Resolving the tsunami wave: interpreting palaeotsunami deposits by integrating numerical modelling and sedimentology
The 8.15ka Storegga submarine slide was a large, tsunamigenic slide off the coast of Norway.The resulting tsunami had estimated run-up heights of around 10-20m on the Norwegian coast, over 20m in Shetland, 3-6 metres on the Scottish mainland coast and reached as far as Greenland. Run-up height can b...
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ftdatacite:10.6084/m9.figshare.9771917.v3 2023-05-15T16:29:59+02:00 Resolving the tsunami wave: interpreting palaeotsunami deposits by integrating numerical modelling and sedimentology Hill, Jon 2019 https://dx.doi.org/10.6084/m9.figshare.9771917.v3 https://figshare.com/articles/Resolving_the_tsunami_wave_interpreting_palaeotsunami_deposits_by_integrating_numerical_modelling_and_sedimentology/9771917/3 unknown figshare https://dx.doi.org/10.6084/m9.figshare.9771917 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Physical Geography 40604 Natural Hazards FOS Earth and related environmental sciences 91501 Computational Fluid Dynamics FOS Other engineering and technologies Presentation MediaObject article Audiovisual 2019 ftdatacite https://doi.org/10.6084/m9.figshare.9771917.v3 https://doi.org/10.6084/m9.figshare.9771917 2021-11-05T12:55:41Z The 8.15ka Storegga submarine slide was a large, tsunamigenic slide off the coast of Norway.The resulting tsunami had estimated run-up heights of around 10-20m on the Norwegian coast, over 20m in Shetland, 3-6 metres on the Scottish mainland coast and reached as far as Greenland. Run-up height can beestimated in certain locations via tsunami deposits, but these are not preserved everywhere. Moreover, the estimation of wave height and run-up depend on accurate knowledge of past sea-level. So far numericalmodelling of the wave has focussed on the regional wave, with large scale, low resolution models that donot incorporate inundation and hence can only estimate the wave run up using offshore wave heights. New core data were taken from the Ythan valley in NE Scotland. High resolution sedimentary analysis of these data show signatures of multiple waves. We test this hypothesis by creating a very high resolution model (metre-scale)of the wave inundation, coupled to a previous regional model. The new model uses Thetis, a finite elementshallow water solver that is capable of running on many cores utilising multi-scale resolution. The inundation model confirms that multiple waves did pass over the site. We explore the sensitivity of the model to a number of parameters, such as sea level and coastal geomorphology. Combining sedimentological data with high resolution inundation model is a powerful tool in enhancing the sedimentary record of extreme coastal events. Together, they can help interpret the sedimentary record, extending the history of extreme events and hence improve risk knowledge. Conference Object Greenland DataCite Metadata Store (German National Library of Science and Technology) Greenland Storegga ENVELOPE(18.251,18.251,68.645,68.645) |
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collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
Physical Geography 40604 Natural Hazards FOS Earth and related environmental sciences 91501 Computational Fluid Dynamics FOS Other engineering and technologies |
spellingShingle |
Physical Geography 40604 Natural Hazards FOS Earth and related environmental sciences 91501 Computational Fluid Dynamics FOS Other engineering and technologies Hill, Jon Resolving the tsunami wave: interpreting palaeotsunami deposits by integrating numerical modelling and sedimentology |
topic_facet |
Physical Geography 40604 Natural Hazards FOS Earth and related environmental sciences 91501 Computational Fluid Dynamics FOS Other engineering and technologies |
description |
The 8.15ka Storegga submarine slide was a large, tsunamigenic slide off the coast of Norway.The resulting tsunami had estimated run-up heights of around 10-20m on the Norwegian coast, over 20m in Shetland, 3-6 metres on the Scottish mainland coast and reached as far as Greenland. Run-up height can beestimated in certain locations via tsunami deposits, but these are not preserved everywhere. Moreover, the estimation of wave height and run-up depend on accurate knowledge of past sea-level. So far numericalmodelling of the wave has focussed on the regional wave, with large scale, low resolution models that donot incorporate inundation and hence can only estimate the wave run up using offshore wave heights. New core data were taken from the Ythan valley in NE Scotland. High resolution sedimentary analysis of these data show signatures of multiple waves. We test this hypothesis by creating a very high resolution model (metre-scale)of the wave inundation, coupled to a previous regional model. The new model uses Thetis, a finite elementshallow water solver that is capable of running on many cores utilising multi-scale resolution. The inundation model confirms that multiple waves did pass over the site. We explore the sensitivity of the model to a number of parameters, such as sea level and coastal geomorphology. Combining sedimentological data with high resolution inundation model is a powerful tool in enhancing the sedimentary record of extreme coastal events. Together, they can help interpret the sedimentary record, extending the history of extreme events and hence improve risk knowledge. |
format |
Conference Object |
author |
Hill, Jon |
author_facet |
Hill, Jon |
author_sort |
Hill, Jon |
title |
Resolving the tsunami wave: interpreting palaeotsunami deposits by integrating numerical modelling and sedimentology |
title_short |
Resolving the tsunami wave: interpreting palaeotsunami deposits by integrating numerical modelling and sedimentology |
title_full |
Resolving the tsunami wave: interpreting palaeotsunami deposits by integrating numerical modelling and sedimentology |
title_fullStr |
Resolving the tsunami wave: interpreting palaeotsunami deposits by integrating numerical modelling and sedimentology |
title_full_unstemmed |
Resolving the tsunami wave: interpreting palaeotsunami deposits by integrating numerical modelling and sedimentology |
title_sort |
resolving the tsunami wave: interpreting palaeotsunami deposits by integrating numerical modelling and sedimentology |
publisher |
figshare |
publishDate |
2019 |
url |
https://dx.doi.org/10.6084/m9.figshare.9771917.v3 https://figshare.com/articles/Resolving_the_tsunami_wave_interpreting_palaeotsunami_deposits_by_integrating_numerical_modelling_and_sedimentology/9771917/3 |
long_lat |
ENVELOPE(18.251,18.251,68.645,68.645) |
geographic |
Greenland Storegga |
geographic_facet |
Greenland Storegga |
genre |
Greenland |
genre_facet |
Greenland |
op_relation |
https://dx.doi.org/10.6084/m9.figshare.9771917 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.6084/m9.figshare.9771917.v3 https://doi.org/10.6084/m9.figshare.9771917 |
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1766019698630066176 |