Manual on sea level measurement and ... - unesdoc - Unesco

Manual on sea level measurement and ... - unesdoc - Unesco Manual on sea level measurement and ... - unesdoc - Unesco

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Sea Level Measurement and InterpretationAPPENDIX V.Contributed Practical Experiences with VariousTide Gauge TechnologiesThis appendix contains contributions kindly provided by thefollowing people:Daniel Hareide, Hodnesdal, Tor Tørresen and Tor EllefHansen Østebøvik (Norwegian Hydrographic Service)B. Martín, B. Pérez, E. Alvarez Fanjul (Puertos del Estado,Spain)Christoph Blasi and Ulrich Barjenbruch (Federal Instituteof Hydrology, Germany)Ruth Farre (South African Navy Hydrographic Office)Antony Joseph, Prakash Mehra, Joseph Odammeteyand Nkebi E. Kofi (National Institute of Oceanography, India,and Survey of Ghana)Juan Fierro, Chilean Navy Hydrographic and OceanographicService (SHOA)Bernie Kilonsky (University of Hawaii Sea Level Center,USA)Peter Foden (Proudman Oceanographic Laboratory, UK)Laura Kong (International Tsunami Information Centre,Hawaii, USA)Each of these experts is willing to discuss aspects of theirexperiences in more detail with anyone interested.Float Gauges in Stilling Wells: Experience in NorwayDaniel Hareide, Hanne Hodnesdal, Tor Tørresen and Tor Ellef Hansen ØstebøvikNorwegian Hydrographic Service, P.O. Box 60, 4001 Stavanger, NORWAYE-mail: daniel.hareide@statkart.noThe float gauge and stilling wellThe Norwegian Tide Gauge Network, operated by theNorwegian Hydrographic Service (NHS), records sealevel elevations with float gauges at 23 locations.cone, and unwanted wave oscillations are not reducedas they are supposed to be. Inside the cone there is aA typical Norwegian stilling well consists of a polyethylenetube with a conical inlet at the bottom (Figure1). The diameter of the tube is 30 or 40 cm and theinlet (cone) is of copper to reduce marine fouling. Wehave seen that galvanic corrosion can be a problem,probably since we have used parts of stainless steel toclamp the cone to the tube. This can cause holes in theFigure 1. Sea level gauge in Norway and schematic description of stilling well with copper cone and bronze plug.58IOC ong>Manualong>s and Guides No 14 vol IV

Sea Level Measurement and Interpretationremovable orifice of bronze and the orifice can beadjusted with one or more nipples. Some of the tidalstations in Norway are exposed to ice and low temperatures,and 220 V AC heating cables are installed insidethese wells.Each sea level gauge has at least one level switchused for quality control. It is installed inside the stillingwell approximately at mean sea level (MSL). The levelswitch is a tiny float, which switches a current loopwhen the sea level passes the level at which the switchis mounted. The computer registers the time and sealevel when the switch turns on or off, and these datacan be compared with the level at which the switch ismounted. The level switch has been very important inthe detection of several problems, such as drift (trend)in the observations.An encoder with an SDI-12 output is installed abovethe tube, mounted on a concrete block (Figure 2). Theencoder has a sprocket (wheel) on the shaft and is programmedto give an output with a resolution of 0.1cm. The encoder has internal battery backup whichremembers the angular position, in case of powerfailure. A chain with a float and a counterweight runsover the sprocket and the sea level is given by theangular position of the sprocket. It is important thatthe sprocket and chain fit well together. If not, therecould be very small tangential movements betweenthe sprocket and chain and this in turn presents itselfas very slow drift (trend) in the sea level observations.NHS is using a US manufacturer of the chainand sprocket (W.M.Berg Inc. (www.wmberg.com)).Leading marks on the chain and sprocket make it easyto control the system.The data logger is a Sutron 8210 and it collects andstores sea level, barometric pressure and switch-leveldata. The memory of the Sutron 8210 has batterybackup and can hold several months of data.Normally the data are retrieved twice a day from thedata logger, sometimes more often. The data loggerhas a serial port, which is used for communication,either through the ISDN-network or with a GPRS-router.We are now in the process of converting the datatransmission from the ISDN-network to GPRS-routerfor all the tidal stations. This work will be completedduring the next 2–3 years (depending on allocatedbudget) and sea level data will be sent to the office inStavanger every 10–20 min and will be immediately(an automatic quality control is applied to the data)available on our website.The data logger and the communication unit have separatebattery backups. The data logger has less powerconsumption than the communication unit, so, in caseof power failure, the gauge will continue to store dataeven if the communication is broken.ChainContact PointEncoderFigure 2. Encoder, chain and contact point.Levelling is done from the TGBM and one or twoadditional benchmarks to a contact point at thesame bracket as the encoder. The TGBM is in solidrock as close to the sea level gauge as possible.After modernization of the gauges between 1985and 1991, levelling has been done every year. Sincemost of the gauges are located on stable ground,the levelling interval now is three years, except for afew gauges which are sinking. The levelling followsthe procedures outlined in the UNESCO ong>Manualong> onSea-Level Measurement and Interpretation, Volume I,and the accuracy is millimetric. It is more difficult tocalibrate the sea level gauge to the same accuracy.Calibration is done by measuring the distance fromthe sea surface to the contact point with a levellingstaff inside the well, and by taking simultaneouslyreadings on the sea level gauge. This is repeatedseveral times, and the sea level gauge is calibrated bymaking its readings equal to the observations on thestaff. Taking many readings will reduce the problemwith a moving sea surface. There might, however, besome individual differences in the way the calibrationis performed and this may introduce systematicerrors of a few millimetres. We use a sea level gaugezero that is below the lowest observed sea level. Toavoid any confusion, we never use levels like ChartDatum or Land Survey Datum as the gauge zero.The sea level gauges are inspected at intervals of 18months. We should like to carry out levelling andinspections more frequently, but we have to reducethe operational costs as much as possible.For all stations, a close co-operation with localoperators is essential. They look after the equipmentand assist us in various situations, i.e. whenthere are power or communication problems withthe gauge.IOC ong>Manualong>s and Guides No 14 vol IV59

