However, convective cloud sometimes forms inland, reducing the number of hours of sunshine.

Tropical convective clouds play an important part in the Earth's climate system.

Since the tops of tropical systems are much cooler than the surface of the Earth, the presence of high convective clouds cools the climate system.

Further analysis gives the actual base and top height of convective clouds or possible instabilities in the stratification.

Convective precipitation falls over a certain area for a relatively short time, as convective clouds have limited horizontal extent.

The dense atmosphere frequently produces bright white convective clouds, especially over the south pole region.

In addition to the eye, convective clouds had also formed, creating the eyewall of a tropical cyclone.

Special attention is paid to low clouds and convective cloud particularly cumulonimbus incus clouds.

During the daytime, if heating and/or convergence are sufficient, the cap can be broken, resulting in convective clouds.

The associated convective cloud, can extend up to a height of 15 km above the ground.