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Sea-Level Science: Understanding Tides, Surges, Tsunamis and Mean Sea-Level Changes PDF

409 Pages·2014·37.106 MB·English
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i C:/ITOOLS/WMS/CUP-NEW/4604986/WORKINGFOLDER/PUGH/9781107028197HTL.3D [1–2]12.12.20135:22PM Sea-Level Science Understanding Tides, Surges, Tsunamis and Mean Sea-Level Changes Sealevelschangeformanyreasonsandonmanytimescales,andextremesea levelscanresultincatastrophiccoastalflooding,suchastheKatrinastorm surgein2005ortheSumatratsunamiin2004.Asglobalsealevelrises,and coastalpopulationsincrease,understandingsea-levelprocessesbecomeskey toplanfuturecoastaldefenceeffectively. Oceantides,stormsurges,tsunamis,ElNiñoandthesea-levelrisecaused byclimatechangeareamongtheprocessesexplainedinthisbook.Buildingon DavidPugh’sclassicgraduate-levelbookTides,SurgesandMeanSea-Level, thissubstantiallyupdatedandexpandedfull-colourbooknowincorporates majorrecenttechnologicaladvancesintheareasofsatellitealtimetryand othergeodetictechniques(particularlyGPS),tsunamiscience,measurement ofmeansealevelandanalysesofextremesealevels.Theauthors,bothleading internationalexperts,discusshoweachsurveyingandmeasuringtechnique complementsothersinprovidinganunderstandingofpresent-daysea-level changeandmorereliableforecastsoffuturechanges. Givingthehowandthewhyofsea-levelchangeontimescalesfromhours tocenturies,thisauthoritativeandexcitingbookisidealforgraduatestudents andresearchersworkinginoceanography,marineengineering,geodesy, marinegeology,marinebiologyandclimatology.Itwillalsobeofkeyinterest tocoastalengineersandgovernmentalpolicy-makers. DavidPughisamarinescienceconsultant,alsoholdingpositionsas VisitingProfessorattheUniversityofLiverpoolandVisitingScientistatthe NationalOceanographyCentre(NOC).Hisresearchspecialisesintides, surges,meansealevel,coastalmanagementandclimatechange,togetherwith marineeconomicsandthehistoryofsealevel.Afteracareerinscienceand sciencemanagementwiththeUKNaturalEnvironmentResearchCouncil, DrPughservedasPresidentoftheIntergovernmentalOceanographic Commission(IOC)ofUNESCO,2003–7.HehadpreviouslybeenDirectorof thePermanentServiceforMeanSeaLevelandFoundingChairmanoftheIOC GlobalSeaLevelnetwork,GLOSS.DrPughhasauthoredtwobooksand recentlyco-editedTroubledWaters:OceanScienceandGovernance (CambridgeUniversityPress,2010)publishedforthe50thanniversaryofthe IOC.HehasbeenawardedanOBEforservicestomarinesciences. PhilipWoodworthisanIndividualMeritScientistintheNatural EnvironmentalResearchCouncilbasedattheNOCinLiverpool,andalsoa VisitingProfessorattheUniversityofLiverpool.HehasbeenDirectorofthe PSMSLandChairmanofGLOSS.DrWoodworthhaspublishedextensively ii C:/ITOOLS/WMS/CUP-NEW/4604986/WORKINGFOLDER/PUGH/9781107028197HTL.3D [1–2]12.12.20135:22PM ontides,sea-levelchangesandgeodesy,includingco-editingUnderstanding Sea-LevelRiseandVariability(WileyBlackwell,2010),andhasbeeninvolved ineachIPCCresearchassessment.HisawardsincludetheDennyMedalof IMAREST,theVening-MeineszMedaloftheEuropeanGeosciencesUnion, the50thAnniversaryMedaloftheIOC,andaminuteshareinthe2007 NobelPeacePrizeawardedtotheIPCC.HewasawardedanMBEin2011for servicestoscience. iii C:/ITOOLS/WMS/CUP-NEW/4604986/WORKINGFOLDER/PUGH/9781107028197TTL.3D [3–3]12.12.20135:28PM Sea-Level Science Understanding Tides, Surges, Tsunamis and Mean Sea Level David Pugh and Philip Woodworth UniversityofLiverpool iv C:/ITOOLS/WMS/CUP-NEW/4604986/WORKINGFOLDER/PUGH/9781107028197IMP.3D [4–4]12.12.20135:31PM UniversityPrintingHouse,CambridgeCB28BS,UnitedKingdom PublishedintheUnitedStatesofAmericabyCambridgeUniversityPress,NewYork CambridgeUniversityPressispartoftheUniversityofCambridge. ItfurtherstheUniversity’smissionbydisseminatingknowledgeinthepursuitof education,learning,andresearchatthehighestinternationallevelsofexcellence. www.cambridge.org Informationonthistitle:www.cambridge.org/9781107028197 ©DavidPughandPhilipWoodworth2014 Thispublicationisincopyright.Subjecttostatutoryexception andtotheprovisionsofrelevantcollectivelicensingagreements, noreproductionofanypartmaytakeplacewithoutthewritten permissionofCambridgeUniversityPress. FirsteditionpublishedasTides,SurgesandMeanSea-Level:AHandbook forEngineersandScientists,1987,byDavidPugh(WileyBlackwell,all rightsrevertedtoauthor) Secondeditionpublished2014 PrintedandboundintheUnitedKingdomby AcataloguerecordforthispublicationisavailablefromtheBritishLibrary LibraryofCongressCataloguinginPublicationdata ISBN978-1-107-02819-7Hardback CambridgeUniversityPresshasnoresponsibilityforthepersistenceoraccuracyof URLsforexternalorthird-partyinternetwebsitesreferredtointhispublication, anddoesnotguaranteethatanycontentonsuchwebsitesis,orwillremain, accurateorappropriate. v C:/ITOOLS/WMS/CUP-NEW/4609815/WORKINGFOLDER/PUGH/9781107028197TOC.3D [5–6]13.12.20135:18PM Contents Preface pagevii Listofacronyms ix Listofsymbols xi 1 Introduction 1 5.3 Oceantides 105 5.4 Shelftides 111 1.1 Background 1 5.5 Radiationaltides 122 1.2 Earlyideasandobservations 1 5.6 Internaltides 124 1.3 Tidalpatterns 3 5.7 TheyieldingEarth 126 1.4 Meteorologicalandothernon-tidalchanges 7 5.8 Aretideschanging? 129 1.5 Somedefinitionsofcommonterms 8 1.6 Basicstatisticsofsealevelsastimeseries 11 6 Shallow-waterandcoastaltides 133 2 Sea-levelmeasuringsystems 17 6.1 Introduction:someobservations 133 6.2 Hydrodynamicdistortions 133 2.1 Thescienceofmeasurement 17 6.3 Representationbyhigherharmonics 136 2.2 Datumdefinitions 20 6.4 Tidalcurrents 139 2.3 Coastalinstruments 22 6.5 Tidalasymmetry 142 2.4 Open-seagauges 30 6.6 Tidesinrivers 144 2.5 Datareduction 31 6.7 Energybudgets 149 2.6 Datasources 33 7 Stormsurges,meteotsunamisandother 3 Tidalforces 36 meteorologicaleffectsonsealevel 155 3.1 Gravitationalattraction 36 7.1 Introduction 155 3.2 Thetidalforces:afullerdevelopment 40 7.2 Thedepth-averaged(2-D)equations 155 3.3 TheMoon–Earth–Sunsystem 44 7.3 Stormsurges 156 3.4 Tidalpatterns 49 7.4 Statisticsoftidalresiduals 164 3.5 Extremetidalforces 53 7.5 Seiches 165 7.6 Meteotsunamis 170 4 Tidalanalysisandprediction 60 7.7 Waveset-upandsurfbeat 172 4.1 Non-harmonicmethods 61 7.8 Airpressure-relatedchangesofsealevel 4.2 Harmonicanalysis 62 intheworldocean 173 4.3 Responseanalysis 78 8 Tsunamis 189 4.4 Analysisofcurrents 82 4.5 Timezoneconversion 86 8.1 Introduction 189 4.6 Stabilityoftidalparameters 87 8.2 Whytsunamishappen 192 4.7 Tidalpredictions 89 8.3 Tsunamipropagationacross theocean 199 5 Tidaldynamics 97 8.4 Coastalshoalingandrunup 203 5.1 Therealworld 97 8.5 Tsunamisignalsinsea-levelandbottom 5.2 Long-wavecharacteristics 99 pressuredata 206 v vi C:/ITOOLS/WMS/CUP-NEW/4609815/WORKINGFOLDER/PUGH/9781107028197TOC.3D [5–6]13.12.20135:18PM Contents 8.6 Sea-levelandrelatedtechnologiesfor 12 Sea-levelapplications 318 tsunamimonitoring 207 12.1 Designparameters 318 8.7 Tsunamifurtherreading 215 12.2 Extremeconditions 319 9 Sea-levelchangesinspace 223 12.3 Coastaldefences 327 9.1 Introduction 223 12.4 Lagoonsandchannels 329 9.2 TheInternationalTerrestrialReference 12.5 Powergeneration 331 Frame 223 12.6 Emersion–submersionprobabilities 335 9.3 TheGlobalPositioningSystem 224 12.7 Floodwarningsystems 337 9.4 DORIS 227 12.8 Economicsofcoastaldefences 341 9.5 SatellitesandMeanSeaSurface 227 13 Sealevelandlife 345 9.6 Satellitesandthegeoid 233 13.1 Introduction 345 9.7 ModelsoftheMSS,geoid 13.2 TheMoonandus 345 andMDT 240 13.3 Intertidallife 346 9.8 Acommentonepochs 243 13.4 Humandevelopment 351 9.9 Towardsaglobalverticaldatum 243 13.5 Thesea-levelpresent 354 10 Meansea-levelchangesintime 252 13.6 Thesea-levelfuture 355 10.1 Introduction 252 10.2 Sea-leveldata 252 10.3 Mesoscalevariabilityinsealevel 254 AppendixA Basichydrostaticandhydrodynamic 10.4 TheseasonalcycleofMSL 256 equations 361 10.5 Poletide 259 A.1 