Sea Level Measurement <strong>and</strong> Interpretati<strong>on</strong>removable orifice of br<strong>on</strong>ze <strong>and</strong> the orifice can beadjusted with <strong>on</strong>e or more nipples. Some of the tidalstati<strong>on</strong>s in Norway are exposed to ice <strong>and</strong> low temperatures,<strong>and</strong> 220 V AC heating cables are installed insidethese wells.Each <strong>sea</strong> <strong>level</strong> gauge has at least <strong>on</strong>e <strong>level</strong> switchused for quality c<strong>on</strong>trol. It is installed inside the stillingwell approximately at mean <strong>sea</strong> <strong>level</strong> (MSL). The <strong>level</strong>switch is a tiny float, which switches a current loopwhen the <strong>sea</strong> <strong>level</strong> passes the <strong>level</strong> at which the switchis mounted. The computer registers the time <strong>and</strong> <strong>sea</strong><strong>level</strong> when the switch turns <strong>on</strong> or off, <strong>and</strong> these datacan be compared with the <strong>level</strong> at which the switch ismounted. The <strong>level</strong> switch has been very important inthe detecti<strong>on</strong> of several problems, such as drift (trend)in the observati<strong>on</strong>s.An encoder with an SDI-12 output is installed abovethe tube, mounted <strong>on</strong> a c<strong>on</strong>crete block (Figure 2). Theencoder has a sprocket (wheel) <strong>on</strong> the shaft <strong>and</strong> is programmedto give an output with a resoluti<strong>on</strong> of 0.1cm. The encoder has internal battery backup whichremembers the angular positi<strong>on</strong>, in case of powerfailure. A chain with a float <strong>and</strong> a counterweight runsover the sprocket <strong>and</strong> the <strong>sea</strong> <strong>level</strong> is given by theangular positi<strong>on</strong> of the sprocket. It is important thatthe sprocket <strong>and</strong> chain fit well together. If not, therecould be very small tangential movements betweenthe sprocket <strong>and</strong> chain <strong>and</strong> this in turn presents itselfas very slow drift (trend) in the <strong>sea</strong> <strong>level</strong> observati<strong>on</strong>s.NHS is using a US manufacturer of the chain<strong>and</strong> sprocket (W.M.Berg Inc. (www.wmberg.com)).Leading marks <strong>on</strong> the chain <strong>and</strong> sprocket make it easyto c<strong>on</strong>trol the system.The data logger is a Sutr<strong>on</strong> 8210 <strong>and</strong> it collects <strong>and</strong>stores <strong>sea</strong> <strong>level</strong>, barometric pressure <strong>and</strong> switch-<strong>level</strong>data. The memory of the Sutr<strong>on</strong> 8210 has batterybackup <strong>and</strong> can hold several m<strong>on</strong>ths of data.Normally the data are retrieved twice a day from thedata logger, sometimes more often. The data loggerhas a serial port, which is used for communicati<strong>on</strong>,either through the ISDN-network or with a GPRS-router.We are now in the process of c<strong>on</strong>verting the datatransmissi<strong>on</strong> from the ISDN-network to GPRS-routerfor all the tidal stati<strong>on</strong>s. This work will be completedduring the next 2–3 years (depending <strong>on</strong> allocatedbudget) <strong>and</strong> <strong>sea</strong> <strong>level</strong> data will be sent to the office inStavanger every 10–20 min <strong>and</strong> will be immediately(an