You might already know how it feels to touch a cloud without realizing it.<\/p>\n\n\n\n
If you\u2019ve ever been outside on a foggy day, you\u2019ve essentially been inside a cloud, just one very close to the ground instead of high in the sky. Fog and clouds are both made of tiny water droplets \u2013 like the ones you can sometimes see or feel in a hot, steamy shower.<\/p>\n\n\n\n
Clouds form through evaporation and condensation. Water in lakes, rivers, oceans or puddles evaporates into water vapor as the sun heats it up.\u00a0You can evaporate water yourself\u00a0by boiling it \u2013 watch it disappear as vapor.<\/p>\n\n\n\n
Water vapor, which is invisible, naturally rises up from the Earth\u2019s surface into the atmosphere as warm bubbles, like the bubbles you\u2019d see rising in a lava lamp. The higher it goes, the more it cools, until eventually the water vapor condenses back into liquid water.<\/p>\n\n\n\n
Clouds are made of millions of these tiny liquid water droplets. The droplets scatter the colors of the sunlight equally, which makes\u00a0clouds appear white. Even though they can look like cushy puffballs, a cloud can\u2019t support your weight or hold anything up but itself.<\/p>\n\n\n\n
The process of evaporation and condensation in the atmosphere is similar to what happens in your bathroom when you take a hot shower: Warm water evaporates and then condenses back into water on the cold mirror.<\/p>\n\n\n\n
Water vapor does not condense spontaneously. It needs tiny particles or a surface \u2013 like your bathroom mirror \u2013 on which to form a drop.\u00a0Atmospheric scientists like me\u00a0call these tiny particles cloud condensation nuclei, or CCN for short. These CCN are just dirt or dust particles that have been lifted by the wind and are\u00a0floating around in the atmosphere.<\/p>\n\n\n\n
Does that mean that places with a lot of dust and pollution, like cities, have more drops than clean places? Researchers have found more tiny droplets and more clouds in areas where there are a lot of these cloud condensation nuclei, while in areas without them fewer clouds are observed,\u00a0like over the ocean or the Arctic.<\/p>\n\n\n\n
As cloud droplets rise in the atmosphere, the air temperature decreases. The tiny cloud droplets start to freeze when the temperature drops below below 32 degrees Fahrenheit (0 degrees Celsius). It\u2019s the exact same process as making ice cubes in a freezer.<\/p>\n\n\n\n
The frozen droplets are now ice crystals. They continue to grow in size as water vapor turns into ice and sticks onto them. Scientists call this process of a gas turning into a solid \u201cdeposition.\u201d It creates the beautiful branched ice crystals that you find in snowstorms.<\/p>\n\n\n\n
Steady updrafts of air keep these very light water droplets or ice crystals floating in the cloud. So how do they turn into rain and snow and fall to the ground? Easy, they join forces.<\/p>\n\n\n\n
Larger droplets collect smaller droplets on their way to the ground as raindrops. Snow grows in a similar way, with the crystals sticking to each other. Their little arms can interlock to form a bigger snowflake. When water droplets merge with ice crystals, that makes hail.<\/p>\n\n\n\n
Rain droplets grow on their way down to the ground, eventually becoming unstable and breaking up.\u00a0The largest raindrop\u00a0that researchers have found was about a third of an inch across. Some\u00a0giant snowflakes\u00a0have been reported to be as big as 6 inches across. And the biggest piece of hail? In 2010, someone found\u00a0a hailstone 8 inches in diameter\u00a0in South Dakota and took a photo \u2013 so scientists know it was real.<\/p>\n\n\n\n
That would be a lot more painful to collide with than a wispy cloud of water vapor.<\/p>\n\n\n\n
The need for digital IT is needed in daily activities, Bead IT Consultant is the right choice as your partner, visit our website by clicking this link: www.beadgroup.com.<\/p>\n\r\n