Extratidal Water Level: recent observations

Note - This data and webpage is a work in progress.

These water level stations are being incorporated into the tidewatch system:


 These stations are in Newport News (NN), Virginia Beach (VB), and Norfolk (NF).

A Brief Summary and Explanation of Terms

  • Extratidal High Water (XHW) and Extratidal Low Water (XLW) are observed water-level extremes measured above the tidal datum HAT (XHW) or below the tidal datum LAT (XLW). These extremes occur only in the presence of a weather-induced residual water level or "storm surge" (observed water level minus the astronomic tide), a sea-level anomaly (m30-MSL vertical difference) or, more often, a combination of the two. The astronomic tide—the water level change occurring at tidal frequencies—will not exceed either datum in the absence of a sea-level anomaly.
  • m30 is the 30-day mean water level covering the period of observation shown. It represents a time-local departure from MSL that is due to a combination of the seasonal tide, the decadal change in sea level, and the long-term sea-level trend relative to the land. The vertical reference for the astronomic tide is m30.
  • HAT83 is the elevation of Highest Astronomical Tide above MSL (1983-2001) at the station shown.
  • LAT83 is the elevation of Lowest Astronomical Tide below MSL (1983-2001) at the station shown.
  • MHHW, MSL, and MLLW are the tidal datums of Mean Higher High Water, Mean Sea Level, and Mean Lower Low Water as defined by NOAA/NOS for the 1983-2001 National Tidal Datum Epoch (See http://tidesandcurrents.noaa.gov).

For a more extensive explanation, read "What is Extratidal High or Low Water?" (pdf).

Read our Disclaimer and Methods Disclosure document (pdf).