Presentation on theme: "Transfer of Datum for Hydrographic Surveys"— Presentation transcript:
1Transfer of Datum for Hydrographic Surveys Hydrographic Meteorological and Oceanographic Force Element GroupGabriela BallaManager of Tides and Geodetic ControlAustralian Hydrographic Service
2Sounding Datum and Chart Datum: Definitions Sounding Datum is the plane to which soundings are reduced during a hydrographic survey. It is the datum used when compiling a survey “fairsheet” and should be connected to chart datum via a landborne benchmark (BM).Chart Datum is the datum plane adopted for the published chart and is the level above which charted depths, tidal predictions and tidal levels are given in the Australian National Tide Tables (ANTT), AusTides and on the published chart.Ideally, sounding datum for a survey should be the same as the chart datum.
4Chart Datum: Lowest Astronomical Tide (LAT) Chart Datum should be:So low that the water level will seldom fall below it;Not so low as to cause the charted depths to be unrealistically shallow;That it should vary only gradually from area to area and from chart to adjoining chart, to avoid significant discontinuities.In accordance to a resolution of the International Hydrographic Organisation (IHO), Australia adopts Lowest Astronomical Tide (LAT) as the Chart Datum.
6Establish, Recover or Transfer of a Datum? Establish: Today, most surveys are undertaken in areas close to where an established datum already exists.Recover: Where areas have been previously surveyed, the original datum should be used utilising existing Benchmark records and levelling.Transfer: Where no datum exists in the survey area, but datum values exists nearby, the datum values can be transferred. Tidal datum should be transferred at intervals along the coast and distances between tidal stations will vary with different tidal conditions.Where tidal conditions change gradually, along an open coast, the maximum distance between tidal stations is 16 km. Where tidal conditions change rapidly, stations should be 1.6km or less apart.
7Issues with Datum Transfer Always investigate the known ranges of tide at places on either side of the survey before deciding whether a transfer is necessary or not.Serious errors in the reduction can be introduced by using tidal observations at a port which is too far way from the survey and has a different tidal range.
8Example of an Error introduced during Datum Transfer Two Standard Ports along a coast are 50km apartMHWS (from ANTT)MLWS (from ANTT)Mean Spring Range(MSR)Port A4.00.33.7Port B184.108.40.206Survey area ( Port C) lies between these two ports and is 20km from Port B.By linear Interpolation, Port C’s Mean Spring Range (MSR):MSR = /50x1.2 = 3.0mThe ratio of ranges between Port C and Port B = 3.0./2.5 = 1.2If the tide falls to datum at Port B, the range is about 2.7m and the range at Port C will be about 3.2m (2.7x1.2)
9Established Datum Transfer – Methods The primary methods of datum transfer will depend upon the character of the tide:Semi-diurnalDiurnalDirect comparison of low water heightsRatio of rises
10Semi-diurnal Transfer Method Where:R = the observed range at the established gauger = the observed range at the new gaugeM' = the height of observed mean level above CD/SD at the established gaugem' = the height of observed mean level above the zero of the new gaugeM = the height of the true Spring mean level above chart datum at the established gauged = the height of sounding datum above the zero of the new gauge
11Semi-diurnal Transfer Method (cont) Therefore, from the diagram it can be seen that the height of the sounding datum above the zero on the new gauge (d):d = m' – (M' – M) – [M x (r/R)]Where the true Spring Mean Level is not known, this formula reduces to:d = m' – [(M' x r)/R]
12Semi-diurnal Transfer Method (cont) Example AH533
13Semi-diurnal Transfer Method Example AH533 (cont)
14Diurnal Transfer Method – AHO-preferred H = the sum of the heights of the 4 principal constituents at the established gaugeh = the sum of the heights of the same constituents at new gaugeZ‘ = the height of MSL above Chart Datum at the established gauge (Zo from analysis).z‘ = the height of MSL above the zero of the new gauge (So from analysis)Zoo = the true (average) height of MSL above Chart Datum at the established gauge (obtained from ANTT)d = the height of sounding datum above the zero of the new gauge
15Diurnal Transfer Method (cont) From the previous slide it can be seen that:d = z' + (Zoo – Z') – [Zoo x (h/H)]Where the True Mean Sea Level (Zoo) is not known, this formula reduces to:d = z' – [Z' x (h/H)]
16Diurnal Transfer Method (cont) Example H = 0.79 (the sum of the heights of the 4 principal constituents at the established gaugeh = 1.25 (the sum of the heights of the same constituents at new gauge)Z‘ = 1.50 (the height of MSL above Chart Datum at the established gauge (Zo from analysis))z‘ = 2.60 (the height of MSL above the zero of the new gauge (So from analysis))Zoo = 1.15 (the true (average) height of MSL above Chart Datum at the established gauge (obtained from ANTT))From the equation on the previous page:d = z' + (Zoo - Z') – [Zoo x (h/H)]= (1.15 – 1.5) – [1.15 x (1.25/0.79)]= 2.6 – 0.35 – 1.82= 0.43m above the zero of the new gauge
17Direct ComparisonObserved LW heights at the new tidal station are plotted against predicted, or better still, the observed LW heights at the Standard Port.The point where the line of “best fit” cuts the axis of the new location is the height datum above (below) the zero of the new location.
