Data depository - "Quantifying the effect of wind on volcanic plumes: implications for plume modelling" ...

This depository contains all data to understand, evaluate, and build upon the research reported in the manuscript: "Quantifying the effect of wind on volcanic plumes: implications for plume modelling", submitted to Journal of Geophysical Research. Abstract The considerable effects that win...

Full description

Bibliographic Details
Main Authors: Dürig, Tobias, Gudmundsson, Magnús T., Dioguardi, Fabio, Schmidt, Louise S.
Format: Dataset
Language:English
Published: Zenodo 2022
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.7040203
https://zenodo.org/record/7040203
id ftdatacite:10.5281/zenodo.7040203
record_format openpolar
spelling ftdatacite:10.5281/zenodo.7040203 2023-06-11T04:11:33+02:00 Data depository - "Quantifying the effect of wind on volcanic plumes: implications for plume modelling" ... Dürig, Tobias Gudmundsson, Magnús T. Dioguardi, Fabio Schmidt, Louise S. 2022 https://dx.doi.org/10.5281/zenodo.7040203 https://zenodo.org/record/7040203 en eng Zenodo https://dx.doi.org/10.5281/zenodo.7040202 Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess eruption source parameters; volcanic ash; uncertainty; explosive volcanic eruptions; buoyant plume models; wind entrainment coefficient Dataset dataset 2022 ftdatacite https://doi.org/10.5281/zenodo.704020310.5281/zenodo.7040202 2023-05-02T11:03:49Z This depository contains all data to understand, evaluate, and build upon the research reported in the manuscript: "Quantifying the effect of wind on volcanic plumes: implications for plume modelling", submitted to Journal of Geophysical Research. Abstract The considerable effects that wind can have on estimates of mass eruption rates (MERs) in explosive eruptions based on volcanic plume height are well known but difficult to quantify rigorously. Many explicitly wind-affected plume models have the additional difficulty that they require the use of centerline heights of bent-over plumes, a parameter not easily obtained directly from observational data. We tested two such models by using the time series of varying plume heights and wind speeds of the 2010 Eyjafjallajökull eruption. The mapped fallout and photos taken during this eruption allow us to estimate the plume geometry and to empirically constrain input parameters for the two models tested. Two strategies are presented to correct the difference in ... : When using the provided data or scripts in any form, please cite our corresponding article. ... Dataset Eyjafjallajökull 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 English
topic eruption source parameters; volcanic ash; uncertainty; explosive volcanic eruptions; buoyant plume models; wind entrainment coefficient
spellingShingle eruption source parameters; volcanic ash; uncertainty; explosive volcanic eruptions; buoyant plume models; wind entrainment coefficient
Dürig, Tobias
Gudmundsson, Magnús T.
Dioguardi, Fabio
Schmidt, Louise S.
Data depository - "Quantifying the effect of wind on volcanic plumes: implications for plume modelling" ...
topic_facet eruption source parameters; volcanic ash; uncertainty; explosive volcanic eruptions; buoyant plume models; wind entrainment coefficient
description This depository contains all data to understand, evaluate, and build upon the research reported in the manuscript: "Quantifying the effect of wind on volcanic plumes: implications for plume modelling", submitted to Journal of Geophysical Research. Abstract The considerable effects that wind can have on estimates of mass eruption rates (MERs) in explosive eruptions based on volcanic plume height are well known but difficult to quantify rigorously. Many explicitly wind-affected plume models have the additional difficulty that they require the use of centerline heights of bent-over plumes, a parameter not easily obtained directly from observational data. We tested two such models by using the time series of varying plume heights and wind speeds of the 2010 Eyjafjallajökull eruption. The mapped fallout and photos taken during this eruption allow us to estimate the plume geometry and to empirically constrain input parameters for the two models tested. Two strategies are presented to correct the difference in ... : When using the provided data or scripts in any form, please cite our corresponding article. ...
format Dataset
author Dürig, Tobias
Gudmundsson, Magnús T.
Dioguardi, Fabio
Schmidt, Louise S.
author_facet Dürig, Tobias
Gudmundsson, Magnús T.
Dioguardi, Fabio
Schmidt, Louise S.
author_sort Dürig, Tobias
title Data depository - "Quantifying the effect of wind on volcanic plumes: implications for plume modelling" ...
title_short Data depository - "Quantifying the effect of wind on volcanic plumes: implications for plume modelling" ...
title_full Data depository - "Quantifying the effect of wind on volcanic plumes: implications for plume modelling" ...
title_fullStr Data depository - "Quantifying the effect of wind on volcanic plumes: implications for plume modelling" ...
title_full_unstemmed Data depository - "Quantifying the effect of wind on volcanic plumes: implications for plume modelling" ...
title_sort data depository - "quantifying the effect of wind on volcanic plumes: implications for plume modelling" ...
publisher Zenodo
publishDate 2022
url https://dx.doi.org/10.5281/zenodo.7040203
https://zenodo.org/record/7040203
genre Eyjafjallajökull
genre_facet Eyjafjallajökull
op_relation https://dx.doi.org/10.5281/zenodo.7040202
op_rights Open Access
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5281/zenodo.704020310.5281/zenodo.7040202
_version_ 1768386707797835776