Estimating present day extreme water level exceedance probabilities around the coastline of Australia: tropical cyclone-induced storm surges
The incidence of major storm surges in the last decade have dramatically emphasized the immense destructive capabilities of extreme water level events, particularly when driven by severe tropical cyclones. Given this risk, it is vitally important that the exceedance probabilities of extreme water le...
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Published in | Climate dynamics Vol. 42; no. 1-2; pp. 139 - 157 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Berlin/Heidelberg
Springer Berlin Heidelberg
01.01.2014
Springer Springer Nature B.V |
Subjects | |
Online Access | Get full text |
ISSN | 0930-7575 1432-0894 |
DOI | 10.1007/s00382-012-1653-0 |
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Abstract | The incidence of major storm surges in the last decade have dramatically emphasized the immense destructive capabilities of extreme water level events, particularly when driven by severe tropical cyclones. Given this risk, it is vitally important that the exceedance probabilities of extreme water levels are accurately evaluated to inform risk-based flood and erosion management, engineering and for future land-use planning and to ensure the risk of catastrophic structural failures due to under-design or expensive wastes due to over-design are minimised. Australia has a long history of coastal flooding from tropical cyclones. Using a novel integration of two modeling techniques, this paper provides the first estimates of present day extreme water level exceedance probabilities around the whole coastline of Australia, and the first estimates that combine the influence of astronomical tides, storm surges generated by both extra-tropical and tropical cyclones, and seasonal and inter-annual variations in mean sea level. Initially, an analysis of tide gauge records has been used to assess the characteristics of tropical cyclone-induced surges around Australia. However, given the dearth (temporal and spatial) of information around much of the coastline, and therefore the inability of these gauge records to adequately describe the regional climatology, an observationally based stochastic tropical cyclone model has been developed to synthetically extend the tropical cyclone record to 10,000 years. Wind and pressure fields derived for these synthetically generated events have then been used to drive a hydrodynamic model of the Australian continental shelf region with annual maximum water levels extracted to estimate exceedance probabilities around the coastline. To validate this methodology, selected historic storm surge events have been simulated and resultant storm surges compared with gauge records. Tropical cyclone induced exceedance probabilities have been combined with estimates derived from a 61-year water level hindcast described in a companion paper to give a single estimate of present day extreme water level probabilities around the whole coastline of Australia. Results of this work are freely available to coastal engineers, managers and researchers via a web-based tool (
www.sealevelrise.info
). The described methodology could be applied to other regions of the world, like the US east coast, that are subject to both extra-tropical and tropical cyclones. |
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AbstractList | The incidence of major storm surges in the last decade have dramatically emphasized the immense destructive capabilities of extreme water level events, particularly when driven by severe tropical cyclones. Given this risk, it is vitally important that the exceedance probabilities of extreme water levels are accurately evaluated to inform risk-based flood and erosion management, engineering and for future land-use planning and to ensure the risk of catastrophic structural failures due to under-design or expensive wastes due to over-design are minimised. Australia has a long history of coastal flooding from tropical cyclones. Using a novel integration of two modeling techniques, this paper provides the first estimates of present day extreme water level exceedance probabilities around the whole coastline of Australia, and the first estimates that combine the influence of astronomical tides, storm surges generated by both extra-tropical and tropical cyclones, and seasonal and inter-annual variations in mean sea level. Initially, an analysis of tide gauge records has been used to assess the characteristics of tropical cyclone-induced surges around Australia. However, given the dearth (temporal and spatial) of information around much of the coastline, and therefore the inability of these gauge records to adequately describe the regional