author_facet Konovalov, Yuri V.
Konovalov, Yuri V.
author Konovalov, Yuri V.
spellingShingle Konovalov, Yuri V.
Annals of Glaciology
Ice-shelf vibrations modeled by a full 3-D elastic model
Earth-Surface Processes
author_sort konovalov, yuri v.
spelling Konovalov, Yuri V. 0260-3055 1727-5644 Cambridge University Press (CUP) Earth-Surface Processes http://dx.doi.org/10.1017/aog.2019.9 <jats:title>ABSTRACT</jats:title><jats:p>Forced ice-shelf vibration modeling is performed using a full 3-D finite-difference elastic model, which also takes into account sub-ice seawater flow. The sea water flow is described by the wave equation. Ice-shelf flexure therefore results from hydrostatic pressure perturbations in the sub-ice seawater layer. Numerical experiments were undertaken for idealized rectangular ice-shelf geometry. The ice-plate vibrations were modeled for harmonic incoming pressure perturbations and for a wide range of incoming wave frequencies. The spectra showed distinct resonant peaks, which demonstrate the ability of the model to simulate a resonant-like motion. The spectra obtained by the full 3-D model are compared with exact solutions for the elastic thin plate with two fixed edges and two free edges. The spectra are also compared with the spectra modeled by the thin-plate Holdsworth and Glynn model (1978).</jats:p> Ice-shelf vibrations modeled by a full 3-D elastic model Annals of Glaciology
doi_str_mv 10.1017/aog.2019.9
facet_avail Online
Free
finc_class_facet Geologie und Paläontologie
Geographie
format ElectronicArticle
fullrecord blob:ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTAxNy9hb2cuMjAxOS45
id ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTAxNy9hb2cuMjAxOS45
institution DE-D275
DE-Bn3
DE-Brt1
DE-Zwi2
DE-D161
DE-Zi4
DE-Gla1
DE-15
DE-Pl11
DE-Rs1
DE-14
DE-105
DE-Ch1
DE-L229
imprint Cambridge University Press (CUP), 2019
imprint_str_mv Cambridge University Press (CUP), 2019
issn 0260-3055
1727-5644
issn_str_mv 0260-3055
1727-5644
language English
mega_collection Cambridge University Press (CUP) (CrossRef)
match_str konovalov2019iceshelfvibrationsmodeledbyafull3delasticmodel
publishDateSort 2019
publisher Cambridge University Press (CUP)
recordtype ai
record_format ai
series Annals of Glaciology
source_id 49
title Ice-shelf vibrations modeled by a full 3-D elastic model
title_unstemmed Ice-shelf vibrations modeled by a full 3-D elastic model
title_full Ice-shelf vibrations modeled by a full 3-D elastic model
title_fullStr Ice-shelf vibrations modeled by a full 3-D elastic model
title_full_unstemmed Ice-shelf vibrations modeled by a full 3-D elastic model
title_short Ice-shelf vibrations modeled by a full 3-D elastic model
title_sort ice-shelf vibrations modeled by a full 3-d elastic model
topic Earth-Surface Processes
url http://dx.doi.org/10.1017/aog.2019.9
publishDate 2019
physical 68-74
description <jats:title>ABSTRACT</jats:title><jats:p>Forced ice-shelf vibration modeling is performed using a full 3-D finite-difference elastic model, which also takes into account sub-ice seawater flow. The sea water flow is described by the wave equation. Ice-shelf flexure therefore results from hydrostatic pressure perturbations in the sub-ice seawater layer. Numerical experiments were undertaken for idealized rectangular ice-shelf geometry. The ice-plate vibrations were modeled for harmonic incoming pressure perturbations and for a wide range of incoming wave frequencies. The spectra showed distinct resonant peaks, which demonstrate the ability of the model to simulate a resonant-like motion. The spectra obtained by the full 3-D model are compared with exact solutions for the elastic thin plate with two fixed edges and two free edges. The spectra are also compared with the spectra modeled by the thin-plate Holdsworth and Glynn model (1978).</jats:p>
