Increase in humidity, and decrease in temperature.
White fluffy clouds, known as cumulus clouds, do not bring rain on their own. Rain typically falls from higher-level clouds such as nimbostratus or cumulonimbus clouds, which have more moisture and larger vertical development. Cumulus clouds may eventually develop into rain-producing clouds if they continue to grow and merge with other clouds.
Cumulus clouds can develop into cumulonimbus clouds, which are usually thunderstorms. All thunderstorms contain an updraft, which is a rising air current. Under the right conditions this updraft can start rotating, becoming a mesocyclone. The thunderstorm is now called a supercell. Sometimes the bottom of the mesocyclone can tighten and intensify to produce a tornado.
They don't. It is the other way around. Cold fronts commonly cause cumulonimbus. Such clouds form when the atmosphere is unstable, meaning that a parcel of air, when given an upward nudge, will continue to rise on its own. A cold front provides that upward nudge to trigger cumulonimbus development.
Cumulus clouds are fluffy, white clouds with a rounded shape and flat base. They usually signal fair weather, but can also develop into larger storm clouds if conditions are right. Cumulus clouds are formed by the vertical convection of warm air rising and cooling in the atmosphere.
Cumulonimbus clouds appear dark because they are very thick and tall, blocking most of the sunlight from passing through. The more dense the cloud, the less light gets through, making the bottom look dark or gray.
They don't. However, a cumulus cloud can develop into a cumulonimbus cloud (a.k.a. thunderstorm) under the right conditions. Even then conditions have to be specific for it to produce a tornado.
Cumulus clouds cause fair weather, but cumulonimbus on the other hand don't, they cause thunderstorms and severe weather. Cumulus clouds can occur on fair weather days because of areas of rising and sinking air from the surface. This is typical of a conditionally stable atmosphere. Cumulonimbus clouds are the result of frontal lifting, allowing air rising to tap into atmospheric energy and therefore allowing the air to rise on its own without further frontal lifting required.
Cumulus clouds are puffy, billowing clouds rather than stratified, and can exist as well-defined within a mass of otherwise clear air. Rapid heating can cause towering cumulus clouds or may create the related forms known as cumulonimbus (thunderstorm) clouds.
There are two main rain/snow making clouds. Nimbostratus, a thick uniformly grey cloud at low heights will cause light to moderate rain or snow to fall over long periods of time. Cumulonimbus, a massive white towering cloud sometimes with the shape of an anvil, with a very dark appearance from below. These clouds will make very heavy rain/snow fall over a short time, often with the presence of lightning. These are the clouds that will make rain and snow
No. First of all, cirrus are high-altitude whispy clouds. Low-altitude puffy clouds are called cumulus. Cumulus clouds can occasionally produce a few drops of rain, but usually indicate fair weather. Precipitation is more often associated with stratus and cumulonimbus clouds.
Cumulus clouds are puffy, billowing clouds rather than stratified, and can exist as well-defined within a mass of otherwise clear air. Rapid heating can cause towering cumulus clouds or may create the related forms known as cumulonimbus (thunderstorm) clouds.
White fluffy clouds, known as cumulus clouds, do not bring rain on their own. Rain typically falls from higher-level clouds such as nimbostratus or cumulonimbus clouds, which have more moisture and larger vertical development. Cumulus clouds may eventually develop into rain-producing clouds if they continue to grow and merge with other clouds.
what are the six that cause a change in supply
Weathering and erosion cause exposed land to change.
cumulonimbus
A cumulonimbus cloud
Cumulonimbus