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The effect of temporal wave averaging on the performance of an empirical shoreline evolution model
The effect of using time-averaged wave statistics in a simple empirical model for shoreline change is investigated. The model was first calibrated with a six-year time series of hourly wave conditions and weekly shoreline position at the Gold Coast, Australia. The model was then recalibrated with th...
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Published in: | Coastal engineering (Amsterdam) 2011-08, Vol.58 (8), p.802-805 |
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container_title | Coastal engineering (Amsterdam) |
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creator | Davidson, M.A. Turner, I.L. Guza, R.T. |
description | The effect of using time-averaged wave statistics in a simple empirical model for shoreline change is investigated. The model was first calibrated with a six-year time series of hourly wave conditions and weekly shoreline position at the Gold Coast, Australia. The model was then recalibrated with the hourly waves averaged over intervals up to 1
year. With wave averaging up to 2
days, model performance was approximately constant (squared correlation r
2
~
0.61–0.62), with only small changes in the values of empirical model parameters (e.g. the beach response coefficient
c varied by less than 4%). With between 2 and 40
day averaging, individual storms are not resolved; model skill decreased only modestly (r
2
~
0.55), but
c varied erratically by up to 40% of the original value. That is, optimal model coefficients depend on wave averaging, an undesirable result. With increased averaging (>
40
days) seasonal variability in the wave field is not resolved well and model skill declined markedly. Thus, temporal averaging of wave conditions increases numerical efficiency, but over-averaging degrades model performance and distorts best-fit values of model free parameters. |
doi_str_mv | 10.1016/j.coastaleng.2011.03.007 |
format | article |
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year. With wave averaging up to 2
days, model performance was approximately constant (squared correlation r
2
~
0.61–0.62), with only small changes in the values of empirical model parameters (e.g. the beach response coefficient
c varied by less than 4%). With between 2 and 40
day averaging, individual storms are not resolved; model skill decreased only modestly (r
2
~
0.55), but
c varied erratically by up to 40% of the original value. That is, optimal model coefficients depend on wave averaging, an undesirable result. With increased averaging (>
40
days) seasonal variability in the wave field is not resolved well and model skill declined markedly. Thus, temporal averaging of wave conditions increases numerical efficiency, but over-averaging degrades model performance and distorts best-fit values of model free parameters.</description><identifier>ISSN: 0378-3839</identifier><identifier>EISSN: 1872-7379</identifier><identifier>DOI: 10.1016/j.coastaleng.2011.03.007</identifier><identifier>CODEN: COENDE</identifier><language>eng</language><publisher>Kidlington: Elsevier B.V</publisher><subject>Argus ; Coefficients ; Earth sciences ; Earth, ocean, space ; Empirical analysis ; Exact sciences and technology ; Geomorphology, landform evolution ; Intervals ; Marine and continental quaternary ; Mathematical models ; Prediction ; Shoreline ; Shorelines ; Skills ; Statistics ; Surficial geology ; Temporal logic ; Video ; Wave averaging</subject><ispartof>Coastal engineering (Amsterdam), 2011-08, Vol.58 (8), p.802-805</ispartof><rights>2011 Elsevier B.V.</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a403t-77cdd3bca7ba1f2323451d40dcc551d08961d07e2a63d3ceb5ace02d29b8265e3</citedby><cites>FETCH-LOGICAL-a403t-77cdd3bca7ba1f2323451d40dcc551d08961d07e2a63d3ceb5ace02d29b8265e3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=24289470$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Davidson, M.A.</creatorcontrib><creatorcontrib>Turner, I.L.</creatorcontrib><creatorcontrib>Guza, R.T.</creatorcontrib><title>The effect of temporal wave averaging on the performance of an empirical shoreline evolution model</title><title>Coastal engineering (Amsterdam)</title><description>The effect of using time-averaged wave statistics in a simple empirical model for shoreline change is investigated. The model was first calibrated with a six-year time series of hourly wave conditions and weekly shoreline position at the Gold Coast, Australia. The model was then recalibrated with the hourly waves averaged over intervals up to 1
year. With wave averaging up to 2
days, model performance was approximately constant (squared correlation r
2
~
0.61–0.62), with only small changes in the values of empirical model parameters (e.g. the beach response coefficient
c varied by less than 4%). With between 2 and 40
day averaging, individual storms are not resolved; model skill decreased only modestly (r
2
~
0.55), but
c varied erratically by up to 40% of the original value. That is, optimal model coefficients depend on wave averaging, an undesirable result. With increased averaging (>