climatology, an observationally based stochastic tropical cyclone model has been developed to synthetically extend the tropical cyclone record to 10,000 years. Wind and pressure fields derived for these synthetically generated events have then been used to drive a hydrodynamic model of the Australian continental shelf region with annual maximum water levels extracted to estimate exceedance probabilities around the coastline. To validate this methodology, selected historic storm surge events have been simulated and resultant storm surges compared with gauge records. Tropical cyclone induced exceedance probabilities have been combined with estimates derived from a 61-year water level hindcast described in a companion paper to give a single estimate of present day extreme water level probabilities around the whole coastline of Australia. Results of this work are freely available to coastal engineers, managers and researchers via a web-based tool (
www.sealevelrise.info
). The described methodology could be applied to other regions of the world, like the US east coast, that are subject to both extra-tropical and tropical cyclones. The incidence of major storm surges in the last decade have dramatically emphasized the immense destructive capabilities of extreme water level events, particularly when driven by severe tropical cyclones. Given this risk, it is vitally important that the exceedance probabilities of extreme water levels are accurately evaluated to inform risk-based flood and erosion management, engineering and for future land-use planning and to ensure the risk of catastrophic structural failures due to under-design or expensive wastes due to over-design are minimised. Australia has a long history of coastal flooding from tropical cyclones. Using a novel integration of two modeling techniques, this paper provides the first estimates of present day extreme water level exceedance probabilities around the whole coastline of Australia, and the first estimates that combine the influence of astronomical tides, storm surges generated by both extra-tropical and tropical cyclones, and seasonal and inter-annual variations in mean sea level. Initially, an analysis of tide gauge records has been used to assess the characteristics of tropical cyclone-induced surges around Australia. However, given the dearth (temporal and spatial) of information around much of the coastline, and therefore the inability of these gauge records to adequately describe the regional climatology, an observationally based stochastic tropical cyclone model has been developed to synthetically extend the tropical cyclone record to 10,000 years. Wind and pressure fields derived for these synthetically generated events have then been used to drive a hydrodynamic model of the Australian continental shelf region with annual maximum water levels extracted to estimate exceedance probabilities around the coastline. To validate this methodology, selected historic storm surge events have been simulated and resultant storm surges compared with gauge records. Tropical cyclone induced exceedance probabilities have been combined with estimates derived from a 61-year water level hindcast described in a companion paper to give a single estimate of present day extreme water level probabilities around the whole coastline of Australia. Results of this work are freely available to coastal engineers, managers and researchers via a web-based tool (www.sealevelrise.info). The described methodology could be applied to other regions of the world, like the US east coast, that are subject to both extra-tropical and tropical cyclones. The incidence of major storm surges in the last decade have dramatically emphasized the immense destructive capabilities of extreme water level events, particularly when driven by severe tropical cyclones. Given this risk, it is vitally important that the exceedance probabilities of extreme water levels are accurately evaluated to inform risk-based flood and erosion management, engineering and for future land-use planning and to ensure the risk of catastrophic structural failures due to under-design or expensive wastes due to over-design are minimised. Australia has a long history of coastal flooding from tropical cyclones. Using a novel integration of two modeling techniques, this paper provides the first estimates of present day extreme water level exceedance probabilities around the whole coastline of Australia, and the first estimates that combine the influence of astronomical tides, storm surges generated by both extra-tropical and tropical cyclones, and seasonal and inter-annual variations in mean sea level. Initially, an analysis of tide gauge records has been used to assess the characteristics of tropical cyclone-induced