A visible mass of condensed water vapor floating in the atmosphere, typically high above the ground.There are five main ways water vapor can be added to the air. Increased vapor content can result from wind convergence over water or moist ground into areas of upward motion. Precipitation or virga falling from above also enhances moisture content. Daytime heating causes water to evaporate from the surface of oceans, water bodies or wet land. Transpiration from plants is another typical source of water vapor. Lastly, cool or dry air moving over warmer water will become more humid. As with daytime heating, the addition of moisture to the air increases it's heat content and instability and helps set into motion those processes that lead to the formation of cloud or fog.
rain cloud fluffy cloud dark cloud wispy cloud
It's called in-cloud or cloud-to-cloud lightning.
there is no mediem cloud in the sky!
Inter-cloud lightning!
It's called in-cloud or cloud-to-cloud lightning.
Because it the humidity is in the cloud it makes the cloud warm so the cloud rises. So then the cloud is higher up.
a cloud
It's called in-cloud or cloud-to-cloud lightning.
An accessory cloud is a small cloud formation which is found attached to or close by a major cloud in one of the main cloud genera, responsible for its formation.
It's called in-cloud or cloud-to-cloud lightning.
Depending on context, cloud can be translated as:NounWolke (cloud in the sky)in Misskredit (as in: to be under a cloud)Schutz (as in: under the cloud of night)Verbsich bewölkentrübenvernebelnverdüsternverschleiernverdunkeln
Cloud's full name is Cloud Strife.