Tidewatch

What is Extratidal High (low) Water?

Map for all points in Google

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.
• HAT is the elevation of Highest Astronomical Tide for the station shown. No predicted tide referenced to MSL or MLLW should ever be higher than HAT.
• LAT is the elevation of Lowest Astronomical Tide for the station shown. No predicted tide referenced to MSL or MLLW should ever be lower than LAT.
• MHHW, MSL, 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/ ).

Locations within the Chesapeake Bay Region

• SWPT - Sewells Point
• JMTN - Jamestown
• YRCG - York River Coast Guard
• WMPT - Windmill Point
• CBBT - Chesapeake Bay Bridge Tunnel
• MNPT - Money Point
• KIPT - Kiptopeke

For further information, please contact [[boon, John Boon]].