surges around Australia. However, given the dearth (temporal and spatial) of information around much of the coastline, and therefore the inability of these gauge records to adequately describe the regional climatology, an observationally based stochastic tropical cyclone model has been developed to synthetically extend the tropical cyclone record to 10,000 years. Wind and pressure fields derived for these synthetically generated events have then been used to drive a hydrodynamic model of the Australian continental shelf region with annual maximum water levels extracted to estimate exceedance probabilities around the coastline. To validate this methodology, selected historic storm surge events have been simulated and resultant storm surges compared with gauge records. Tropical cyclone induced exceedance probabilities have been combined with estimates derived from a 61-year water level hindcast described in a companion paper to give a single estimate of present day extreme water level probabilities around the whole coastline of Australia. Results of this work are freely available to coastal engineers, managers and researchers via a web-based tool (www.sealevelrise.info). The described methodology could be applied to other regions of the world, like the US east coast, that are subject to both extra-tropical and tropical cyclones.[PUBLICATION ABSTRACT] The incidence of major storm surges in the last decade have dramatically emphasized the immense destructive capabilities of extreme water level events, particularly when driven by severe tropical cyclones. Given this risk, it is vitally important that the exceedance probabilities of extreme water levels are accurately evaluated to inform risk-based flood and erosion management, engineering and for future land-use planning and to ensure the risk of catastrophic structural failures due to under-design or expensive wastes due to over-design are minimised. Australia has a long history of coastal flooding from tropical cyclones. Using a novel integration of two modeling techniques, this paper provides the first estimates of present day extreme water level exceedance probabilities around the whole coastline of Australia, and the first estimates that combine the influence of astronomical tides, storm surges generated by both extra-tropical and tropical cyclones, and seasonal and inter-annual variations in mean sea level. Initially, an analysis of tide gauge records has been used to assess the characteristics of tropical cyclone-induced surges around Australia. However, given the dearth (temporal and spatial) of information around much of the coastline, and therefore the inability of these gauge records to adequately describe the regional climatology, an observationally based stochastic tropical cyclone model has been developed to synthetically extend the tropical cyclone record to 10,000 years. Wind and pressure fields derived for these synthetically generated events have then been used to drive a hydrodynamic model of the Australian continental shelf region with annual maximum water levels extracted to estimate exceedance probabilities around the coastline. To validate this methodology, selected historic storm surge events have been simulated and resultant storm surges compared with gauge records. Tropical cyclone induced exceedance probabilities have been combined with estimates derived from a 61-year water level hindcast described in a companion paper to give a single estimate of present day extreme water level probabilities around the whole coastline of Australia. Results of this work are freely available to coastal engineers, managers and researchers via a web-based tool (www.sealevelrise.info). The described methodology could be applied to other regions of the world, like the US east coast, that are subject to both extra-tropical and tropical cyclones. Keywords Extreme water levels * Storm surges * Tides * Extra-tropical cyclones * Tropical cyclones * Hurricanes * Return levels * Return periods * Australia |
Audience | Academic |
Author | Wijeratne, E. M. S. Pattiaratchi, Charitha B. MacPherson, Leigh R. Mason, Matthew S. Crompton, Ryan P. Haigh, Ivan D. George, Steve |
