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==Synoptic evolution==
A shortwave moved through the southern stream of the polar jet of the Westerlies, dropping temperatures in its wake across the southeast [[United States]]. [[Cyclogenesis]] spurred a developing surface [[cyclone]] which quickly occluded. Surface pressure gradient between this cyclone and a sprawling high stretching around its periphery from [[New England]] into the [[Deep South]] led to strong winds in the Carolinas. The cyclone deepened to a central pressure of 999 [[hPa]] 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 low pressure center which moved offshore the Mid-Atlantic later on [[November 22]] and then proceded towards [[New England]] late on [[November 23]]. This cyclone was much weaker, and its effects for the [[Mid-Atlantic States]] and New England states were less significant than seen in the Carolinas.
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==Effects==
[[Image:Namussfc2006112212.gif|thumb|right|250 px|[[Surface analysis]] from [[November 22]], [[2006]] at 1200 [[UTC]] showing the cyclone moving into mainland [[North Carolina]]]]
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