Many clouds are flat on the bottom because as the air rises from the surface it cools, and at the saturation temperature it starts to condense, which is where the clouds start. Since the whole column is starting at the same conditions and going through the same process, it all condenses at the same height.
Clouds are formed when the temperature of the atmosphere reaches the condensation point (this is when it turns to water vapor). When this happens, the water vapor sticks to dust particles in the air and becomes visible. The temperature of the atmosphere usually changes(gets colder) as you go up, so only at a certain point can the water vapor droplets form. When you see the flat bottoms of clouds, you see where this point begins - this is the beginning of the proper temperature for water vapor to form.
clouds.
Flat bottom clouds are called stratocumulus clouds. They are low-lying clouds that appear as a layer or patch with a flat, broad base. Stratocumulus clouds often indicate stable weather conditions.
These are cumulus clouds.
a cloud that forms a layer with other flat,clouds is a
Those would be cumulus clouds, which are characterized by their fluffy, cotton-like appearance and their flat base. Cumulus clouds often form on fair weather days but can develop into larger storm clouds if conditions are right.
A cumulus cloud typically has a flat bottom and a puffy top. These clouds form due to rising air currents and are often associated with fair weather.
Yes, Cumulus clouds have flat bottoms.
A cumulus cloud is a puffy cloud that appears to rise up from a flat bottom that are associated with fine weather.
cumulonimbus clouds. They are puffy that appear to rise up from a flat bottom.
Clouds in flat layers are called stratus.
Clouds appear flat on the bottom because that is the boundary between the moist rising air creating the cloud and the drier surrounding air. The fluffy appearance at the top is due to the cloud particles spreading out as the cloud reaches higher altitudes where temperatures are colder, causing the water vapor to condense into smaller droplets.
The description matches a cumulus cloud. These clouds are formed by rising air currents and are typically associated with fair weather. Cumulus clouds have a fluffy appearance with a flat base and rounded top.