Author_xml | – sequence: 1 givenname: Ivan D. surname: Haigh fullname: Haigh, Ivan D. organization: Ocean and Earth Science, National Oceanography Centre, University of Southampton, School of Environmental Systems Engineering and UWA Oceans Institute, The University of Western Australia – sequence: 2 givenname: Leigh R. surname: MacPherson fullname: MacPherson, Leigh R. email: leigh.macpherson@uwa.edu.au organization: School of Environmental Systems Engineering and UWA Oceans Institute, The University of Western Australia – sequence: 3 givenname: Matthew S. surname: Mason fullname: Mason, Matthew S. organization: Risk Frontiers, Natural Hazards Research Centre, Macquarie University – sequence: 4 givenname: E. M. S. surname: Wijeratne fullname: Wijeratne, E. M. S. organization: School of Environmental Systems Engineering and UWA Oceans Institute, The University of Western Australia – sequence: 5 givenname: Charitha B. surname: Pattiaratchi fullname: Pattiaratchi, Charitha B. organization: School of Environmental Systems Engineering and UWA Oceans Institute, The University of Western Australia – sequence: 6 givenname: Ryan P. surname: Crompton fullname: Crompton, Ryan P. organization: Risk Frontiers, Natural Hazards Research Centre, Macquarie University – sequence: 7 givenname: Steve surname: George fullname: George, Steve organization: Antarctic Climate and Ecosystems Cooperative Research Centre |
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Issue | 1-2 |
Keywords | Extra-tropical cyclones Tropical cyclones Storm surges Hurricanes Extreme water levels Return levels Australia Tides Return periods Century 21st Extreme event Australasia Forecast model tides coastal zone hurricanes Return period Severe weather Sea surge Tropical cyclone Risk assessment Storm surge Risk management Natural hazards sea level |
Language | English |
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PublicationDate | 2014-01-01 |
PublicationDateYYYYMMDD | 2014-01-01 |
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PublicationDecade | 2010 |
PublicationPlace | Berlin/Heidelberg |
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PublicationSubtitle | Observational, Theoretical and Computational Research on the Climate System |
PublicationTitle | Climate dynamics |
PublicationTitleAbbrev | Clim Dyn |
PublicationYear | 2014 |
Publisher | Springer Berlin Heidelberg Springer Springer Nature B.V |
Publisher_xml | – name: Springer Berlin Heidelberg – name: Springer – name: Springer Nature B.V |
References | McInnes KL, Macadam I, Hubbert GD, O’Grady JG (2011a) An assessment of current and future vulnerability to coastal inundation due to sea level extremes in Victoria, southeast Australia. Int J Clim. doi:10.1002/joc.3405 Harper BA, Holland GJ (1999) An updated parametric model of the tropical cyclone. In: 23rd conference on hurricanes and tropical meteorology, 893–896 Harper BA (ed) (2001) Queensland climate change and community vulnerability to tropical cyclones—ocean hazards assessment stage 1—review of technical requirements. Report prepared by Systems Engineering Australia Pty Ltd in association with James Cook University Marine Modelling Unit, Queensland Government, 375 pp, March 2001 McInnes KL, O’Grady JG, Hemer M, Macadam I, Abbs DJ, White CJ, Bennett JC, Corney SP, Holz GK, Grose MR, Gaynor SM, Bindoff NL (2011b) Climate future for Tasmania: Extreme tide and sea-level events. Technical Report, Antarctic Climate and Ecosystems Corporate Research Centre HardyTAMcConochieJDMasonLBModeling tropical cyclone wave population of the Great Barrier ReefJ Waterway Port Coastal Ocean Eng2003129104113 Seneviratne SI, Nicholls N, Easterling D, Goodess CM, Kanae S, Kossin J, Luo Y, Marengo J, McInnes K, Rahimi M, Reichstein M, Sorteberg A, Vera C, Zhang X (2012) Changes in climate extremes and their impacts on the natural physical environment. In: Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation. Editors: Field CB, Barros V, Stocker TF, Qin D, Dokken DJ, Ebi KL, Mastrandrea MD, Mach KJ, Plattner GK, Allen SK, Tignor M, Midgley PM. A Special Report of Working Groups I and II of the Intergovernmental Panel on Climate Change (IPCC). Cambridge University Press, Cambridge, UK, and New York, NY, USA, pp 109–230 NichollsRJMarinovaNLoweJABrownSVellingaPde GusmaoDHinkelJTolRSJSea-level rise and its possible impacts given a ‘beyond 4°C world’ in the twenty-first centuryPhilos Trans R Soc A Math Phys Eng Sci2011369193416118110.1098/rsta.2010.0291 PughDTChanging sea levels: effects of tides, weather and climate2004Cambridge, United KingdomCambridge University Press280 pp GeorgiouPNDavenportAGVickeryBJDesign wind speeds in regions dominated by tropical cyclonesJ Wind Eng Ind Aerodyn19831313915210.1016/0167-6105(83)90136-8 HolmesJDWind loading of structures2001LondonSpon Press10.4324/9780203301647356 pp EgbertGDErofeevaSEfficient inverse modeling of barotropic ocean tidesJ Atmos Ocean Technol200219218320410.1175/1520-0426(2002)019<0183:EIMOBO>2.0.CO;2 HarperBHardyTMasonLFryarRDevelopments in storm tide modelling and risk assessment in the Australian regionNat Hazards20095122523810.1007/s11069-009-9382-3 WoodworthPLBlackmanDLEvidence for systematic changes in extreme high waters since the mid-1970sJ Clim20041761190119710.1175/1520-0442(2004)017<1190:EFSCIE>2.0.CO;2 KistlerRKalnayECollinsWSahaSWhiteGWoollenJChelliahMEbisuzakiWKanamitsuMKouskyVDoolHJenneRFiorinoMThe