2019
DOI: 10.1016/j.margeo.2019.105971
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Bimodal climate control of shoreline change influenced by Interdecadal Pacific Oscillation variability along the Cooloola Sand Mass, Queensland, Australia

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Cited by 18 publications
(19 citation statements)
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“…To evaluate how sub-pixel waterline extraction performs when the optimal value of the threshold is not known in advance, we also compared performance using two more realistic threshold selection strategies. The simplest 'zero' threshold scenario applied a consistent threshold of zero to all environments and metrics, in an approach which has been widely used in waterline extraction analyses [7,22,64]. Our results indicate a uniform zero threshold was unable to consistently reproduce the absolute reference waterline position across the five contrasting environments or three water indices we assessed.…”
Section: Effect Of Water Index Thresholdmentioning
confidence: 88%
“…To evaluate how sub-pixel waterline extraction performs when the optimal value of the threshold is not known in advance, we also compared performance using two more realistic threshold selection strategies. The simplest 'zero' threshold scenario applied a consistent threshold of zero to all environments and metrics, in an approach which has been widely used in waterline extraction analyses [7,22,64]. Our results indicate a uniform zero threshold was unable to consistently reproduce the absolute reference waterline position across the five contrasting environments or three water indices we assessed.…”
Section: Effect Of Water Index Thresholdmentioning
confidence: 88%
“…However, their study did not include any pre-and post-storm imagery; thus, erosive episodes could not be linked to specific events. Kelly et al (2019) expanded their work with Landsat imagery over 25 years and showed that long-term shoreline change at the Cooloola Sand Mass is controlled by variability in the Interdecadal Pacific Oscillation (IPO). However, Landsat imagery does not have high spatial resolution; thus, the affects of individual storms also could not be discerned, unless the event resulted in shoreline migration of more than~15 m. Other documented shoreline changes occurring in response to large-scale storm events not only include erosion and progradation, but washover fan development (May et al, 2017;Williams, 2015) and new inlet formation (FitzGerald and Pendleton, 2002;Maio et al, 2014).…”
Section: History Of Cyclonesmentioning
confidence: 99%
“…interact and influence a seasonal wave climate that is highly variable with respect to wave heights and direction (Hemer, McInnes, and Ranasinghe, 2013). Recent work has shown that long-term CSM shoreline dynamics are predominantly controlled by IPO phase variability (Kelly et al, 2019).…”
Section: Study Sitementioning
confidence: 99%
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