Contact: David Malmquist
Virginia Institute of Marine Science
Caption: Intra-seasonal variability (bottom panel) can raise water levels a moderate amount over long periods (here 3 weeks in 2009). Hurricanes and nor'easters (e.g., Irene in 2011) generate higher, shorter peaks. "Superstorm Sandy" (top panel) was unusual in generating a storm surge that persisted through numerous tidal cycles. All data are from the Chesapeake Bay Bridge Tunnel. MLLW = Mean Lower Low Water.
Credit: Graph compiled from NOAA tide gauge data by Dr. John Brubaker
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