Sea Level Measurement <strong>and</strong> Interpretati<strong>on</strong>should fix the datum to approximately centimetre accuracy.However it is tedious <strong>and</strong> can <strong>on</strong>ly be carried outinfrequently in remote areas.3.3.4 Multiple Pressure Transducer Systems(‘B’ gauges)A method was developed at POL in the early 1990sfor precise datum c<strong>on</strong>trol of <strong>sea</strong> <strong>level</strong> records frompressure tide gauges. An additi<strong>on</strong>al pressure pointwas located at approximately mean <strong>sea</strong> <strong>level</strong> <strong>and</strong>fixed relative to the c<strong>on</strong>tact point of the gauge. Thejuncture at which the tide fell below this sec<strong>on</strong>dsensor could be used to fix the datum of the recordfrom the principal sensor. The technique was foundto be extremely reliable <strong>and</strong> accurate <strong>and</strong> now formsthe basis of gauges, called ‘B’ gauges, in POL’s SouthAtlantic <strong>and</strong> Antarctic networks (Spencer et al.,1993). The principle of the technique was describedin detail in Volume 2 of the <str<strong>on</strong>g>Manual</str<strong>on</strong>g> (IOC, 1994) <strong>and</strong>in the scientific literature (Woodworth et al., 1996).At the time of writing, it is not possible to purcha<strong>sea</strong> ‘B’ gauge although expressi<strong>on</strong>s of interest in theirmanufacture have been obtained from major suppliers.A schematic ‘B’ gauge setup is shown in Figure 3.4,with an absolute pressure sensor in the water (‘C’)<strong>and</strong> another in the atmosphere (‘A’). Paroscientificdigiquartz sensors are employed throughout, althoughless expensive sensors should work reas<strong>on</strong>ably well<strong>and</strong> are being investigated. The difference C–A gives<strong>sea</strong> <strong>level</strong>, after correcti<strong>on</strong>s for <strong>sea</strong>water density <strong>and</strong>accelerati<strong>on</strong> due to gravity are applied. A third sensoris placed at ‘Datum B’ which is near mean <strong>sea</strong> <strong>level</strong>.The height of ‘Datum B’ has to be known accuratelyrelative to the c<strong>on</strong>tact point of the installati<strong>on</strong> <strong>and</strong> tothe local l<strong>and</strong> <strong>level</strong>ling network. The difference B–A isagain a <strong>sea</strong> <strong>level</strong> height, but <strong>on</strong>ly when the <strong>sea</strong> <strong>level</strong>is above ‘Datum B’. The top part of this record can befitted to the equivalent part of the record from theprincipal sensor to transpose the known datum to thefull <strong>sea</strong> <strong>level</strong> record. It is important that all sensors aredriven from the same c<strong>on</strong>trol <strong>and</strong> logging system tomaintain synchr<strong>on</strong>y. Sampling the data at 15-minuteintervals or less is preferred for the identificati<strong>on</strong> ofthe inflexi<strong>on</strong> points, i.e. the time at which the <strong>sea</strong> <strong>level</strong>falls (or rises) below (or above) ‘Datum-B’.The essential feature is that, while any pressure measuredby a sensor at B will c<strong>on</strong>tain an offset, <strong>and</strong> perhapsa drift, the vertical height of its effective pressurepoint can be positi<strong>on</strong>ed at ‘Datum B’ very accurately.So, although it is not known what it is measuring towithin perhaps a few hectopascals (centimetres), it isknown where it is measuring with millimetric precisi<strong>on</strong>.The flat part of B–A <strong>and</strong> its inflexi<strong>on</strong> points provide anextremely precisely defined shape which is immune toany problems with datum offsets <strong>and</strong> low-frequencyinstrumental drifts. Experience with several instrumentsat different sites suggests that datums can be fixed towithin a few millimetres by this technique.To work properly, the method needs a sizable tidal range,so that B will spend half its time in water <strong>and</strong> half in air.It will not work in lakes or microtidal areas, but mostcoastal <strong>and</strong> many isl<strong>and</strong> sites have usable tidal ranges,even if <strong>on</strong>ly at spring tides. In the presence of waves,the flat porti<strong>on</strong> of the ‘B’ gauge is reduced in length<strong>and</strong> may be unu<strong>sea</strong>ble under large wave c<strong>on</strong>diti<strong>on</strong>s.However, there are is always a sufficient number of calmdays during which the technique can be applied.In practice, the two pressure sensors in the <strong>sea</strong> are colocatednear the base of the installati<strong>on</strong> with a rigidtube c<strong>on</strong>necting the ‘B’ gauge to its appropriate datumpoint. This avoids the ‘B’ sensor being subject to atmospherictemperature variati<strong>on</strong>s that are more severethan those of the <strong>sea</strong>. The barometric sensor may alsobe installed at the same positi<strong>on</strong> with a tube open toatmosphere. Alternatively it may be installed as partof the data logger in the tide gauge hut. The methoddoes not require the actual installed height of C or A tobe known. Where it is difficult to install a fixed gaugeC below the water, because of shallow gradients perhaps,then a pop-up or bottom-mounted gauge couldequally well be used.3.3.5 Pressure Transducers in Stilling WellsA variant of