18Establishing Datum for “Sketch” surveys The height of Sounding Datum (d) above the zero of the new gauge is obtained from:d = m – 0.5rwhere: r = [r/R] x Rm = observed Mean Level height at the new gauger = observed range at the new stationR = predicted range at the Standard PortR’ = required range at the Standard Port
19“Sketch” survey example Crocodile Beach (survey) Darwin (Standard Port)Observed H.W = 5.60m Predicted H.W = 5.52mObserved L.W = 1.95m Predicted L.W = 0.65mObserved Range ( r ) = 3.65m Predicted Range ( R ) = 4.87mObserved ML (m) = 3.78m Predicted ML = 3.09mApproximate ratio of ranges = [r/R] ->3.65/4.87 = 0.75From ANTT, Table I. LAT at Darwin = 0.0m and HAT at Darwin = 8.1m, hence R’ = 8.1The equivalent Range on the pole at Crocodile Beach will be:r = [r/R] x R -> x 8.1 = 6.07mand the required ½ range at the pole on Crocodile Beach will therefore be:0.5r -> 0.5 x = 3.04mThe height of Sounding Datum above/below the zero of the pole:d = m – 0.5r -> – = 0.74m above the zero of the pole
20Validation – Ratio of Rises AHO has the ability from harmonic constants to compare the new location to the standard port to determineD = Ratio Range*Std Port + MSL OffsetTime difference
21Establishing an Independent Datum By reference to the land levelling system where the relationship between Chart Datum and the Australian Height Datum (AHD) is known at neighbouring places.By harmonic constants – rarely used these days.By mean sea level – where the tidal range is small.
22Establishing Datums in Rivers and Estuaries There are methods for establishing tidal datums in:A riverRiver entrance and estuaryAreas of impounding
23Establishing Datums in Rivers and Estuaries (cont) As a tidal wave enters the estuary it is constricted:Causes a gradual increase in range so high waters begin to rise higher and low waters to fall lower as the wave proceeds up the estuary.This continues to a point where the topography of the sea bed no longer permits the lowest low water to continue falling.Another complicating factor in the upper reaches of the river is the effect of varying quantities of river water coming down stream.
24Establishing Datums in Rivers and Estuaries (cont) General Principles to keep in mindThe sea bed topographyRiver and tidal flow boundaryRiver entrances with large sand banksImpounding zones
25Off-shore Datums: Co-Tidal Charts Relate to waters some distance from the shoreline but depth of water doesn’t allow a tide gauge to be positionedCo-tidal charts are constructedAssumptionsTruly accurate near HW/LW ->errors may occur at other times, particularly near half-tideChanges between the lines are linearRefer to Admiralty NP122(2) for instructions
26Off-shore Datums: Semi-Diurnal Co-Tidal Charts Solid co-tidal lines: show time corrections based on tide time at APecked co-range lines: tide range ratios on the tide at AAt B: high water 30 min before ATidal range is 0.65x the range at A
27Connecting Chart Datum to the Australian Height Datum (AHD)
28Connecting Chart Datum to the Australian Height Datum (AHD): Benchmarks Critical to ensure that levelling between gauge and marks are madeLevelled into the Land levelling network and or connection to Ellipsoidal Height for Geoid referencing.