一句。
③ 学 · 重点表达
- Fog forms when moist air cools rapidly near the ground overnight. 雾在夜间近地面的潮湿空气迅速冷却时形成。
- Dew point temperature must be reached for condensation to begin visibly. 只有当气温降至露点,才能开始肉眼可见的凝结。
- Its density depends on moisture content, cooling rate, and atmospheric stability. 雾的浓密程度取决于水汽含量、冷却速率和大气稳定性。
④ 懂 · 选一选
⑤ 今天会说这一句
Fog forms when moist air cools rapidly near the ground overnight.
⑥ 跟读并录音
Fog forms when moist air cools rapidly near the ground overnight.
第一版:录下来、回听、再听标准音。系统打分以后再加。
⑦ 说 · 自己来一句
用今天的表达,自己说一句。
例子:Fog forms when moist air cools rapidly near the ground overnight.
已记下。连续天数以后会显示在课表里。
陈老师指导
课程开发中,敬请期待。成人和孩子都可以先自学听读、精读。
这边的讲解音轨还在做。想先跟着老师走完固定 30 课,可以去陈老师带读社(和自学通行不是同一份会员)。
课程开发中,敬请期待。