dew point
dew point temperature, causing the water vapor in the air to condense into water droplets or ice crystals. These condensed water droplets or ice crystals then come together to form cumulus clouds.
First, warm air, heated by the surface, rises. As it rises, the temperature drops, which increases the relative humidity. Once the relative humidity passes 100%, water vapor in the air begins to condense. The formation of a cumulus cloud occurs when the water vapor condenses on various nuclei in the air. This creates the puffy cotton-like look of cumulus clouds.
The formation of sun is the most important part of solar system formation. Sun is the reason for formation of rocky planets.
condensation
Star formation starts in a nebula.
The process of tornado formation generally begins in a rotating mass of air within a mesocyclone, a rotating mass of air in a type of thunderstorm called a supercell. A downdraft wraps around the mesocyclone, causing it to tighten and intensify, while at the same time stretching to extend downward. This process usually begins two or three miles above ground level. If the intense vortex reaches the ground, it is considered a tornado.
Condensation begins
The process of air reaching its dew point is called condensation. As the air pressure reaches the dew point, the humidity increases.
First, warm air, heated by the surface, rises. As it rises, the temperature drops, which increases the relative humidity. Once the relative humidity passes 100%, water vapor in the air begins to condense. The formation of a cumulus cloud occurs when the water vapor condenses on various nuclei in the air. This creates the puffy cotton-like look of cumulus clouds.
condensation level
Dew Point
Dew Point
condense into tiny water droplets. This process is known as condensation and is responsible for the formation of clouds and other forms of precipitation.
dew point
It is called the dewpoint.
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The birth stage in a thunderstorm is called the cumulus stage. During this stage, warm air rises and begins to form cumulus clouds due to the updrafts. The air then cools and condenses, leading to the development of the storm clouds.
The first stage is the cumulus cloud stage in which the fluffy cumulus cloud in an unstable (warm and moist near surface and very cold aloft) builds into a towing cumulus. All we have is an updraft! In the next stage, the mature stage rain begins to fall dragging down cool air and evaporating into the downdraft and cooling it. Then we have an updraft and a downdraft together. When the mature thunderstorm reaches way up in the atmospehere to the tropopause (boundary between the layer of the atmospehere where sensible weather occurs and the stratosphere) an anvil shape becomes evident. The final stage is the dissipating stage. The rain and rain cooled air become so dominant that the updraft dies and all that is left is the downdraft. The thunderstorm dies without an updraft.