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Research output: Contribution in Book/Report/Proceedings - With ISBN/ISSN › Conference contribution/Paper
Research output: Contribution in Book/Report/Proceedings - With ISBN/ISSN › Conference contribution/Paper
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TY - GEN
T1 - Estimation of environmental contours using a block resampling method
AU - Mackay, Ed B.L.
AU - Jonathan, Philip
N1 - Funding Information: We thank Andreas Haselsteiner for productive discussions that motivated this work. EM was funded under the Engineering and Physical Sciences Research Council (EPSRC) grant EP/R007519/1 and as part of the Tidal Stream Industry Energiser Project (TIGER), which has received funding from the European Union’s INTERREG V A France (Channel) England Research and Innovation Programme, which is co-financed by the European Regional Development Fund (ERDF). Funding Information: We thank Andreas Haselsteiner for productive discussions that motivated this work. EM was funded under the Engineering and Physical Sciences Research Council (EPSRC) grant EP/R007519/1 and as part of the Tidal Stream Industry Energiser Project (TIGER), which has received funding from the European Union's INTERREG V A France (Channel) England Research and Innovation Programme, which is co-financed by the European Regional Development Fund (ERDF). Publisher Copyright: © 2020 ASME Copyright: Copyright 2021 Elsevier B.V., All rights reserved.
PY - 2020/8/7
Y1 - 2020/8/7
N2 - A new method for estimating joint distributions of environmental variables is presented. The key difference to previous methods is that the joint distribution of only storm-peak parameters is modelled, rather than fitting a model to all observations. This provides a stronger justification for the use of asymptotic extreme value models, as the data considered are approximately independent. The joint distribution of all data is recovered by resampling and rescaling storm histories, conditional on the peak values. This simplifies the analysis as much of the complex dependence structure is resampled, rather than modelled explicitly. The storm histories are defined by splitting the time series into discrete blocks, with the dividing points defined as the minimum value of a variable between adjacent maxima. Storms are characterised in terms of the peak values of each parameter within each discrete block, which need not coincide in time. The key assumption is that rescaling a measured storm history results in an equally realistic time series, provided that the change in peak values is not large. Two examples of bivariate distribution are considered: the joint distribution of significant wave height (Hs) and zero up-crossing period (Tz) and the joint distribution of Hs and wind speed. It is shown that the storm resampling method gives estimates of environmental contours that agree well with the observations and provides a rigorous method for estimating extreme values.
AB - A new method for estimating joint distributions of environmental variables is presented. The key difference to previous methods is that the joint distribution of only storm-peak parameters is modelled, rather than fitting a model to all observations. This provides a stronger justification for the use of asymptotic extreme value models, as the data considered are approximately independent. The joint distribution of all data is recovered by resampling and rescaling storm histories, conditional on the peak values. This simplifies the analysis as much of the complex dependence structure is resampled, rather than modelled explicitly. The storm histories are defined by splitting the time series into discrete blocks, with the dividing points defined as the minimum value of a variable between adjacent maxima. Storms are characterised in terms of the peak values of each parameter within each discrete block, which need not coincide in time. The key assumption is that rescaling a measured storm history results in an equally realistic time series, provided that the change in peak values is not large. Two examples of bivariate distribution are considered: the joint distribution of significant wave height (Hs) and zero up-crossing period (Tz) and the joint distribution of Hs and wind speed. It is shown that the storm resampling method gives estimates of environmental contours that agree well with the observations and provides a rigorous method for estimating extreme values.
KW - Extremes
KW - Joint distribution
KW - Metocean
M3 - Conference contribution/Paper
AN - SCOPUS:85098580139
T3 - Proceedings of the International Conference on Offshore Mechanics and Arctic Engineering - OMAE
BT - Structures, Safety, and Reliability
PB - American Society of Mechanical Engineers (ASME)
T2 - ASME 2020 39th International Conference on Ocean, Offshore and Arctic Engineering, OMAE 2020
Y2 - 3 August 2020 through 7 August 2020
ER -