The droplets of water outside the glass likely came from condensation. When warm air comes into contact with a colder surface, such as the glass, the air cools down and can no longer hold as much moisture. This excess moisture then forms droplets on the cooler surface, which is the condensation you see on the outside of the glass.
It is Sleet. Hail is when water droplets condense out of the cloud and are carried upwards in a draught to a colder refion, whereupon the water droplets freeze into ice. and fall to Earth as hail.
yes, it condenses. thats why it rains. clouds become too heavy and water droplets (rain) fall. if the air is cold as it falls it can become snow or hail.
Simple answer: They don't. Clouds ARE water - tiny, tiny droplets of water just like fog. If colder air moves into a cloud, it causes there to be even more water droplets forming. When the droplets get close enough together, they start touching and turning themselves into even larger droplets. Then the "even larger" water droplets touch, and make water drops . . . at some point in this process, the water droplets grow large enough that they are too heavy to stay where they are, and then they fall to the ground. This falling to the ground is what we call, "Rain".
Hail falls from the sky when supercooled water droplets in a thunderstorm freeze into ice pellets due to updrafts carrying them to colder altitudes. These ice pellets grow as they collide with other droplets and fall to the ground when they become too heavy for the updraft to support.
The correct term is condensation. This occurs when rising water vapor meets colder air, causing it to lose heat and change back into liquid water in the form of water droplets.
They are made of bolth because they are vertically developed. The bottom is made of water, and as they develop higher, become ice.
When you get out of shower, there are water droplets on your body. Some of the body's heat is loss to them before they evaporate. So we felt colder. YP
That is the correct spelling of "chillier" (more chilly).
Water vapor needs to cool down in order to turn into droplets. This cooling process can happen by either coming into contact with a colder surface or by the surrounding air temperature dropping. Once the water vapor cools sufficiently, it will condense into droplets.
The droplets of water outside the glass likely came from condensation. When warm air comes into contact with a colder surface, such as the glass, the air cools down and can no longer hold as much moisture. This excess moisture then forms droplets on the cooler surface, which is the condensation you see on the outside of the glass.
It is Sleet. Hail is when water droplets condense out of the cloud and are carried upwards in a draught to a colder refion, whereupon the water droplets freeze into ice. and fall to Earth as hail.
yes, it condenses. thats why it rains. clouds become too heavy and water droplets (rain) fall. if the air is cold as it falls it can become snow or hail.
Dew is formed by condensation - the water from the air around the ground becomes heavy enough to form into droplets on any areas which are colder than the air.Rain is formed when water droplets condense above the ground and fall.
Condensation/Hot Moist Air Meeting Colder Air
Simple answer: They don't. Clouds ARE water - tiny, tiny droplets of water just like fog. If colder air moves into a cloud, it causes there to be even more water droplets forming. When the droplets get close enough together, they start touching and turning themselves into even larger droplets. Then the "even larger" water droplets touch, and make water drops . . . at some point in this process, the water droplets grow large enough that they are too heavy to stay where they are, and then they fall to the ground. This falling to the ground is what we call, "Rain".
Frozen rain droplets can form in thunderstorms when raindrops get carried into colder upper atmosphere regions where they freeze. These frozen droplets, called hail, can grow larger as they are carried by updrafts within the storm, eventually falling to the ground when they become too heavy to be supported by the updraft.