NCEP-NCAR 50-year Reanalysis: monthly Means CD ROM and documentationBull Am Meteorol Soc200182224726710.1175/1520-0477(2001)082<0247:TNNYRM>2.3.CO;2 SimiuEScanlanRHWind effects on structures19862New YorkWiley-Interscience HollandGJOn the quality of the Australian tropical cyclone data baseAust Meteorol Mag198129169181 HollandGJAn analytic model of the wind and pressure profiles in hurricanesMon Weather Rev19801081212121810.1175/1520-0493(1980)108<1212:AAMOTW>2.0.CO;2 KaplanJDeMariaMA simple empirical model for predicting the decay of tropical cyclone winds after landfallJ Appl Meteorol1995342499251210.1175/1520-0450(1995)034<2499:ASEMFP>2.0.CO;2 JevrejevaSMooreJCGrinstedAHow will sea level respond to changes in natural and anthropogenic forcings by 2100?Geophys Res Lett2010377L0770310.1029/2010GL042947 Haigh ID, Pattiaratchi C (2010) 21st century changes in extreme sea levels around Western Australia. In: Proceedings of the 17th National Australian Meteorological & Oceanographic Society Conference, Canberra, Australia Haigh ID, Wijeratne EMS, MacPherson LR, Pattiaratchi CB, George S (2013) Estimating present day extreme total water level exceedance probabilities around the coastline of Australia: tides, extra-tropical storm surges and mean sea level. Clim Dyn. doi:10.1007/s00382-012-1652-1 KepertJThe dynamics of boundary layer jets within the tropical cyclone core. Part 1: linear TheoryJ Atmos Sci2001582469248410.1175/1520-0469(2001)058<2469:TDOBLJ>2.0.CO;2 VermeerMRahmstorfSGlobal sea level linked to global temperatureProc Natl Acad Sci20091062152710.1073/pnas.0907765106 McInnesKLWalshKJEHubbertGDBeerTImpact of sea-level rise and storm surges on a coastal communityNat Hazards200330218720710.1023/A:1026118417752 HortonRHerweijerCRosenzweigCLiuJGornitzVRuaneACSea level rise projections for current generation CGCMs based on the semi-empirical methodGeophys Res Lett2008352L0271510.1029/2007GL032486 Cardone VJ, Cox AT, Greenwood JA, Thompson EF (1994) Upgrade of tropical cyclone surface wind field model. Miscellaneous Paper, CERC-94-14, prepared for U.S. Army Corps of Engineers (101 pp) McInnesKLMacadamIHubbertGDO'GradyJDA modelling approach for estimating the frequency of sea level extremes and the impact of climate change in southeast AustraliaNat Hazards2009511153710.1007/s11069-009-9383-2 PawlowiczRBeardsleyBLentzSClassical tidal harmonic analysis including error estimates in MATLAB using T_TIDEComput Geosci200228892993710.1016/S0098-3004(02)00013-4 LoweJAWoodworthPLKnutsonTMcDonaldREMcInnesKWothKVon StorchHWolfJSwailVBernierNGulevSHorsburghKUnnikrishnanASHunterJWeisseRChurchJAWoodworthPLAarupTWilsonSPast and future changes in extreme water levels and wavesUnderstanding sea-level rise and variability2010OxfordWiley-Blackwell McConochieJDHardyTAMasonLBModelling tropical cyclone over-water wind and pressure fieldsOcean Eng2004311757178210.1016/j.oceaneng.2004.03.009 Danish Hydraulic Institute (2013) Mike 21 & Mike 3 flow model FM. Hydrodynamic and transport module scientific documentation. http://www.dhisoftware.com/Download/DocumentsAndTools/~/media/Microsite_MIKEbyDHI/Publications/PDF/Short%20descriptions/MIKE213_FM_HD_Short_Description.ashx NottJHayneMHow high was the storm surge from tropical cyclone MahinaAust J Emerg Manag2000151113 HaighIDNichollsRJWellsNCRising sea levels in the english channel 1900–2100Proc ICE Marit Eng20111642819210.1680/maen.2011.164.2.81 Meehl GA, Stocker TF, Collins WD, Friedlingstein P, Gaye AT, Gregory JM, Kitoh A, Knutti R, Murphy JM, Noda A, Raper SCB, Watterson IG, Weaver AJ, Zhao ZC (2007) Global climate projections. In: Solomon S, Qin D, Manning M, Chen Z, Marquis M, Averyt KB, Tignor M, Miller HL (eds) Climate change 2007: The physical science basis. Contribution of working group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, pp 747–845 Colberg F, McInnes KL (2012) The impact of storminess changes on extreme sea levels over southern Australia. JGR-Oceans, doi:10.1029/2012JC007919. EliotMPattiaratchiCRemote forcing of water levels by tropical cyclones in southwest AustraliaCont Shelf Res201030141549156110.1016/j.csr.2010.06.002 McConochie JD, Mason LB, Hardy TA (1999) A Coral Sea cyclone wind model intended for wave modelling. In: Proceedings of 14th conference on coastal and ocean engineering, IEAust, Perth, pp 413–418 Hunter J (2011) A simple technique for estimating an allowance for uncertain sea-level rise. Clim Change. doi:10.1007/s10584-011-0332-1 UhlhornEWBlackPGFranklinJLGoodberletMCarswellJGoldsteinASHurricane surface wind measurements from an operational stepped frequency microwave radiometerMon Weather Rev20071353070308510.1175/MWR3454.1 ColesSAn introduction to statistical modelling of extreme