the ‘B’ gauge method described aboveis to install an absolute pressure sensor below lowwater in a stilling well that has been used hithertoin a float system. This transducer will be functi<strong>on</strong>allythe same as sensor ‘C’ <strong>and</strong> will be complementedby a transducer ‘A’ that records atmospheric pressure,as described above. Alternatively, a ‘differential’sensor could be used. Instead of a third sensoremployed in the ‘B’ gauge, datum c<strong>on</strong>trol for theC–A pressure-difference time-series is provided bymeans of regular, preferably daily, electr<strong>on</strong>ic datumprobe checks of the <strong>level</strong> in the well relative to thetide gauge CP <strong>and</strong> TGBM. Comparis<strong>on</strong> of the valuesof C–A, corrected for density <strong>and</strong> accelerati<strong>on</strong>due to gravity, with the well soundings, providesan <strong>on</strong>going datum for the time-series which canaccommodate transducer drift <strong>and</strong> variati<strong>on</strong>s in theproperties of the <strong>sea</strong> water.This method has many of the advantages of pressuresystems <strong>and</strong> of electr<strong>on</strong>ic datum probes, combinedwith the recognized disadvantages inherent in theuse of stilling wells (Lenn<strong>on</strong>, 1971). It may be apreferred opti<strong>on</strong> if <strong>measurement</strong>s are required froma well that has produced l<strong>on</strong>g-term <strong>measurement</strong>sfrom a float gauge.3.3.6 Bottom-mounted Pressure GaugesBottom pressure gauges rest <strong>on</strong> the <strong>sea</strong> bed <strong>and</strong>record pressure at intervals over periods of a year or16IOC <str<strong>on</strong>g>Manual</str<strong>on</strong>g>s <strong>and</strong> Guides No 14 vol IV
Sea Level Measurement <strong>and</strong> Interpretati<strong>on</strong>amore. They are self-c<strong>on</strong>tained instruments poweredby batteries. They have little applicati<strong>on</strong> to the l<strong>on</strong>gterm<strong>measurement</strong> of coastal <strong>sea</strong> <strong>level</strong> but have beenused extensively to obtain initial tidal knowledge ofan area where a coastal gauge is planned. Their mainproblem in the GLOSS c<strong>on</strong>text is the lack of a datum.They have principally proved their value offshore <strong>and</strong>in the deep ocean (Spencer <strong>and</strong> Vassie, 1997).3.4 Acoustic Tide GaugesA number of acoustic tide gauges have been developedwhich depend <strong>on</strong> measuring the travel timeof acoustic pulses reflected vertically from the <strong>sea</strong>surface. This type of <strong>measurement</strong> can theoreticallybe made in the open with the acoustic transducermounted vertically above the <strong>sea</strong> surface, but in certainc<strong>on</strong>diti<strong>on</strong>s the reflected signals may be lost. Toensure c<strong>on</strong>tinuous <strong>and</strong> reliable operati<strong>on</strong> the sensoris located inside a tube that provides some degreeof surface stilling <strong>and</strong> protects the equipment; somesensors even c<strong>on</strong>strain the acoustic pulses within anarrow vertical tube, which is c<strong>on</strong>tained inside theprevious <strong>on</strong>e. This outer tube does not completelyfilter out wave acti<strong>on</strong> but, by averaging a number of<strong>measurement</strong>s, the desired filtering is achieved.bThe velocity of sound in air varies significantly withtemperature <strong>and</strong> humidity (about 0.17%/°C) <strong>and</strong>some form of compensati<strong>on</strong> is necessary to obtainsufficient accuracy. The simplest method is to measurethe air temperature c<strong>on</strong>tinuously at a point inthe air column <strong>and</strong> use this to calculate the soundvelocity. To account for temperature gradients in theair column, temperature sensors may be required ata number of different <strong>level</strong>s.A more accurate method of compensati<strong>on</strong> is by useof an acoustic reflector at a fixed <strong>level</strong> in the air column.By relating the reflecti<strong>on</strong> from the <strong>sea</strong> surfaceto that from the fixed reflector, direct compensati<strong>on</strong>for variati<strong>on</strong> in sound velocity between the acoustictransducer <strong>and</strong> the fixed reflector can be achieved.However this still does not account for any variati<strong>on</strong>in sound velocity between the fixed reflector <strong>and</strong>the <strong>sea</strong> surface. To achieve full compensati<strong>on</strong> wouldrequire, in principle, a number of fixed reflectorscovering the full tidal range, but n<strong>on</strong>e of the knownacoustic sensors has this possibility.Figure 3.4 (a,b) Schematics of operati<strong>on</strong> of a ‘B’ gauge.3.4.1 Acoustic Gauges with Sounding TubesThe Nati<strong>on</strong>al Oceanic <strong>and</strong> Atmospheric Administrati<strong>on</strong>(NOAA), Nati<strong>on</strong>al Ocean Service (NOS) in the USA,initiated over a decade ago a multi-year implementati<strong>on</strong>of a Next-Generati<strong>on</strong> Water Level MeasurementSystem (NGWLMS), both within the US nati<strong>on</strong>altide gauge network <strong>and</strong> at selected sites aroundIOC <str<strong>on</strong>g>Manual</str<strong>on</strong>g>s <strong>and</strong> Guides No 14 vol IV17