Condensation happens at the base of Cumulus clouds.
1) Cumulus clouds are vertically developed clouds. 2) Cumulus clouds have a flat base, which is the location of the lifting condensation level. 3) Cumulus clouds can develop into cumulonimbus clouds. 4) Cumulus clouds have a lifetime of less than an hour.
They could be seagulls, or snowflakes, or clouds.
It depends on what cumulus type you are talking about. Cumulus humilis clouds are 'fatter' than they are tall. This is what people would usually refer to if they say just 'cumulus'. These are the clouds you see in the morning, and all also called fair weather clouds. You normally see a cumulus humilis cloud at an altitude of 2,000 to 3,500 feet. (600-1,050 m) Cumulus mediocris clouds are an alternate version of the humilis version. These clouds are taller than they are fat. You normally see a cumulus humilis cloud at an altitude of 2,000 to 4,000 feet. (600-1,200 m) Cumulus congestus clouds are the only cumulus clouds that produce substantial precipitation. When you hear someone saying '"cumulus clouds can produce precipitation"', they refer to these clouds. You normally see a cumulus congestus cloud at an altitude of 2,000 to 20,000 feet. (600-6,000 m). If you want to know what my reference is, it is a book called "Weather", by William J. Burroughs, Bob Crowder, Ted Robertson, Eleanor Vallier-Talbot, and Richard Whitaker.
they are mid altitude clouds, forms when warm air rises, they are also puffy, white clouds that tend to have flat bottoms, and they indicate fair weather
Clouds are divided into two general categories: layered and convective. These are named stratus clouds (or stratiform, the Latin stratus means "layer") and cumulus clouds (or cumuliform; cumulus means "piled up"), respectively. These two cloud types are divided into four more groups that distinguish the cloud's altitude. Clouds are classified by the cloud base height, not the cloud top. This system was proposed by Luke Howard in 1802 in a presentation to the Askesian Society. High clouds (Family A) * Cirrocumulus * Cirrus cloud * Cirrostratus Middle clouds (Family B) * Altostratus * Altocumulus Low clouds (Family C) These are found up to 2,000 m (6,500 feet) and include the stratus (dense and grey). When stratus clouds contact the ground, they are called fog. Clouds in Family C include: * Cumulus (Cu) * Cumulus humilis ** Cumulus mediocris * Stratocumulus (Sc) * Nimbostratus (Ns) * Stratus (St) Vertical clouds (Family D) These clouds can have strong up-currents, rise far above their bases and form at many heights. Clouds in Family D include: * Cumulonimbus (associated with heavy precipitation and thunderstorms) (Cb) * Cumulonimbus calvus ** Cumulonimbus incus ** Cumulonimbus with mammatus * Cumulus (Cu) * Cumulus congestus * Pyrocumulus Other clouds A few clouds can be found above the troposphere; these include noctilucent and polar stratospheric clouds (or nacreous clouds), which occur in the mesosphere and stratosphere respectively. Some clouds form as a consequence of interactions with specific geographical features. Perhaps the strangest geographically-specific cloud in the world is Morning Glory, a rolling cylindrical cloud which appears unpredictably over the Gulf of Carpentaria in Northern Australia. Associated with a powerful "ripple" in the atmosphere, the cloud may be "surfed" in glider aircraft.
1) Cumulus clouds are vertically developed clouds. 2) Cumulus clouds have a flat base, which is the location of the lifting condensation level. 3) Cumulus clouds can develop into cumulonimbus clouds. 4) Cumulus clouds have a lifetime of less than an hour.
They could be seagulls, or snowflakes, or clouds.
Cumulus Clouds do.
Cumulus clouds are the extremely puffy clouds in the sky. The base of the cloud is usually flat and is topped by billowing towers of puffy white clouds resembling cauliflower heads.
Cumulus clouds, the base of each cloud is often flat and may only be 1000 meters above the ground. Tops may extend to 12,000 meters high
It depends on what cumulus type you are talking about. Cumulus humilis clouds are 'fatter' than they are tall. This is what people would usually refer to if they say just 'cumulus'. These are the clouds you see in the morning, and all also called fair weather clouds. You normally see a cumulus humilis cloud at an altitude of 2,000 to 3,500 feet. (600-1,050 m) Cumulus mediocris clouds are an alternate version of the humilis version. These clouds are taller than they are fat. You normally see a cumulus humilis cloud at an altitude of 2,000 to 4,000 feet. (600-1,200 m) Cumulus congestus clouds are the only cumulus clouds that produce substantial precipitation. When you hear someone saying '"cumulus clouds can produce precipitation"', they refer to these clouds. You normally see a cumulus congestus cloud at an altitude of 2,000 to 20,000 feet. (600-6,000 m). If you want to know what my reference is, it is a book called "Weather", by William J. Burroughs, Bob Crowder, Ted Robertson, Eleanor Vallier-Talbot, and Richard Whitaker.
I do believe they are called cumulus clouds, as they appear to be very fluffy and have a cotton sort of look, but they have a flat-looking base that is darker than the rest of the cloud.
6,000 feet MSL.
they are mid altitude clouds, forms when warm air rises, they are also puffy, white clouds that tend to have flat bottoms, and they indicate fair weather
Clouds are divided into two general categories: layered and convective. These are named stratus clouds (or stratiform, the Latin stratus means "layer") and cumulus clouds (or cumuliform; cumulus means "piled up"), respectively. These two cloud types are divided into four more groups that distinguish the cloud's altitude. Clouds are classified by the cloud base height, not the cloud top. This system was proposed by Luke Howard in 1802 in a presentation to the Askesian Society. High clouds (Family A) * Cirrocumulus * Cirrus cloud * Cirrostratus Middle clouds (Family B) * Altostratus * Altocumulus Low clouds (Family C) These are found up to 2,000 m (6,500 feet) and include the stratus (dense and grey). When stratus clouds contact the ground, they are called fog. Clouds in Family C include: * Cumulus (Cu) * Cumulus humilis ** Cumulus mediocris * Stratocumulus (Sc) * Nimbostratus (Ns) * Stratus (St) Vertical clouds (Family D) These clouds can have strong up-currents, rise far above their bases and form at many heights. Clouds in Family D include: * Cumulonimbus (associated with heavy precipitation and thunderstorms) (Cb) * Cumulonimbus calvus ** Cumulonimbus incus ** Cumulonimbus with mammatus * Cumulus (Cu) * Cumulus congestus * Pyrocumulus Other clouds A few clouds can be found above the troposphere; these include noctilucent and polar stratospheric clouds (or nacreous clouds), which occur in the mesosphere and stratosphere respectively. Some clouds form as a consequence of interactions with specific geographical features. Perhaps the strangest geographically-specific cloud in the world is Morning Glory, a rolling cylindrical cloud which appears unpredictably over the Gulf of Carpentaria in Northern Australia. Associated with a powerful "ripple" in the atmosphere, the cloud may be "surfed" in glider aircraft.
A cumulus cloud has a flat base and a rounded fluffy appearance. The top looks like a cotton-ball and is irregular.
Cumulus clouds typically indicate fair weather. They are fluffy and white with a flat base and appear during stable atmospheric conditions. However, they can develop into cumulonimbus clouds, which bring thunderstorms and potentially severe weather.