40
days) seasonal variability in the wave field is not resolved well and model skill declined markedly. Thus, temporal averaging of wave conditions increases numerical efficiency, but over-averaging degrades model performance and distorts best-fit values of model free parameters.</description><subject>Argus</subject><subject>Coefficients</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Empirical analysis</subject><subject>Exact sciences and technology</subject><subject>Geomorphology, landform evolution</subject><subject>Intervals</subject><subject>Marine and continental quaternary</subject><subject>Mathematical models</subject><subject>Prediction</subject><subject>Shoreline</subject><subject>Shorelines</subject><subject>Skills</subject><subject>Statistics</subject><subject>Surficial geology</subject><subject>Temporal logic</subject><subject>Video</subject><subject>Wave averaging</subject><issn>0378-3839</issn><issn>1872-7379</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><recordid>eNqFkE1LxDAQhoMouH78h1zEU2s-2iY9qvgFghc9hzSZrlnaZk26K_57Z1nRo4FkcnjeGeYhhHJWcsabq1Xpos2zHWBaloJxXjJZMqYOyIJrJQolVXtIFkwqXUgt22NykvOK4Wl0vSDd6ztQ6HtwM409nWFcx2QH-mm3QPEmuwzTksaJzgiuIfUxjXZysKPtRJEPKThM5PeYYAgTttvGYTMHzIzRw3BGjno7ZDj_qafk7f7u9faxeH55eLq9fi5sxeRcKOW8l52zqrO8F1LIqua-Yt65Gj9Mtw2-CoRtpJcOuto6YMKLttOiqUGekst933WKHxvIsxlDdjAMdoK4yUa3La-YEjWSek-6FHNO0Jt1CqNNX4Yzs7NqVubPqtlZNUwatIrRi58hNuPWfUIXIf_mRSV0WymG3M2eA9x4GyCZ7AKgNx8SujY-hv-HfQNH5pRs</recordid><startdate>20110801</startdate><enddate>20110801</enddate><creator>Davidson, M.A.</creator><creator>Turner, I.L.</creator><creator>Guza, R.T.</creator><general>Elsevier B.V</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>20110801</creationdate><title>The effect of temporal wave averaging on the performance of an empirical shoreline evolution model</title><author>Davidson, M.A. ; Turner, I.L. ; Guza, R.T.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a403t-77cdd3bca7ba1f2323451d40dcc551d08961d07e2a63d3ceb5ace02d29b8265e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>Argus</topic><topic>Coefficients</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Empirical analysis</topic><topic>Exact sciences and technology</topic><topic>Geomorphology, landform evolution</topic><topic>Intervals</topic><topic>Marine and continental quaternary</topic><topic>Mathematical models</topic><topic>Prediction</topic><topic>Shoreline</topic><topic>Shorelines</topic><topic>Skills</topic><topic>Statistics</topic><topic>Surficial geology</topic><topic>Temporal logic</topic><topic>Video</topic><topic>Wave averaging</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Davidson, M.A.</creatorcontrib><creatorcontrib>Turner, I.L.</creatorcontrib><creatorcontrib>Guza, R.T.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Coastal engineering (Amsterdam)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Davidson, M.A.</au><au>Turner, I.L.</au><au>Guza, R.T.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The effect of temporal wave averaging on the performance of an empirical shoreline evolution model</atitle><jtitle>Coastal engineering (Amsterdam)</jtitle><date>2011-08-01</date><risdate>2011</risdate><volume>58</volume><issue>8</issue><spage>802</spage><epage>805</epage><pages>802-805</pages><issn>0378-3839</issn><eissn>1872-7379</eissn><coden>COENDE</coden><abstract>The effect of using time-averaged wave statistics in a simple empirical model for shoreline change is investigated. The model was first calibrated with a six-year time series of hourly wave conditions and weekly shoreline position at the Gold Coast, Australia. The model was then recalibrated with the hourly waves averaged over intervals up to 1
year. With wave averaging up to 2
days, model performance was approximately constant (squared correlation r
2
~
0.61–0.62), with only small changes in the values of empirical model parameters (e.g. the beach response coefficient
c varied by less than 4%). With between 2 and 40
day averaging, individual storms are not resolved; model skill decreased only modestly (r
2
~
0.55), but
c varied erratically by up to 40% of the original value. That is, optimal model coefficients depend on wave averaging, an undesirable result. With increased averaging (>
40
days) seasonal variability in the wave field is not resolved well and model skill declined markedly. Thus, temporal averaging of wave conditions increases numerical efficiency, but over-averaging degrades model performance and distorts best-fit values of model free parameters.</abstract><cop>Kidlington</cop><pub>Elsevier B.V</pub><doi>10.1016/j.coastaleng.2011.03.007</doi><tpages>4</tpages></addata></record> |
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subjects | Argus Coefficients Earth sciences Earth, ocean, space Empirical analysis Exact sciences and technology Geomorphology, landform evolution Intervals Marine and continental quaternary Mathematical models Prediction Shoreline Shorelines Skills Statistics Surficial geology Temporal logic Video Wave averaging |
title | The effect of temporal wave averaging on the performance of an empirical shoreline evolution model |
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