automatic quality c<strong>on</strong>trol is applied to the data)available <strong>on</strong> our website.The data logger <strong>and</strong> the communicati<strong>on</strong> unit have separatebattery backups. The data logger has less powerc<strong>on</strong>sumpti<strong>on</strong> than the communicati<strong>on</strong> unit, so, in caseof power failure, the gauge will c<strong>on</strong>tinue to store dataeven if the communicati<strong>on</strong> is broken.ChainC<strong>on</strong>tact PointEncoderFigure 2. Encoder, chain <strong>and</strong> c<strong>on</strong>tact point.Levelling is d<strong>on</strong>e from the TGBM <strong>and</strong> <strong>on</strong>e or twoadditi<strong>on</strong>al benchmarks to a c<strong>on</strong>tact point at thesame bracket as the encoder. The TGBM is in solidrock as close to the <strong>sea</strong> <strong>level</strong> gauge as possible.After modernizati<strong>on</strong> of the gauges between 1985<strong>and</strong> 1991, <strong>level</strong>ling has been d<strong>on</strong>e every year. Sincemost of the gauges are located <strong>on</strong> stable ground,the <strong>level</strong>ling interval now is three years, except for afew gauges which are sinking. The <strong>level</strong>ling followsthe procedures outlined in the UNESCO <str<strong>on</strong>g>Manual</str<strong>on</strong>g> <strong>on</strong>Sea-Level Measurement <strong>and</strong> Interpretati<strong>on</strong>, Volume I,<strong>and</strong> the accuracy is millimetric. It is more difficult tocalibrate the <strong>sea</strong> <strong>level</strong> gauge to the same accuracy.Calibrati<strong>on</strong> is d<strong>on</strong>e by measuring the distance fromthe <strong>sea</strong> surface to the c<strong>on</strong>tact point with a <strong>level</strong>lingstaff inside the well, <strong>and</strong> by taking simultaneouslyreadings <strong>on</strong> the <strong>sea</strong> <strong>level</strong> gauge. This is repeatedseveral times, <strong>and</strong> the <strong>sea</strong> <strong>level</strong> gauge is calibrated bymaking its readings equal to the observati<strong>on</strong>s <strong>on</strong> thestaff. Taking many readings will reduce the problemwith a moving <strong>sea</strong> surface. There might, however, besome individual differences in the way the calibrati<strong>on</strong>is performed <strong>and</strong> this may introduce systematicerrors of a few millimetres. We use a <strong>sea</strong> <strong>level</strong> gaugezero that is below the lowest observed <strong>sea</strong> <strong>level</strong>. Toavoid any c<strong>on</strong>fusi<strong>on</strong>, we never use <strong>level</strong>s like ChartDatum or L<strong>and</strong> Survey Datum as the gauge zero.The <strong>sea</strong> <strong>level</strong> gauges are inspected at intervals of 18m<strong>on</strong>ths. We should like to carry out <strong>level</strong>ling <strong>and</strong>inspecti<strong>on</strong>s more frequently, but we have to reducethe operati<strong>on</strong>al costs as much as possible.For all stati<strong>on</strong>s, a close co-operati<strong>on</strong> with localoperators is essential. They look after the equipment<strong>and</strong> assist us in various situati<strong>on</strong>s, i.e. whenthere are power or communicati<strong>on</strong> problems withthe gauge.IOC <str<strong>on</strong>g>Manual</str<strong>on</strong>g>s <strong>and</strong> Guides No 14 vol IV59

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