Smoke particles can act as condensation nuclei, providing surfaces for water vapor to condense and form cloud droplets. This process enhances cloud formation by increasing the number of cloud droplets in the atmosphere. Additionally, smoke particles can also affect the properties of clouds, such as their reflectivity and longevity, through interactions with sunlight and other atmospheric processes.
The presence of smoke can significantly contribute to cloud formation by providing additional particulate matter, known as aerosols, that serve as cloud condensation nuclei (CCN). These particles facilitate the condensation of water vapor, allowing droplets to form around them more easily. As more droplets accumulate, they can lead to the development of clouds. Additionally, smoke can influence local humidity and temperature, further enhancing cloud formation processes.
It depends which form of cloud you're using.'a cloud of smoke' (noun): billow, blanket'the sky is cloudy' (verb): overcast, darken'cloud your judgement' (verb): obscure, muddy
"Mist" is a word that blends with both "smoke" and "fog." Mist is a weather phenomenon that resembles fog, which is a cloud that forms at ground level, and it can often be associated with smoke in certain environments.
A condensation nucleus is something that is found in a cloud droplet. Condensation nuclei are tiny solid particles such as dust, smoke, or even bacteria onto which water condenses, allowing clouds to form.
Cloud ceiling refers to the height above the ground at which a ceiling layer of clouds or obscuring phenomena (such as fog or smoke) exist. It is an important meteorological parameter used in aviation to determine visibility and flight conditions.
The presence of smoke can significantly contribute to cloud formation by providing additional particulate matter, known as aerosols, that serve as cloud condensation nuclei (CCN). These particles facilitate the condensation of water vapor, allowing droplets to form around them more easily. As more droplets accumulate, they can lead to the development of clouds. Additionally, smoke can influence local humidity and temperature, further enhancing cloud formation processes.
very thick smoke
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The cloud-like gases from something burning are likely smoke. When a material burns, it releases particles and gases into the air, creating a visible cloud of smoke. It is important to ensure proper ventilation and fire safety measures when dealing with smoke from a fire.
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The Landsat Thematic Mapper band that best shows cloud smoke and haze is Band 1 (Blue band). This band is sensitive to atmospheric particles and can effectively highlight the presence of aerosols and smoke. Additionally, Band 2 (Green band) can also assist in identifying haze, but Band 1 is typically more effective for detecting these atmospheric conditions.
Collective nouns for 'smoke' are:a wisp of smokea puff of smokea column of smokea cloud of smoke
It is not smoke. It is condensing water vapor forming a miniature cloud.
a cloud of smoke
Two conditions required for cloud formation are cooling air to reach its dew point temperature and the presence of particles, such as dust, smoke, or salt, for water vapor to condense upon and form droplets.
Smoke can act as cloud condensation nuclei in the atmosphere, providing surfaces for water vapor to condense and form cloud droplets. These cloud droplets can then grow and eventually fall as rain. However, excessive smoke can also have negative impacts on the environment and human health.
When smoke touches cold water in a test tube, it cools down rapidly, causing the smoke particles and gases to condense and form a visible cloud. This cloud is the result of the water vapor in the smoke condensing into tiny water droplets, making the smoke more visible.