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Clouds form when invisible water vapor condenses into microscopic water droplets or into microscopic ice crystals. This may happen when air with a high proportion of gaseous water cools. A distrail forms when the heat of engine exhaust evaporates the liquid water droplets in a cloud, turning them back into invisible, gaseous water vapor.
Sea of fog riding the coastal marine layer through the Golden Gate Bridge at San Francisco, California Afternoon smog within a coastal marine layer in West Los Angeles. A marine layer is an air mass that develops over the surface of a large body of water, such as an ocean or large lake, in the presence of a temperature inversion.
Also actiniform. Describing a collection of low-lying, radially structured clouds with distinct shapes (resembling leaves or wheels in satellite imagery), and typically organized in extensive mesoscale fields over marine environments. They are closely related to and sometimes considered a variant of stratocumulus clouds. actinometer A scientific instrument used to measure the heating power of ...
Cloud-chasing [note 1] is the activity of blowing large clouds of vapor using an electronic cigarette. [8] Using the devices for "cloud-chasing" began in the West Coast of the US . [ 8 ] The exact origins of the activity are unclear, [ 9 ] but most competitive e-cigarette users say that it started around 2012. [ 10 ]
What different clouds mean. Clouds are more than just picturesque features of the sky; they are critical indicators of the weather to come. Understanding the various types of clouds can provide ...
Cloud formation is a complex process that begins with the condensation of water vapor in the atmosphere. This process typically occurs when moist air rises and cools to its dew point, leading to the formation of water droplets or ice crystals. [ 5 ]
Connection between sea foam and sea spray formation. The dark orange line indicates processes common to the formation of both sea spray and sea foam. When wind, whitecaps, and breaking waves mix air into the sea surface, the air regroups to form bubbles, floats to the surface, and bursts at the air-sea interface. [10]
The island generates wave motion in the wind passing over it, creating regularly spaced orographic clouds. The wave crests raise and cool the air to form clouds, while the troughs remain too low for cloud formation. Note that while the wave motion is generated by orographic lift, it is not required. In other words, one cloud often forms at the ...