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Very high electrostatic potential, cloud to earth and cloud to cloud.
A cloud bust is the act of causing a cloud to disperse by focusing on it with your eyes and thus your will.
Not if they stampeded in a swamp!
George E. Hyde has written: 'The Pawnee Indians' -- subject(s): Pawnee Indians 'Red Cloud's folk' -- subject(s): History, Oglala Indians, Red Cloud Indian Agency, United States, United States. Office of Indian Affairs. Red Cloud Agency 'Indians of the woodlands: from prehistoric times to 1725' -- subject(s): Indians of North America, History
The amount of mouisture in a cloud may increase causing it to release precipitation more rapidly. The amount of mouisture in a cloud may increase causing it to release precipitation more rapidly.
Yes, under certain conditions, it is possible for a cloud to freeze. This can occur at high altitudes where temperatures are extremely cold, causing the water droplets in the cloud to freeze into ice crystals.
the tornado 'wanders' out and 'ventures' through the 'water' causing a 'water'spout
The Iceland ash cloud from the Eyjafjallajökull volcano eruption in 2010 lasted for about a week, causing widespread disruption to air travel in Europe.
The funnel cloud forms ins the very early stages as the vortex descends below cloud base. It pulls in moist air, and the pressure drop in side it cools the air, causing the moisture to condense.
A cloud that indicates a storm is approaching is a cumulonimbus cloud. It is a large, dense cloud that forms due to strong upward air currents and is known for causing thunderstorms and severe weather. Cumulonimbus clouds are often characterized by their towering, anvil-shaped appearance.
As the cloud collapses the force of gravity drawing the cloud inward gradually becomes stronger because the strength of gravity follows an inverse square law with distance. hope that helps.
Advection cloud refers to a type of cloud formation that occurs when warm, moist air moves horizontally and encounters cooler air, causing the warm air to rise and condense. This process often leads to the development of long, broad cloud structures, such as stratus clouds. Advection clouds are common in areas where different air masses meet.