This form of lightening happens with a buildup of one type of charge, usually a positive change that come from the top of a thunderstorm, releases to an area of opposite change, that is somewhere in the atmosphere around the storm. Cloud-to-air lightening is not generally as powerful as an actual bolt of lightening that strikes the ground. In addition, this form of lightening is usually seen when the storm is farther away to the person who happens to see this bolt. When one sees this kind of bolt, there is usually no thunder due to how far away the storm is from their actual location. However, when this positive bolt does make contact with the ground, it is called a Bolt from the Blue, because the positive lightening travels straight out of the storm, for a few miles, and then strikes the ground (What causes lightning?). Cloud-to-ground lightening most often occurs near the boundary between the updraft region, where the darkest clouds are formed, and the downdraft/raining region, which is the lighter, fuzzy appearance. Sometimes, however, the lightening bolt can come out of the side of the storm, and strike a location miles away, seemingly from out of the clear blue
This form of lightening happens with a buildup of one type of charge, usually a positive change that come from the top of a thunderstorm, releases to an area of opposite change, that is somewhere in the atmosphere around the storm. Cloud-to-air lightening is not generally as powerful as an actual bolt of lightening that strikes the ground. In addition, this form of lightening is usually seen when the storm is farther away to the person who happens to see this bolt. When one sees this kind of bolt, there is usually no thunder due to how far away the storm is from their actual location. However, when this positive bolt does make contact with the ground, it is called a Bolt from the Blue, because the positive lightening travels straight out of the storm, for a few miles, and then strikes the ground (What causes lightning?). Cloud-to-ground lightening most often occurs near the boundary between the updraft region, where the darkest clouds are formed, and the downdraft/raining region, which is the lighter, fuzzy appearance. Sometimes, however, the lightening bolt can come out of the side of the storm, and strike a location miles away, seemingly from out of the clear blue