Thehydrostaticequation 361 10.6 Nodaltide 261 A.2 Conservationofmass 361 10.7 Airpressure-relatedsea-level A.3 Thehorizontalmomentum variability 262 equations 361 10.8 Large-scalepatternsofinterannual AppendixB Currents 363 variability 264 B.1 Analysisofcurrents 363 10.9 Long-termchangesinsealevel 268 B.2 Currentdynamics 365 10.10 Understandingsea-levelchange 276 AppendixC Highandlowwatertimesand 10.11 Futureriseinmeanandextremesea heightsfromharmonic levels 280 constituents 368 11 Sea-levelchangesintimetodowith AppendixD Theoreticaltidaldynamics 370 thesolidEarth 296 D.1 Longprogressivewave,no rotation 370 11.1 Introduction 296 D.2 Standingwaves 372 11.2 Techniquesformeasuringverticalland D.3 Longwavesonarotating movement 296 Earth 373 11.3 GlacialIsostaticAdjustment 301 D.4 Co-tidalandco-amplitude 11.4 Tectonicsea-levelchanges 303 lines 374 11.5 Man-madecrustalmovements 307 AppendixE Legaldefinitionsinthecoastal 11.6 Geophysicalfingerprintsofsea-level zone 376 change 308 Glossary 380 11.7 Coastalprocesses 310 Index 389 vi vii C:/ITOOLS/WMS/CUP-NEW/4604986/WORKINGFOLDER/PUGH/9781107028197PRF.3D [7–8]12.12.20135:38PM Preface Wespendmuchofourtimestudyingsea-levelscience,a spanning Chapters 7 to 11, we review the major new wide-ranging and constantly fascinating subject. We developments insea-levelscience:weathereffects, tsu- analysedata,readandwritepapers,andpresentfindings namis, satellites and geodesy, and global sea-level atconferenceswheretherearepeopleinthesamesea- changes related to climate change. Our discussion of levelcommunityasus.However,everysooftenwegetto the latter can be readalongside the recently published meetotherpeoplewhohavebeenexposedtothissubject FifthAssessmentReportoftheIntergovernmentalPanel in amorepersonalway:someonewholostrelatives in onClimateChange,whichprovidesevenmorefactsand the1953NorthSeastormsurge,anotherwholostevery- figuresonsealevelandclimate. thingmorethanonceinBangladeshfloods,acolleague In the third component, containing the final two whosurvivedthe2004Sumatratsunami. chapters, we discuss more generally how humankind Weremember ataconferenceofsea-levelexperts has been affected by changes in sea level in the past, intheMaldivessomeyearsagoasmallboyholdinga andseekstomakepracticalarrangementsforchanges homemadeposterdeclaring‘Downwithsea-levelrise’, inthefuture.Itisundoubtedlythecasethatchangesin as he feared for the future of his country. Concern sealevelaffectthewayweliveourlivestoday,andthey about possible global warming and sea-level rise has willbecomeincreasinglyimportantinthefuture.Sea- rarelybeenexpressedassimplyoraseffectively.These levelsciencematterstousall. examples remind us that the results of our work are important, not just for the scientific papers that are Acknowledgements produced,but alsofor many practical reasons, which somehowwefindreassuring. Wearegratefulforthehelpofmanyscientificcolleagues Thisbookisanintegratedaccountofsealeveland andfriends,whowerekindenoughtocommentonearly thephysicalreasonswhyitisendlesslychanging:tides, versions of each chapter and provide valuable advice. weather effects, tsunamis, long-term climate change, Particular thanks go to Trevor Baker, John Hunter, and even changes in the solid Earth. The chapters AlexanderRabinovichandRichardRay,whoseexpertise cover many fields: oceanography, geology, geodesy, onoceanandearthtides,sea-levelextremesandtsuna- climatechange,coastalengineering,datamanagement miswassofreelymadeavailabletous. andothers. Several of our colleagues at the National It takes as its starting point David Pugh’s 1987 Oceanography Centre were imposed upon to read Tides, Surges and Mean Sea Level, which is now long draft chapters or advise on others. Special thanks go out of print, and significantly out of date. That book toAngelaHibbert,MiguelAngelMoralesMaqueda,Jo was published at a time of renaissance for sea-level