Vertical datums and water levels

All surveyed features on a navigational chart are positioned on some horizontal datum system such as NAD27 (North American Datum of 1927) or NAD83 (North American Datum of 1983). In addition to a horizontal datum reference, all charts also require a vertical datum reference.

For navigational safety, depths on a chart are shown from a low-water surface or a low-water datum called chart datum. Chart datum is selected so that the water level will seldom fall below it and only rarely will there be less depth available than what is portrayed on the chart. In non-tidal waters, chart datum is set so that the water level will be above datum approximately 95% of the time.

The water level of a lake or river is always changing due to variations in supply and discharge or in meteorological conditions. Dry and wet periods in many drainage basins such as the Great Lakes seem to occur in several-year cycles, causing corresponding periods of low and high water. Chart datum must be set with the low-stage years in mind and may appear pessimistically low during high-stage years.

On most lakes a single, level surface is adopted as chart datum over the whole lake. Along a river, chart datum is a sloping surface that approximates the slope of the river surface at low stage.

In non-tidal waters, chart datums are often assigned an elevation on some vertical reference system. On the Great Lakes, water level and chart datum elevations are presently referenced to International Great Lakes Datum 1985 (IGLD 1985). Some of the previous vertical reference systems used for charting on the Great Lakes are IGLD 1955, USLS 1903 (U.S. Lake Survey 1903 Datum) and USLS 1935.

A new reference system is required approximately every 25-30 years to correct for differential movement of the earth's crust in the Great Lakes region. IGLD 1985 was implemented in January 1992 and replaced the previous system, IGLD 1955. Since the plane of chart datum was not changed, the depths and heights portrayed on the charts are the same for both reference systems. However, the elevation assigned to chart datum is slightly different.

Nautical charts also require a high-water line which is used to define some vertical features and the shoreline on a chart. The high-water line is selected as a level above which the water will seldom rise. For example, a level of 1.3 metres above chart datum is used for the high-water line on CHS charts of Lake Ontario and Lake Erie.

As features on a chart, a depth falls below chart datum, a rock awash is at chart datum, a drying height falls between chart datum and the high-water line and a height is above the high-water line. This information is shown graphically on page 36 in the current CHS Chart Number 1 publication that explains all of the symbols, abbreviations and terms used on navigational charts.

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In tidal waters, clearances and elevations are given above high water. In non-tidal waters such as the Great Lakes, heights of islands, clearances and elevation of lights are given above chart datum. Therefore, a knowledge of the present water level relative to chart datum is required to correct these charted heights and all depths to the current conditions. For example, a clearance of 9 metres on an inland chart will only be 8 metres when the water level is one metre above chart datum.

Water-level gauges are referenced to the same vertical datums that are used for charts. To inform the mariner of the possible range of water-level fluctuations, a hydrograph is included on non-tidal charts to show the average water level and extreme levels for each month from historical observations. Up-to-date water-level information for the Great Lakes is available from water-level bulletins as monthly averages, on marine broadcasts as weekly averages or directly from CHS announcing gauges for the present levels.