2022
DOI: 10.1080/21664250.2022.2088194
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Impacts in ports on a tectonically active coast for climate-driven projections under the RCP 8.5 scenario: 7 Chilean ports under scrutiny

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Cited by 3 publications
(2 citation statements)
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“…Though the relatively low probability of occurrence of these events [51] within the analyzed projection (2026-2045) is minor, they should not be disregarded a priori. Along this line, efforts to combine both coseismic seafloor changes and coastal flooding to compute wave overtopping [31] or to explain the role of such changes in shoreline erosion along the Chilean coasts [52] have already been achieved (note that, similarly to the flood level used herein, wave overtopping and shoreline erosion also depend on the tide, storm surge, waves, and sea level rise). The complex interaction between climate-driven changes in oceanographic variables and those associated to the tectonic nature of subduction zones should be addressed in future studies following, for example, the novel approaches of Sepulveda et al [53,54] in combination with projections of urban growth of cities.…”
Section: Limitations On Th Estimation Of the Flood Hazardmentioning
confidence: 99%
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“…Though the relatively low probability of occurrence of these events [51] within the analyzed projection (2026-2045) is minor, they should not be disregarded a priori. Along this line, efforts to combine both coseismic seafloor changes and coastal flooding to compute wave overtopping [31] or to explain the role of such changes in shoreline erosion along the Chilean coasts [52] have already been achieved (note that, similarly to the flood level used herein, wave overtopping and shoreline erosion also depend on the tide, storm surge, waves, and sea level rise). The complex interaction between climate-driven changes in oceanographic variables and those associated to the tectonic nature of subduction zones should be addressed in future studies following, for example, the novel approaches of Sepulveda et al [53,54] in combination with projections of urban growth of cities.…”
Section: Limitations On Th Estimation Of the Flood Hazardmentioning
confidence: 99%
“…The ocean bottom was modelled with a spatial resolution of 1 • using ETOPO2v2's bathymetry [29] in combination with a coastline from the GHHSGVIII database [30]. Details of the model parametrization are included in [31], and it has shown a good performance off Chile's coasts [32].…”
Section: Computation Of the Flooding Hazardmentioning
confidence: 99%