2020
DOI: 10.1038/s41598-020-73132-x
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Revising evidence of hurricane strikes on Abaco Island (The Bahamas) over the last 700 years

Abstract: The northern Bahamas have experienced more frequent intense-hurricane impacts than almost anywhere else in the Atlantic since 1850 CE. In 2019, category 5 (Saffir-Simpson scale) Hurricane Dorian demonstrated the destructive potential of these natural hazards. Problematically, determining whether high hurricane activity levels remained constant through time is difficult given the short observational record (< 170 years). We present a 700-year long, near-annually resolved stratigraphic record of hurricane pas… Show more

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Cited by 36 publications
(77 citation statements)
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“…We determine active and quiet intervals in our pseudo sediment records using established methods (Donnelly et al., 2015; Lane et al., 2011; E. J. Wallace et al., 2019; Winkler et al., 2020) for comparison with the number observed in the South Andros sediment record (Figure ). Active intervals are defined as consecutive years when the 100‐year window event frequency is above an upper confidence limit encompassing the expected random variability of hurricane strikes at a site.…”
Section: Methodsmentioning
confidence: 99%
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“…We determine active and quiet intervals in our pseudo sediment records using established methods (Donnelly et al., 2015; Lane et al., 2011; E. J. Wallace et al., 2019; Winkler et al., 2020) for comparison with the number observed in the South Andros sediment record (Figure ). Active intervals are defined as consecutive years when the 100‐year window event frequency is above an upper confidence limit encompassing the expected random variability of hurricane strikes at a site.…”
Section: Methodsmentioning
confidence: 99%
“…Documenting and dating event beds in sediment cores provides high resolution archives of TC activity at a location over thousands of years. In particular, collecting cores from blue holes in the Caribbean Sea have allowed for near‐annual resolution records extending back over a thousand years (Schmitt et al., 2020; van Hengstum et al., 2014; E. J. Wallace et al., 2019; Winkler et al., 2020). While there is a myriad of different storm properties (e.g., intensity, track, and size) that could influence storm surge at a site, both modern event attribution in these sediment cores (Lane et al., 2011; E. J. Wallace et al., 2019; Winkler et al., 2020) and hydrodynamic modeling of large suites of synthetic TCs passing the sites (Lin et al., 2014) indicate that the vast majority of storms that leave deposits are above some intensity threshold (>Category 2 or 3) and passing proximal (within <100 km) to the site.…”
Section: Introductionmentioning
confidence: 99%
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