Williams,SimonWilliamsandJudithWolf. science – a rebirth driven by the technology of satel- We have also appreciated specific guidance and lites and ever more powerful computers; and by fun- help from Thorkild Aarup, Yasser Abualnaja, Ole damentalpublicconcernsabouttheeffectsofclimate Andersen, Isabel Goncalves Araújo, Richard Bingley, changeandpotentialincreasedcoastalflooding.These David Blackman, David Cotton, Roland Gehrels, concerns have been reinforced byrecentcatastrophic Jonathan Gregory, Ivan Haigh, Lee Harris, Kevin tsunamiandstormsurgeevents. Horsburgh, John Howarth, Chris Hughes, Paul This new account has roughly three components. Hughes, Antony Joseph, Mark Lawless, David Long, Thefirstcomponentconsistsofsixchaptersthatfollow MarkMerrifield,GlennMilne,AndyPlater,RuiPonte, the1987book’streatmentoftides:instruments,forces, ReinerRummel,MikisTsimplis,JavierValladares,Ian vii analysis and dynamics. In the second component, Vassie, Ric Williams and Chris Wilson. We are also viii C:/ITOOLS/WMS/CUP-NEW/4604986/WORKINGFOLDER/PUGH/9781107028197PRF.3D [7–8]12.12.20135:38PM Preface grateful for help and advice from our colleagues in ones, as we have acknowledged appropriately in the the Permanent Service for Mean Sea Level: Lesley captions. Rickards, Simon Holgate, Svetlana Jevrejeva, Mark RobertSmithandKateDavishaveadvisedonand Tamisiea, Andy Matthews, Kathy Gordon and Liz preparedmanyofthefigures.Weacknowledgetheuse Bradshaw. oftheGenericMappingToolspackageforothers. Other colleagues provided us with top copies of David Pugh thanks the King Abdullah University figuresfromtheirworkorhelpedusfindphotographs. of Science and Technology for their hospitality while Insomecases,thefiguresprovidedwereunpublished sectionsofthisbookwereprepared. viii ix C:/ITOOLS/WMS/CUP-NEW/4604986/WORKINGFOLDER/PUGH/9781107028197MFM01.3D [9–10]12.12.20135:44PM Acronyms ACC AntarcticCircumpolarCurrent GCN GLOSSCoreNetwork ADCP AcousticDopplerCurrent GCOS GlobalClimateObserving Profiler System AMO AtlanticMultidecadalOscillation GEOSS GlobalEarthObservationSystem AMOC AtlanticMeridionalOverturning ofSystems Circulation GEV GeneralisedExtremeValue AO ArcticOscillation GFO GeoSatFollow-onSatellite AOGCM AtmosphereOceanGeneral GGOS GlobalGeodeticObserving CirculationModel System(oftheInternational AR4 IPCCFourthAssessmentReport AssociationofGeodesy) AR5 IPCCFifthAssessmentReport GIA GlacialIsostaticAdjustment BM BenchMark GLONASS GlobalOrbitingNavigation BP BeforePresentorBottom SatelliteSystem Pressure GLOSS GlobalSeaLevelObserving BPR BottomPressureRecorder System(oftheIntergovernmental CGPS ContinuousGPS OceanographicCommission) CM CentreofMass GNSS GlobalNavigationSatellite DART Deep-oceanAssessmentand System ReportingofTsunami GOCE GravityFieldandSteady-State DD DoubleDifferencing(GPSdata OceanCirculationExplorer processingmethod) Satellite DORIS DopplerOrbitographyand GOOS GlobalOceanObservingSystem RadiopositioningIntegratedby GPS GlobalPositioningSystem Satellite GRACE GravityRecoveryandClimate DNA Deoxyribonucleicacid ExperimentSatellite ECDIS ElectronicChartDisplayand GTS GlobalTelecommunications InformationSystem System EGPS EpochalorEpisodicGPS HAT HighestAstronomicalTide EKE EddyKineticEnergy IAG InternationalAssociationof ENSO ElNiño–SouthernOscillation Geodesy Envisat EnvironmentalSatelliteofthe IB InverseBarometer EuropeanSpaceAgency ICESat Ice,CloudandLandElevation EOF EmpiricalOrthogonalFunction Satellite EOP EarthOrientationParameter IERS InternationalEarthRotation ERS-1,-2 EuropeanRemoteSensing Service satellite-1and-2 IGS InternationalGNSSService ESA EuropeanSpaceAgency InSAR InterferometricSynthetic EUMETSAT EuropeanOrganisationforthe ApertureRadar ExploitationofMeteorological IOC Intergovernmental Satellites OceanographicCommission ix FBM FundamentalBenchMark IOD IndianOceanDipole

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