Tsunamis due to ice masses: Different calving mechanisms and linkage to landslide-tsunamis - Dataset

Land ice melt and retreat is one of the most visible effects of climate change and contributes ≈1.5 mm/year to global sea-level rise (SLR) of a total of ≈2.7 mm/year. Global warming results in the shrinking of ice masses in most ice covered regions in the World, particularly in the Alps and in Green...

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Main Author: Valentin, Heller
Format: Dataset
Language:unknown
Published: Zenodo 2019
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.2554184
https://zenodo.org/record/2554184
id ftdatacite:10.5281/zenodo.2554184
record_format openpolar
spelling ftdatacite:10.5281/zenodo.2554184 2023-05-15T16:21:17+02:00 Tsunamis due to ice masses: Different calving mechanisms and linkage to landslide-tsunamis - Dataset Valentin, Heller 2019 https://dx.doi.org/10.5281/zenodo.2554184 https://zenodo.org/record/2554184 unknown Zenodo https://zenodo.org/communities/hydralab https://dx.doi.org/10.5281/zenodo.2554183 https://zenodo.org/communities/hydralab Embargoed Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/embargoedAccess CC-BY Capsizing Greenland Iceberg Iceberg-tsunamis Laboratory experiments Outlet glacier Tsunamis dataset Dataset 2019 ftdatacite https://doi.org/10.5281/zenodo.2554184 https://doi.org/10.5281/zenodo.2554183 2021-11-05T12:55:41Z Land ice melt and retreat is one of the most visible effects of climate change and contributes ≈1.5 mm/year to global sea-level rise (SLR) of a total of ≈2.7 mm/year. Global warming results in the shrinking of ice masses in most ice covered regions in the World, particularly in the Alps and in Greenland and the Greenlandic mass loss is estimated at –269 ±51 Gt/year. A significant part of this mass loss is through the detachment of icebergs at glacier fronts in a mechanism called iceberg calving. Such iceberg impacting into a water body generate tsunamis, such called "iceberg-tsunamis". Such an iceberg-tsunami reached a height of 50 m at the Eqip Sermia outlet glacier in 2014. These tsunamis pose a considerable hazard for the local community, the fishing industry and the increasing number of tourists in ice covered areas. Several iceberg calving mechanisms have been proposed including fall, over-turning and capsizing. Reliable guidance on the upper limit of iceberg-tsunami heights are currently unavailable. A main reason for this limited understanding is that reliable field data are rare, such that laboratory tests complemented with numerical simulations are important to advance this research field. This was the aim of this HYDRALAB+ funded study. The wave features (height, length, velocity) caused by icebergs in function of the iceberg calving mechanisms (fall, over-turning, capsizing), as well as the mass volume and kinematics, were modelled in unique large-scale experiments. This minimised both scale effects and wave reflection. The attached files and folders include information about and data from these experiments. Dataset glacier Greenland greenlandic ice covered areas DataCite Metadata Store (German National Library of Science and Technology) Eqip Sermia ENVELOPE(-50.067,-50.067,69.817,69.817) Greenland
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Capsizing
Greenland
Iceberg
Iceberg-tsunamis
Laboratory experiments
Outlet glacier
Tsunamis
spellingShingle Capsizing
Greenland
Iceberg
Iceberg-tsunamis
Laboratory experiments
Outlet glacier
Tsunamis
Valentin, Heller
Tsunamis due to ice masses: Different calving mechanisms and linkage to landslide-tsunamis - Dataset
topic_facet Capsizing
Greenland
Iceberg
Iceberg-tsunamis
Laboratory experiments
Outlet glacier
Tsunamis
description Land ice melt and retreat is one of the most visible effects of climate change and contributes ≈1.5 mm/year to global sea-level rise (SLR) of a total of ≈2.7 mm/year. Global warming results in the shrinking of ice masses in most ice covered regions in the World, particularly in the Alps and in Greenland and the Greenlandic mass loss is estimated at –269 ±51 Gt/year. A significant part of this mass loss is through the detachment of icebergs at glacier fronts in a mechanism called iceberg calving. Such iceberg impacting into a water body generate tsunamis, such called "iceberg-tsunamis". Such an iceberg-tsunami reached a height of 50 m at the Eqip Sermia outlet glacier in 2014. These tsunamis pose a considerable hazard for the local community, the fishing industry and the increasing number of tourists in ice covered areas. Several iceberg calving mechanisms have been proposed including fall, over-turning and capsizing. Reliable guidance on the upper limit of iceberg-tsunami heights are currently unavailable. A main reason for this limited understanding is that reliable field data are rare, such that laboratory tests complemented with numerical simulations are important to advance this research field. This was the aim of this HYDRALAB+ funded study. The wave features (height, length, velocity) caused by icebergs in function of the iceberg calving mechanisms (fall, over-turning, capsizing), as well as the mass volume and kinematics, were modelled in unique large-scale experiments. This minimised both scale effects and wave reflection. The attached files and folders include information about and data from these experiments.
format Dataset
author Valentin, Heller
author_facet Valentin, Heller
author_sort Valentin, Heller
title Tsunamis due to ice masses: Different calving mechanisms and linkage to landslide-tsunamis - Dataset
title_short Tsunamis due to ice masses: Different calving mechanisms and linkage to landslide-tsunamis - Dataset
title_full Tsunamis due to ice masses: Different calving mechanisms and linkage to landslide-tsunamis - Dataset
title_fullStr Tsunamis due to ice masses: Different calving mechanisms and linkage to landslide-tsunamis - Dataset
title_full_unstemmed Tsunamis due to ice masses: Different calving mechanisms and linkage to landslide-tsunamis - Dataset
title_sort tsunamis due to ice masses: different calving mechanisms and linkage to landslide-tsunamis - dataset
publisher Zenodo
publishDate 2019
url https://dx.doi.org/10.5281/zenodo.2554184
https://zenodo.org/record/2554184
long_lat ENVELOPE(-50.067,-50.067,69.817,69.817)
geographic Eqip Sermia
Greenland
geographic_facet Eqip Sermia
Greenland
genre glacier
Greenland
greenlandic
ice covered areas
genre_facet glacier
Greenland
greenlandic
ice covered areas
op_relation https://zenodo.org/communities/hydralab
https://dx.doi.org/10.5281/zenodo.2554183
https://zenodo.org/communities/hydralab
op_rights Embargoed Access
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
info:eu-repo/semantics/embargoedAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.5281/zenodo.2554184
https://doi.org/10.5281/zenodo.2554183
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