The June 2016 Australian East Coast Low: Importance of Wave Direction for Coastal Erosion Assessment

In June 2016, an unusual East Coast Low storm affected some 2000 km of the eastern seaboard of Australia bringing heavy rain, strong winds and powerful wave conditions. While wave heights offshore of Sydney were not exceptional, nearshore wave conditions were such that beaches experienced some of th...

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Main Authors: Thomas R. Mortlock, Ian D. Goodwin, John K. McAneney, Kevin Roche
Format: Article
Language:English
Published: MDPI AG 2017-02-01
Series:Water
Subjects:
Online Access:http://www.mdpi.com/2073-4441/9/2/121
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spelling doaj-0f5e467f577d4c23b653afa4ebf863472020-11-25T00:04:51ZengMDPI AGWater2073-44412017-02-019212110.3390/w9020121w9020121The June 2016 Australian East Coast Low: Importance of Wave Direction for Coastal Erosion AssessmentThomas R. Mortlock0Ian D. Goodwin1John K. McAneney2Kevin Roche3Risk Frontiers, Macquarie University, North Ryde, NSW 2109, AustraliaMarine Climate Risk Group, Department of Environmental Sciences, Macquarie University, North Ryde, NSW 2109, AustraliaRisk Frontiers, Macquarie University, North Ryde, NSW 2109, AustraliaRisk Frontiers, Macquarie University, North Ryde, NSW 2109, AustraliaIn June 2016, an unusual East Coast Low storm affected some 2000 km of the eastern seaboard of Australia bringing heavy rain, strong winds and powerful wave conditions. While wave heights offshore of Sydney were not exceptional, nearshore wave conditions were such that beaches experienced some of the worst erosion in 40 years. Hydrodynamic modelling of wave and current behaviour as well as contemporaneous sand transport shows the east to north-east storm wave direction to be the major determinant of erosion magnitude. This arises because of reduced energy attenuation across the continental shelf and the focussing of wave energy on coastal sections not equilibrated with such wave exposure under the prevailing south-easterly wave climate. Narrabeen–Collaroy, a well-known erosion hot spot on Sydney’s Northern Beaches, is shown to be particularly vulnerable to storms from this direction because the destructive erosion potential is amplified by the influence of the local embayment geometry. We demonstrate the magnified erosion response that occurs when there is bi-directionality between an extreme wave event and preceding modal conditions and the importance of considering wave direction in extreme value analyses.http://www.mdpi.com/2073-4441/9/2/121East Coast Lownearshore processescoastal erosioncoastal managementclimate changenumerical modellingSoutheast Australia
collection DOAJ
language English
format Article
sources DOAJ
author Thomas R. Mortlock
Ian D. Goodwin
John K. McAneney
Kevin Roche
spellingShingle Thomas R. Mortlock
Ian D. Goodwin
John K. McAneney
Kevin Roche
The June 2016 Australian East Coast Low: Importance of Wave Direction for Coastal Erosion Assessment
Water
East Coast Low
nearshore processes
coastal erosion
coastal management
climate change
numerical modelling
Southeast Australia
author_facet Thomas R. Mortlock
Ian D. Goodwin
John K. McAneney
Kevin Roche
author_sort Thomas R. Mortlock
title The June 2016 Australian East Coast Low: Importance of Wave Direction for Coastal Erosion Assessment
title_short The June 2016 Australian East Coast Low: Importance of Wave Direction for Coastal Erosion Assessment
title_full The June 2016 Australian East Coast Low: Importance of Wave Direction for Coastal Erosion Assessment
title_fullStr The June 2016 Australian East Coast Low: Importance of Wave Direction for Coastal Erosion Assessment
title_full_unstemmed The June 2016 Australian East Coast Low: Importance of Wave Direction for Coastal Erosion Assessment
title_sort june 2016 australian east coast low: importance of wave direction for coastal erosion assessment
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2017-02-01
description In June 2016, an unusual East Coast Low storm affected some 2000 km of the eastern seaboard of Australia bringing heavy rain, strong winds and powerful wave conditions. While wave heights offshore of Sydney were not exceptional, nearshore wave conditions were such that beaches experienced some of the worst erosion in 40 years. Hydrodynamic modelling of wave and current behaviour as well as contemporaneous sand transport shows the east to north-east storm wave direction to be the major determinant of erosion magnitude. This arises because of reduced energy attenuation across the continental shelf and the focussing of wave energy on coastal sections not equilibrated with such wave exposure under the prevailing south-easterly wave climate. Narrabeen–Collaroy, a well-known erosion hot spot on Sydney’s Northern Beaches, is shown to be particularly vulnerable to storms from this direction because the destructive erosion potential is amplified by the influence of the local embayment geometry. We demonstrate the magnified erosion response that occurs when there is bi-directionality between an extreme wave event and preceding modal conditions and the importance of considering wave direction in extreme value analyses.
topic East Coast Low
nearshore processes
coastal erosion
coastal management
climate change
numerical modelling
Southeast Australia
url http://www.mdpi.com/2073-4441/9/2/121
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