File:Снежная ива.jpg
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Русский: Ледяной туман, или морозный туман — туман, состоящий из кристалликов льда и наблюдаемый при температуре воздуха ниже -10...-15°С и высокой влажности. Представляет собой помутнение воздуха, при котором горизонтальная видимость падает до одного и меньше километров. Ледяной туман вызван наличием в воздухе большого количества ледяных игл, мельчайших (диаметром 10—20 мкм) капелек, а также ледяных кристаллов (диаметром от 10 до 100 мкм), иногда смешанных с переохлаждёнными капельками. Наибольшей интенсивности ледяной туман достигает при температуре воздуха ниже -30°С.
English: Ice fog, or freezing fog — fog composed of ice crystals and observed at air temperatures below -10 to -15°C and high humidity. Is a clouding of the air, where horizontal visibility falls to one and less miles. Ice fog caused by the presence in the air a large number of ice needles, the smallest (diameter 10-20 µm) droplets and ice crystals (with diameters from 10 to 100 µm), sometimes mixed with supercooled droplets. The highest intensity of ice fog up when the air temperature is below -30°C. |
| Date | |
| Source | Own work |
| Author | Schimanscky Ivan |
| Camera location |  | View this and other nearby images on: OpenStreetMap |  |
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I, the copyright holder of this work, hereby publish it under the following license:
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This image was uploaded as part of Wiki Science Competition 2017. |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 15:41, 21 November 2017 | | 3,428 × 2,295 (7.05 MB) | Schimanscky.v (talk | contribs) | User created page with UploadWizard |
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