Timely seeding of the feeder clouds can lessen the storm’s severity, while increasing overall rainfall. This is accomplished in a variety of ways, effectively spreading the energy released by the storm over a slightly larger area. The concept of dynamic seeding is a physically plausible approach that offers an opportunity to increase rainfall by much larger amounts than the static concept.  This concept is to seed supercooled clouds with large enough quantities of ice nuclei to cause glaciation of the cloud.  Due to seeding, supercooled liquid water is converted into ice particles, releasing latent heat, increasing buoyancy, and thereby invigorating cloud updrafts.  In favorable conditions, this will cause the cloud to grow larger, process more water vapor, and yield more precipitation (Bruintjes, 1999).  The enhanced updraft may also promote the initiation of convection in the surroundings.