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5 results for “Relative Sea-level change”
STEHME files & HOLSEA spreadsheet for "Creel et al. 2022: Postglacial Relative Sea Level Change in Norway" and Balascio et al. 2023: "Refining Holocene sea-level dynamics for the Lofoten and Vesterålen archipelagos, northern Norway: Implications for prehistoric human-environment interactions"
<p><strong>Data Files for Creel et al. 2022: "Postglacial Relative Sea Level Change in Norway" and Balascio et al. 2023: "</strong><strong>Refining Holocene sea-level dynamics for the Lofoten and Vesterålen archipelagos, northern Norway: Implications for prehistoric human-environment interactions"</strong></p> <p>This repository contains the following files:</p> <p>1. Netcdf and csv files for the mean (stehme_mean.nc, stehme_mean_ts.csv) and standard deviation (stehme_std.nc, stehme_std_ts.csv) of the spatiotemporal empirical hierarchical model ensemble (STEHME) produced for Creel et al. 2022. The 'ts' suffix denotes time series for each unique lat/lon site. The netcdf files contain spatial maps at 100 yr resolution.</p> <p>2. mmc1.xlsx, the HOLSEA format Norway data compilation produced for Creel et al. 2022.</p> <p>3. Netcdf and csv files for the mean (stehme_mean_230721.nc, stehme_mean_ts_230721.csv) and standard deviation (stehme_std_230721.nc, stehme_std_ts_230721.csv) of the spatiotemporal empirical hierarchical model ensemble (STEHME) produced for Balascio et al. 2023. The 'ts' suffix denotes time series for each unique lat/lon site. The netcdf files contain spatial maps at 100 yr resolution. </p>
A global analysis of subsidence, relative sea-level change and coastal flood exposure
<p>This repository contains the data and the scripts used to create results, figures and tables in the paper "A global analysis of subsidence, relative sea-level change and coastal flood exposure" by R. Nicholls et al. published in Nature Climate Change (DOI-link to follow).</p>
Middle Holocene relative sea-level changes and vertical tectonic crustal movements on Shikoku Island near the Nankai Trough, Japan
<p>The Philippine Sea plate subducts beneath the Eurasia plate at the Nankai Trough, northwestern Pacific, causing crustal deformation, mega-thrust earthquakes, and tsunami events. Shikoku Island, 150 km northwest of the trough, experiences both coseismic and interseismic deformation. Coastal sediments potentially record vertical crustal movements as relative sea level (RSL) changes. We studied sedimentary facies and microfossil ostracodes in core SKM from southwestern Shikoku Island for evidence of middle Holocene tsunami events and deformation. The core sediments included nine event layers corresponding to storm or tsunami events. Using modern analog techniques, we estimated RSLs from the ostracode assemblages of core SKM and 13 other cores from Shikoku Island and the surrounding region. Then, we subtracted RSL changes due to glacio-hydro isostatic adjustment from the estimated RSLs to estimate vertical tectonic movement rates in these cores between 8.6 and 4.7 ka. The inferred RSL changes suggest that the Sukumo site has experienced both uplift and subsidence since 8.6 ka. Before 6.6 ka, rates of the tectonic crustal movement were higher than the modern-day rate, and its spatial distribution also differed. After 6.6 ka, the tectonic crustal movement showed a similar spatial pattern and occurred at rates close to the modern-day interseismic rate. The spatial pattern and rates of tectonic crustal movement could be caused by changes in rupture areas between Eurasia and the Philippine Sea plates beneath Shikoku Island and in stress conditions of the asthenosphere. Some of the vertical displacements can be explained by the movements of local active faults.</p>
Middle Holocene relative sea-level changes and vertical tectonic crustal movements on Shikoku Island near the Nankai Trough, Japan
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Data from: Did post-glacial sea-level changes initiate the evolutionary divergence of a Tasmanian endemic raptor from its mainland relative?
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