 The cyclone deepened to a central pressure of before swinging westward into the Outer Banks of North Carolina on November 22.At this time, a trio of upper-level shortwaves were rotating around the main closed cyclone aloft, which spurred development of a new, weaker low pressure center offshore North Carolina.This cyclone was weaker after its interaction with North Carolina until it reached New England, when renewed strengthening led to significant impacts across Long Island and southern New England.