Clouds

The correct spelling is tule fog instead of tulie fog. Tule fog is defined as a thick ground fog in areas of California's Great Central Valley. Tule fog forms in late fall after the first significant rainfall until spring.

Fog is just clouds that came down from the sky during the night..

A cloud may be considered partly fog; for example, the part of a cloud that is suspended in the air above the ground is not considered fog, whereas the part of the cloud that comes in contact with higher ground is considered fog. Fog is distinguished from mist only by its density. Fog reduces visibility to less than 1 km, whereas mist reduces visibility to no less than 1 km but less than 2 km.

Meghalaya in India is known as the 'Abode of Clouds' due to its heavy rainfall and misty landscapes, creating a picturesque and lush environment.

During the formation of clouds, water vapor in the air condenses into liquid water droplets or ice crystals around tiny dust particles or aerosols. This process occurs when the air becomes saturated with moisture, which can happen when warm, moist air rises and cools at higher altitudes. The condensed water droplets/ice crystals then come together to form clouds.

Cloud formation at a front is influenced by the temperature and moisture content of the air masses involved. When warm, moist air rises and cools at a front, it may reach its dew point, causing condensation and cloud formation. Conversely, if the air is too dry or stable, clouds may not form despite the presence of the front.

Fog and clouds in higher altitudes are alike in that they are both composed of tiny water droplets or ice crystals suspended in the air. They both can reduce visibility and may be formed through similar processes, such as cooling of air or condensation of water vapor. Additionally, both fog and high-altitude clouds play a role in the Earth's water cycle and weather systems.

the sun has 5 billion more years to live before it dies. when it does it will no longer provide the earth with light, energy, or warmth. but you do not have to worry, the sun

5,000,000,000

earth

2012

we have loads of time. stop worrying!

Cumulonimbus incus, which has an obvious anvil top. Only very strong ones, called supercells, spawn tornadoes.
Cumulonimbus icnus is the most likely type of storm cloud to produce a tornado. These cumulonimbus clouds are often supercells.
Tornadoes can form from any cumulonimbus cloud, but they usually form from Cumulonimbus incus (heaped rain cloud with anvil) with a rotating updraft called a mesocyclone. The type of storm this rotating cumulonimbus cloud brings is a strong thunderstorm called a supercell, the thunderstorm most likely to form a tornado
cumulonimbus clouds

The thickest fog is the densest fog. It is highly saturated with moisture and highly condensed at cool to cold temperatures. When density lessens and moisture burned off, the cloud bank becomes lighter.

Water vapor condensed to form oceans on Earth's surface early in Earth's history, as the planet cooled down and the atmospheric temperature decreased to a point where the water vapor could no longer remain in its gaseous state.

Luke Howard, a British naturalist who lived in the 19th century, is credited with being among the first to devise a classification system for cloud types. He proposed the classification of clouds into four main types based on their appearance: cumulus, stratus, cirrus, and nimbus, which laid the foundation for modern cloud classification systems.

Cumulus clouds- heaping billows-show fair weather.

stratus clouds-low floating layer-altostratus.

cirrus-curling like a lock of hair-cirrus.

Nimbus-(or cumulonimbus) are rain clouds.

Cumulus clouds can bring rain if they develop into mature cumulonimbus clouds, which are often associated with thunderstorms and heavy precipitation. Cumulus clouds themselves, though, typically indicate fair weather.

High level clouds, such as cirrus clouds, typically do not produce hail or tornadoes. Hail and tornadoes are more commonly associated with severe thunderstorms that develop from cumulonimbus clouds, which are characterized by their towering vertical structure. These types of storms have strong updrafts and downdrafts that are conducive to the formation of hail and tornadoes.

well that's a hard one but i don't think anyone can ever make rain its kinda impossible. rain fall from the sky and the sky is too high up for you guys to reach but you can make your own one by going in an aeroplane and throw water from the sky (LOL)

Cirrus clouds typically form at high altitudes, around 20,000 to 40,000 feet (6,000 to 12,000 meters) above the ground.

Each 1000ft of ascent will bring a cooling of about 3 degrees Centigrade, so at 15000 feet the temperature would have fallen by 45 Centigrade degrees. That seems a lot but that was our basic guide in wartime when we learned to fly. If the cockpit canopy didn't close too well your nose would suffer unless it was inside your flying mask.

Well a nimbus cloud is not a cloud. If you are referring to a cumulonimbus cloud than yes. A cumulonimbus cloud is a storm cloud. Clouds that have names that include -nimbus or nimbo- are likely to produce precipitation.

Altostratus clouds are found in the middle layer of the atmosphere known as the altocumulus layer, typically between 6,500 to 20,000 feet. They are thin, gray clouds that often cover the sky and can sometimes produce light precipitation.

A high-altitude cloud made up of smaller clouds is called a cirrocumulus cloud. These clouds are made up of tiny cloudlets and appear as white patches or ripples in the sky. Cirrocumulus clouds are often associated with fair weather, but they can also indicate the approach of a weather change.

Lenticular clouds generally form in mountainous regions. In these areas, there can be pockets of low pressure in the sky. When air encounters these low-pressure regions, it expands. If the air cools enough, it will condense to form lenticular clouds. The name "lenticular" actually means lens-shaped, because these clouds usually form an oval.

Cloudy with a high chance of precipitation.

Cirrus clouds are thin, wispy clouds found at high altitudes, typically above 20,000 feet. They are composed of ice crystals and are often a sign of fair weather. Cirrus clouds can stretch for long distances across the sky due to high-level winds.

Cumulonimbus clouds are typically associated with intense precipitation, including heavy rain, hail, thunderstorms, and even tornadoes. These clouds can reach high altitudes and are characterized by their towering shape and strong vertical development.

Cirrus clouds are thin and wispy, typically found at high altitudes and composed of ice crystals. Cumulus clouds are fluffy and often flat-based, developing vertically due to rising air currents. Stratus clouds are low-lying, layered clouds that cover the sky like a blanket and can bring prolonged overcast conditions.