values2001BerlinSpringer10.1007/978-1-4471-3675-0207 pp MenéndezMWoodworthPLChanges in extreme high water levels based on a quasi-global tide-gauge datasetJ Geophys Res2010115C10C1001110.1029/2009JC005997 Bindoff NL, Willebrand J, Artale V, Cazenave A, Gregory J, Gulev S, Hanawa K, Le Quéré C, Levitus S, Nojiri Y, Shum CK, Talley LD, Unnikrishnan A (2007) Observations: Oceanic climate change and sea level. In: Climate change 2007: the physical science basis. In: Solomon S, Qin D, Manning M, Chen Z, Marquis M, Averyt KB, Tignor M, Miller HL (eds) Contribution of working group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, pp 385–432 JamesMKMasonLBSynthetic tropical cyclone databaseJ Waterw Port Coastal Ocean Eng2005131418119210.1061/(ASCE)0733-950X(2005)131:4(181) RahmstorfSA semi-empirical approach to projecting future sea-level riseScience2007315581036837010.1126/science.1135456 ChurchJAGregoryJMWhiteNJPlattenSMMitrovicaJXUnderstanding and projecting sea level changeOceanography (J Oceanogr Soc)201124213014310.5670/oceanog.2011.33 HunterJEstimating sea-level extremes under conditions of uncertain sea-level riseClim Change201099333135010.1007/s10584-009-9671-6 HorsburghKLWilsonCTide-surge interaction and its role in the distribution of surge residuals in the North SeaJ Geophys Res2007112CO800310.1029/2006JC004033 O’GradyJGMcInnesKLExtreme wind waves and their relationship to storm surges in northeastern Bass StraitAust Meteorol Oceanogr J201060265275 GrinstedAMooreJCJevrejevaSReconstructing sea level from paleo and projected temperatures 200–2100 adClim Dyn201034446147210.1007/s00382-008-0507-2 VickeryPJSkerljPFTwisdaleLASimulation of hurricane risk in the U.S. using empirical track modelJ Struct Eng20001261012221237 HarperBAStroudSAMcCormackMWestSA review of historical tropical cyclone intensity in northwestern Australia and implications for climate change trend analysisAust Meteorol Mag200857121141 M Eliot (1653_CR9) 2010; 30 R Pawlowicz (1653_CR45) 2002; 28 J Hunter (1653_CR25) 2010; 99 R Horton (1653_CR24) 2008; 35 KL McInnes (1653_CR37) 2009; 51 1653_CR26 R Kistler (1653_CR31) 2001; 82 DT Pugh (1653_CR46) 2004 S Jevrejeva (1653_CR28) 2010; 37 A Grinsted (1653_CR11) 2010; 34 J Kepert (1653_CR30) 2001; 58 GJ Holland (1653_CR21) 1981; 29 PL Woodworth (1653_CR53) 2004; 17 1653_CR12 1653_CR13 KL McInnes (1653_CR36) 2003; 30 1653_CR15 1653_CR52 ID Haigh (1653_CR14) 2011; 164 J Kaplan (1653_CR29) 1995; 34 RJ Nicholls (1653_CR42) 2011; 369 1653_CR16 1653_CR17 MK James (1653_CR27) 2005; 131 J Nott (1653_CR43) 2000; 15 1653_CR40 B Harper (1653_CR19) 2009; 51 BA Harper (1653_CR18) 2008; 57 GJ Holland (1653_CR20) 1980; 108 JD McConochie (1653_CR35) 2004; 31 1653_CR48 E Simiu (1653_CR49) 1986 M Menéndez (1653_CR41) 2010; 115 S Rahmstorf (1653_CR47) 2007; 315 S Coles (1653_CR6) 2001 KL Horsburgh (1653_CR23) 2007; 112 1653_CR34 EW Uhlhorn (1653_CR50) 2007; 135 PN Georgiou (1653_CR10) 1983; 13 JD Holmes (1653_CR22) 2001 JG O’Grady (1653_CR44) 2010; 60 JA Lowe (1653_CR32) 2010 1653_CR2 1653_CR1 JA Church (1653_CR4) 2011; 24 1653_CR38 1653_CR39 M Vermeer (1653_CR51) 2009; 106 1653_CR7 GD Egbert (1653_CR8) 2002; 19 1653_CR5 |
References_xml | – reference: McInnes KL, Macadam I, Hubbert GD, O’Grady JG (2011a) An assessment of current and future vulnerability to coastal inundation due to sea level extremes in Victoria, southeast Australia. Int J Clim. doi:10.1002/joc.3405 – reference: JamesMKMasonLBSynthetic tropical cyclone databaseJ Waterw Port Coastal Ocean Eng2005131418119210.1061/(ASCE)0733-950X(2005)131:4(181) – reference: HorsburghKLWilsonCTide-surge interaction and its role in the distribution of surge residuals in the North SeaJ Geophys Res2007112CO800310.1029/2006JC004033 – reference: ColesSAn introduction to statistical modelling of extreme values2001BerlinSpringer10.1007/978-1-4471-3675-0207 pp – reference: GeorgiouPNDavenportAGVickeryBJDesign wind speeds in regions dominated by tropical cyclonesJ Wind Eng Ind Aerodyn19831313915210.1016/0167-6105(83)90136-8 – reference: HollandGJAn analytic model of the wind and pressure profiles in hurricanesMon Weather Rev19801081212121810.1175/1520-0493(1980)108<1212:AAMOTW>2.0.CO;2 – reference: PughDTChanging sea levels: effects of tides, weather and climate2004Cambridge, United KingdomCambridge University Press280 pp – reference: HarperBHardyTMasonLFryarRDevelopments in storm tide modelling and risk assessment in the Australian regionNat Hazards20095122523810.1007/s11069-009-9382-3 – reference: SimiuEScanlanRHWind effects on structures19862New YorkWiley-Interscience – reference: VickeryPJSkerljPFTwisdaleLASimulation of hurricane risk in the U.S. using empirical track modelJ Struct Eng20001261012221237 – reference: McConochieJDHardyTAMasonLBModelling tropical cyclone over-water