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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 ]
Marine stratocumulus is a type of stratocumulus cloud that form in the stable air off the west coast of major land masses. The Earth spins on its axis, which results in the Coriolis force pushing the ocean surface water away from the coast in the mid-latitudes.
DISPLAY-2 (Greece) – A vapour cloud dispersion model for neutral or denser-than-air pollution plumes over irregular, obstructed terrain on a local scale. It accommodates jet releases as well as two-phase (i.e., liquid-vapor mixtures) releases. This model was also developed at the National Centre of Scientific Research "DEMOKRITOS" of Greece.
Flavoring are often added to e-liquids as well as dry smoke blends. There are currently over 7,700 e-liquid flavors available, most have not been laboratory tested for toxicity. [88] There are numerous flavors (e.g., fruit, vanilla, caramel, coffee [5]) of e-liquid available. [7] There are also flavorings that resemble the taste of cigarettes. [7]
The air in the marine layer becomes very moist and very low clouds or fog occurs. [19] [20] If wind gradients turn on-shore with enough strength, this sea fog is blown onto the coastal areas. This marks a sudden and surprising transition from the hot, dry Santa Ana conditions to cool, moist, and gray marine weather, as the Santa Ana fog can ...
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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.
Water vapor normally begins to condense on condensation nuclei such as dust, ice, and salt in order to form clouds. [14] [15] Fog, like its elevated cousin stratus, is a stable cloud deck which tends to form when a cool, stable air mass is trapped underneath a warm air mass. [16] Fog normally occurs at a relative humidity near 100%. [17]