The purpose of this work is to gain a better understanding of the mechanisms that control precipitation in the Southeastern United States. An emphasis is placed on droughts and floods as these events have significant impact on the environment, livlihood, and general health of the affected region.
Of particular interest is the Bermuda High as a primary mechanism in controlling precipitation and moisture flux transport into the Southeast. This is an area of continued work in order to further understand the effects of the Bermuda High.
It is important to note that many mechanisms serve to influence precipitation patterns in the Southeast and that others exist outside of those discussed here.