wind and pressure fieldsOcean Eng2004311757178210.1016/j.oceaneng.2004.03.009 – reference: KistlerRKalnayECollinsWSahaSWhiteGWoollenJChelliahMEbisuzakiWKanamitsuMKouskyVDoolHJenneRFiorinoMThe NCEP-NCAR 50-year Reanalysis: monthly Means CD ROM and documentationBull Am Meteorol Soc200182224726710.1175/1520-0477(2001)082<0247:TNNYRM>2.3.CO;2 – reference: NottJHayneMHow high was the storm surge from tropical cyclone MahinaAust J Emerg Manag2000151113 – reference: NichollsRJMarinovaNLoweJABrownSVellingaPde GusmaoDHinkelJTolRSJSea-level rise and its possible impacts given a ‘beyond 4°C world’ in the twenty-first centuryPhilos Trans R Soc A Math Phys Eng Sci2011369193416118110.1098/rsta.2010.0291 – reference: ChurchJAGregoryJMWhiteNJPlattenSMMitrovicaJXUnderstanding and projecting sea level changeOceanography (J Oceanogr Soc)201124213014310.5670/oceanog.2011.33 – reference: EgbertGDErofeevaSEfficient inverse modeling of barotropic ocean tidesJ Atmos Ocean Technol200219218320410.1175/1520-0426(2002)019<0183:EIMOBO>2.0.CO;2 – reference: HortonRHerweijerCRosenzweigCLiuJGornitzVRuaneACSea level rise projections for current generation CGCMs based on the semi-empirical methodGeophys Res Lett2008352L0271510.1029/2007GL032486 – reference: Bindoff NL, Willebrand J, Artale V, Cazenave A, Gregory J, Gulev S, Hanawa K, Le Quéré C, Levitus S, Nojiri Y, Shum CK, Talley LD, Unnikrishnan A (2007) Observations: Oceanic climate change and sea level. In: Climate change 2007: the physical science basis. In: Solomon S, Qin D, Manning M, Chen Z, Marquis M, Averyt KB, Tignor M, Miller HL (eds) Contribution of working group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, pp 385–432 – reference: Harper BA, Holland GJ (1999) An updated parametric model of the tropical cyclone. In: 23rd conference on hurricanes and tropical meteorology, 893–896 – reference: Meehl GA, Stocker TF, Collins WD, Friedlingstein P, Gaye AT, Gregory JM, Kitoh A, Knutti R, Murphy JM, Noda A, Raper SCB, Watterson IG, Weaver AJ, Zhao ZC (2007) Global climate projections. In: Solomon S, Qin D, Manning M, Chen Z, Marquis M, Averyt KB, Tignor M, Miller HL (eds) Climate change 2007: The physical science basis. Contribution of working group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, pp 747–845 – reference: VermeerMRahmstorfSGlobal sea level linked to global temperatureProc Natl Acad Sci20091062152710.1073/pnas.0907765106 – reference: O’GradyJGMcInnesKLExtreme wind waves and their relationship to storm surges in northeastern Bass StraitAust Meteorol Oceanogr J201060265275 – reference: HaighIDNichollsRJWellsNCRising sea levels in the english channel 1900–2100Proc ICE Marit Eng20111642819210.1680/maen.2011.164.2.81 – reference: HolmesJDWind loading of structures2001LondonSpon Press10.4324/9780203301647356 pp – reference: KaplanJDeMariaMA simple empirical model for predicting the decay of tropical cyclone winds after landfallJ Appl Meteorol1995342499251210.1175/1520-0450(1995)034<2499:ASEMFP>2.0.CO;2 – reference: Harper BA (ed) (2001) Queensland climate change and community vulnerability to tropical cyclones—ocean hazards assessment stage 1—review of technical requirements. Report prepared by Systems Engineering Australia Pty Ltd in association with James Cook University Marine Modelling Unit, Queensland Government, 375 pp, March 2001 – reference: RahmstorfSA semi-empirical approach to projecting future sea-level riseScience2007315581036837010.1126/science.1135456 – reference: McInnesKLMacadamIHubbertGDO'GradyJDA modelling approach for estimating the frequency of sea level extremes and the impact of climate change in southeast AustraliaNat Hazards2009511153710.1007/s11069-009-9383-2 – reference: Cardone VJ, Cox AT, Greenwood JA, Thompson EF (1994) Upgrade of tropical cyclone surface wind field model. Miscellaneous Paper, CERC-94-14, prepared for U.S. Army Corps of Engineers (101 pp) – reference: WoodworthPLBlackmanDLEvidence for systematic changes in extreme high waters since the mid-1970sJ Clim20041761190119710.1175/1520-0442(2004)017<1190:EFSCIE>2.0.CO;2 – reference: Danish Hydraulic Institute (2013) Mike 21 & Mike 3 flow model FM. Hydrodynamic and transport module scientific documentation. http://www.dhisoftware.com/Download/DocumentsAndTools/~/media/Microsite_MIKEbyDHI/Publications/PDF/Short%20descriptions/MIKE213_FM_HD_Short_Description.ashx – reference: Haigh ID, Pattiaratchi C (2010) 21st century changes in extreme sea levels around Western Australia. In: Proceedings of the 17th National Australian Meteorological & Oceanographic Society Conference, Canberra, Australia – reference: KepertJThe dynamics of boundary layer jets within the tropical cyclone core. Part 1: linear TheoryJ Atmos Sci2001582469248410.1175/1520-0469(2001)058<2469:TDOBLJ>2.0.CO;2 – reference: McInnes KL, O’Grady JG, Hemer M, Macadam I, Abbs DJ, White CJ, Bennett JC, Corney SP, Holz GK, Grose MR, Gaynor SM, Bindoff NL (2011b) Climate future for Tasmania: Extreme tide and sea-level events. Technical Report, Antarctic Climate and Ecosystems Corporate Research Centre – reference: PawlowiczRBeardsleyBLentzSClassical tidal harmonic analysis including error estimates in MATLAB using T_TIDEComput Geosci200228892993710.1016/S0098-3004(02)00013-4 – reference: Hunter J (2011) A simple technique for estimating an allowance for uncertain sea-level rise. Clim Change. doi:10.1007/s10584-011-0332-1 – reference: HunterJEstimating sea-level extremes under conditions of uncertain sea-level riseClim Change201099333135010.1007/s10584-009-9671-6 – reference: UhlhornEWBlackPGFranklinJLGoodberletMCarswellJGoldsteinASHurricane surface wind measurements from an operational stepped frequency microwave radiometerMon Weather Rev20071353070308510.1175/MWR3454.1 – reference: HollandGJOn the quality of the Australian tropical cyclone data baseAust Meteorol Mag198129169181 – reference: LoweJAWoodworthPLKnutsonTMcDonaldREMcInnesKWothKVon StorchHWolfJSwailVBernierNGulevSHorsburghKUnnikrishnanASHunterJWeisseRChurchJAWoodworthPLAarupTWilsonSPast and future changes in extreme water levels and wavesUnderstanding sea-level rise and variability2010OxfordWiley-Blackwell – reference: HarperBAStroudSAMcCormackMWestSA review of historical tropical cyclone intensity in northwestern Australia and implications for climate change trend analysisAust Meteorol Mag200857121141 – reference: Seneviratne SI, Nicholls N, Easterling D, Goodess CM, Kanae S, Kossin J, Luo Y, Marengo J, McInnes K, Rahimi M, Reichstein M, Sorteberg A, Vera C, Zhang X (2012) Changes in climate extremes and their impacts on the natural physical environment. In: Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation. Editors: Field CB, Barros V, Stocker TF, Qin D, Dokken DJ, Ebi KL, Mastrandrea MD, Mach KJ, Plattner GK, Allen SK, Tignor M, Midgley PM. A Special Report of Working Groups I and II of the Intergovernmental Panel on Climate Change (IPCC). Cambridge University Press, Cambridge, UK, and New York, NY, USA, pp 109–230 – reference: MenéndezMWoodworthPLChanges in extreme high water levels based on a quasi-global tide-gauge datasetJ Geophys Res2010115C10C1001110.1029/2009JC005997 – reference: Colberg F, McInnes KL (2012) The impact of storminess changes on extreme sea levels over southern Australia. JGR-Oceans, doi:10.1029/2012JC007919. – reference: Haigh ID, Wijeratne EMS, MacPherson LR, Pattiaratchi CB, George S (2013) Estimating present day extreme total water level exceedance probabilities around the coastline of Australia: tides, extra-tropical storm surges and mean sea level. Clim Dyn. doi:10.1007/s00382-012-1652-1 – reference: HardyTAMcConochieJDMasonLBModeling tropical cyclone wave population of the Great Barrier ReefJ Waterway Port Coastal Ocean Eng2003129104113 – reference: JevrejevaSMooreJCGrinstedAHow will sea level respond to changes in natural and anthropogenic forcings by 2100?Geophys Res Lett2010377L0770310.1029/2010GL042947 – reference: McInnesKLWalshKJEHubbertGDBeerTImpact of sea-level rise and storm surges on a coastal communityNat Hazards200330218720710.1023/A:1026118417752 – reference: GrinstedAMooreJCJevrejevaSReconstructing sea level from paleo and projected temperatures 200–2100 adClim Dyn201034446147210.1007/s00382-008-0507-2 – reference: EliotMPattiaratchiCRemote forcing of water levels by tropical cyclones in southwest AustraliaCont Shelf Res201030141549156110.1016/j.csr.2010.06.002 – reference: McConochie JD, Mason LB, Hardy TA (1999) A Coral Sea cyclone wind model intended for wave modelling. 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SubjectTerms | Annual variations Australia climate Climatology coasts continental shelf Continental shelves Cyclones Earth and Environmental Science Earth Sciences Earth, ocean, space engineering Engineering and environment geology. Geothermics engineers Environment Environmental aspects Exact sciences and technology External geophysics Fluid mechanics Geophysics/Geodesy Hurricanes Hydrodynamics Hydrofoil boats Internet land use Land use planning managers Meteorology Natural hazards: prediction, damages, etc Oceanography Physics of the oceans planning researchers risk Sea level Storm surges Storms Surface waves, tides and sea level. Seiches Tidal analysis Tidal waves tides Tropical cyclones United States wastes Water levels |
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Title | Estimating present day extreme water level exceedance probabilities around the coastline of Australia: tropical cyclone-induced storm surges |
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