Data to support modeling of the 2015 Tyndall Glacier landslide, Alaska

Landslide-generated tsunamis pose significant hazards, but developing models to assess these hazards presents unique challenges. George and others (2017) present a new methodology in which a depth-averaged two-phase landslide model (D-Claw) is used to simulate all stages of landslide dynamics and su...

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Main Authors: Cannon, Charles M., George, David L., Iverson, Richard M
Format: Dataset
Language:unknown
Published: U.S. Geological Survey 2017
Subjects:
Online Access:https://dx.doi.org/10.5066/f73r0rr3
https://www.sciencebase.gov/catalog/item/5963e612e4b0d1f9f059d94b
id ftdatacite:10.5066/f73r0rr3
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spelling ftdatacite:10.5066/f73r0rr3 2023-05-15T16:20:26+02:00 Data to support modeling of the 2015 Tyndall Glacier landslide, Alaska Cannon, Charles M. George, David L. Iverson, Richard M 2017 https://dx.doi.org/10.5066/f73r0rr3 https://www.sciencebase.gov/catalog/item/5963e612e4b0d1f9f059d94b unknown U.S. Geological Survey https://dx.doi.org/10.1002/2017gl074341 https://dx.doi.org/10.1016/j.enggeo.2021.106384 dataset Dataset 2017 ftdatacite https://doi.org/10.5066/f73r0rr3 https://doi.org/10.1002/2017gl074341 https://doi.org/10.1016/j.enggeo.2021.106384 2022-02-08T13:42:09Z Landslide-generated tsunamis pose significant hazards, but developing models to assess these hazards presents unique challenges. George and others (2017) present a new methodology in which a depth-averaged two-phase landslide model (D-Claw) is used to simulate all stages of landslide dynamics and subsequent tsunami generation, propagation, and inundation. Because the model describes the evolution of solid and fluid volume fractions, it treats both landslides and tsunamis as special cases of a more general class of phenomena. Therefore, the landslide and tsunami can be seamlessly and efficiently simulated as a single-layer continuum with evolving solid-grain concentrations, and with wave generation via mass displacement and direct longitudinal momentum transfer: dominant physical mechanisms that are unresolved with traditional modeling approaches. To test their methodology, George and others (2017) used D-Claw to model a large subaerial landslide and resulting tsunami that occurred on October, 17, 2015, in Taan Fiord near the terminus of Tyndall Glacier, Alaska. Modeled shoreline inundation patterns compare well with observations derived from satellite imagery. This data release contains topographic datasets used to model the landslide and a Normalized difference vegetation index (NDVI) change image used to assess the model results. These data are intended to accompany the journal article by George and others (2017): George, D.L., Iverson, R.M., and Cannon, C.M., 2017, New methodology for computing tsunami generation by subaerial landslides: application to the 2015 Tyndall Glacier Landslide, Alaska, Geophysical Research Letters, 44, doi:10.1002/2017GL074341. Dataset glacier Alaska DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
description Landslide-generated tsunamis pose significant hazards, but developing models to assess these hazards presents unique challenges. George and others (2017) present a new methodology in which a depth-averaged two-phase landslide model (D-Claw) is used to simulate all stages of landslide dynamics and subsequent tsunami generation, propagation, and inundation. Because the model describes the evolution of solid and fluid volume fractions, it treats both landslides and tsunamis as special cases of a more general class of phenomena. Therefore, the landslide and tsunami can be seamlessly and efficiently simulated as a single-layer continuum with evolving solid-grain concentrations, and with wave generation via mass displacement and direct longitudinal momentum transfer: dominant physical mechanisms that are unresolved with traditional modeling approaches. To test their methodology, George and others (2017) used D-Claw to model a large subaerial landslide and resulting tsunami that occurred on October, 17, 2015, in Taan Fiord near the terminus of Tyndall Glacier, Alaska. Modeled shoreline inundation patterns compare well with observations derived from satellite imagery. This data release contains topographic datasets used to model the landslide and a Normalized difference vegetation index (NDVI) change image used to assess the model results. These data are intended to accompany the journal article by George and others (2017): George, D.L., Iverson, R.M., and Cannon, C.M., 2017, New methodology for computing tsunami generation by subaerial landslides: application to the 2015 Tyndall Glacier Landslide, Alaska, Geophysical Research Letters, 44, doi:10.1002/2017GL074341.
format Dataset
author Cannon, Charles M.
George, David L.
Iverson, Richard M
spellingShingle Cannon, Charles M.
George, David L.
Iverson, Richard M
Data to support modeling of the 2015 Tyndall Glacier landslide, Alaska
author_facet Cannon, Charles M.
George, David L.
Iverson, Richard M
author_sort Cannon, Charles M.
title Data to support modeling of the 2015 Tyndall Glacier landslide, Alaska
title_short Data to support modeling of the 2015 Tyndall Glacier landslide, Alaska
title_full Data to support modeling of the 2015 Tyndall Glacier landslide, Alaska
title_fullStr Data to support modeling of the 2015 Tyndall Glacier landslide, Alaska
title_full_unstemmed Data to support modeling of the 2015 Tyndall Glacier landslide, Alaska
title_sort data to support modeling of the 2015 tyndall glacier landslide, alaska
publisher U.S. Geological Survey
publishDate 2017
url https://dx.doi.org/10.5066/f73r0rr3
https://www.sciencebase.gov/catalog/item/5963e612e4b0d1f9f059d94b
genre glacier
Alaska
genre_facet glacier
Alaska
op_relation https://dx.doi.org/10.1002/2017gl074341
https://dx.doi.org/10.1016/j.enggeo.2021.106384
op_doi https://doi.org/10.5066/f73r0rr3
https://doi.org/10.1002/2017gl074341
https://doi.org/10.1016/j.enggeo.2021.106384
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