A New Formula for the Rain Dew Point II

In the first version of this document there were errors, which will be addressed in ERRATUM. The formula proved was the following for the rain dew point [1].

To–T=(3kTo2/σoao)(P*H2O/Pair)

A table will be devised to show the use of this equation in atmospheric chemistry. All of the variables here can be obtained and T is the undercooling below to the freezing point of water. Pure water can be supercooled to about – 40 °C. The best place to intervene with cloud seeding is in mountains to feed the rivers for the crops [2].