The ground is heated up differently due to receiving different amount of insolation and air over warmer parts will rise first.
Rising air expand with low pressure at high altitude. Air mass cool and relative humidity increase and saturation humidity decreases. Air force upwards, surrounding air is not as warm as rising air.
When air reach dew point, water vapour starts to condense on atmospheric particles which acts as a condensation nuclei. Relative humidity reaches 100% saturation.
Cloud formation continues as high as air rises. When air stop rising, cloud development stops. More uplift means the clouds will be taller and deeper.
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When a cloud forms, it is called condensation. This process occurs when water vapor in the air cools and turns into liquid droplets, which then gather to create a visible cloud.
what happens to a nimbostratus cloud
When water in the air condenses onto tiny particles, it forms droplets. This process is called condensation and is the basis for cloud formation. The water droplets eventually become large enough to fall as precipitation, such as rain or snow.
Condensation.
This type of cloud would be known as a stratus cloud
When a tornado forms, violent rotating winds reach ground level, often kicking up a cloud of dust in the process.
It forms a cloud
It forms a cloud
It forms a funnel cloud.
It forms a cloud
It forms a cloud then it rains
When a cloud holding water vapor suddenly cools, the water vapor condenses into liquid water droplets or ice crystals. This process forms precipitation, such as rain or snow, which falls to the ground.
When a cloud forms, it is called condensation. This process occurs when water vapor in the air cools and turns into liquid droplets, which then gather to create a visible cloud.
what happens to a nimbostratus cloud
When water in the air condenses onto tiny particles, it forms droplets. This process is called condensation and is the basis for cloud formation. The water droplets eventually become large enough to fall as precipitation, such as rain or snow.
Condensation.
Lightning happens when the negative charges (electrons) in the bottom of the cloud are attracted to the positive charges (protons) in the ground.