What two cloud types produce rain?

The prefix “nimbo-” or the suffix “-nimbus” are low-level clouds that have their bases below 2,000 meters (6,500 feet) above the Earth. Clouds that produce rain and snow fall into this category. (“Nimbus” comes from the Latin word for “rain.”) Two examples are the nimbostratus or cumulonimbus clouds.

Which two types of clouds do not produce rain?

Cumulus and Cumulonimbus do not usually produce rain or snow .

Which cloud is rain bearing?

Nimbus clouds are dark clouds as they carry a substantial quantity of water droplets. Nimbus comes in union with other cloud forms that bring substantial precipitation. Nimbostratus is a dense layer of cloud belonging to the very low altitude, lying beneath 8000 ft. Hence the correct answer is Nimbus cloud.

What are heaps of rain clouds called?

Vertical clouds are the heaped up ones, so their names include the root “cumulus.” The big, towering storm clouds are called cumulonimbus.

What is the rarest cloud type?

Most frequently, mammatus clouds are made up primarily of ice but in some cases they’ve been known to be a mixture of ice and liquid. Noctilucent clouds, also known as polar mesopheric clouds, are one of the rarest cloud formations there is. Their name noctilucent roughly means night shining in Latin.

What are the names of rain clouds?

There are many types of rain clouds, including the three most common types: stratus, cirrus, and cumulus.

Which cloud produces rain?

Thunderstorm clouds form when warm air currents rise above the Earth’s surface creating cumulonimbus clouds. These clouds produce rain, lightning, hail and occasionally tornadoes.

How do clouds produce rain?

If water molecules in a cloud combine into a droplet that is too heavy to be suspended in air, then it falls to the ground as precipitation. A rain cloud occurs when atmospheric conditions cause water molecules to rapidly combine, producing large amounts of precipitation.

Are stratus clouds high or low?

Stratus cloud. Stratus clouds are low-level clouds characterized by horizontal layering with a uniform base, as opposed to convective or cumuliform clouds that are formed by rising thermals.