container_issue 79
container_start_page 68
container_title Annals of Glaciology
container_volume 60
format_de105 Article, E-Article
format_de14 Article, E-Article
format_de15 Article, E-Article
format_de520 Article, E-Article
format_de540 Article, E-Article
format_dech1 Article, E-Article
format_ded117 Article, E-Article
format_degla1 E-Article
format_del152 Buch
format_del189 Article, E-Article
format_dezi4 Article
format_dezwi2 Article, E-Article
format_finc Article, E-Article
format_nrw Article, E-Article
_version_ 1792332378631307266
geogr_code not assigned
last_indexed 2024-03-01T13:55:03.805Z
geogr_code_person not assigned
openURL url_ver=Z39.88-2004&ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fvufind.svn.sourceforge.net%3Agenerator&rft.title=Ice-shelf+vibrations+modeled+by+a+full+3-D+elastic+model&rft.date=2019-09-01&genre=article&issn=1727-5644&volume=60&issue=79&spage=68&epage=74&pages=68-74&jtitle=Annals+of+Glaciology&atitle=Ice-shelf+vibrations+modeled+by+a+full+3-D+elastic+model&aulast=Konovalov&aufirst=Yuri+V.&rft_id=info%3Adoi%2F10.1017%2Faog.2019.9&rft.language%5B0%5D=eng
SOLR
_version_ 1792332378631307266
author Konovalov, Yuri V.
author_facet Konovalov, Yuri V., Konovalov, Yuri V.
author_sort konovalov, yuri v.
container_issue 79
container_start_page 68
container_title Annals of Glaciology
container_volume 60
description <jats:title>ABSTRACT</jats:title><jats:p>Forced ice-shelf vibration modeling is performed using a full 3-D finite-difference elastic model, which also takes into account sub-ice seawater flow. The sea water flow is described by the wave equation. Ice-shelf flexure therefore results from hydrostatic pressure perturbations in the sub-ice seawater layer. Numerical experiments were undertaken for idealized rectangular ice-shelf geometry. The ice-plate vibrations were modeled for harmonic incoming pressure perturbations and for a wide range of incoming wave frequencies. The spectra showed distinct resonant peaks, which demonstrate the ability of the model to simulate a resonant-like motion. The spectra obtained by the full 3-D model are compared with exact solutions for the elastic thin plate with two fixed edges and two free edges. The spectra are also compared with the spectra modeled by the thin-plate Holdsworth and Glynn model (1978).</jats:p>
doi_str_mv 10.1017/aog.2019.9
facet_avail Online, Free
finc_class_facet Geologie und Paläontologie, Geographie
format ElectronicArticle
format_de105 Article, E-Article
format_de14 Article, E-Article
format_de15 Article, E-Article
format_de520 Article, E-Article
format_de540 Article, E-Article
format_dech1 Article, E-Article
format_ded117 Article, E-Article
format_degla1 E-Article
format_del152 Buch
format_del189 Article, E-Article
format_dezi4 Article
format_dezwi2 Article, E-Article
format_finc Article, E-Article
format_nrw Article, E-Article
geogr_code not assigned
geogr_code_person not assigned
id ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTAxNy9hb2cuMjAxOS45
imprint Cambridge University Press (CUP), 2019
imprint_str_mv Cambridge University Press (CUP), 2019
institution DE-D275, DE-Bn3, DE-Brt1, DE-Zwi2, DE-D161, DE-Zi4, DE-Gla1, DE-15, DE-Pl11, DE-Rs1, DE-14, DE-105, DE-Ch1, DE-L229
issn 0260-3055, 1727-5644
issn_str_mv 0260-3055, 1727-5644
language English
last_indexed 2024-03-01T13:55:03.805Z
match_str konovalov2019iceshelfvibrationsmodeledbyafull3delasticmodel
mega_collection Cambridge University Press (CUP) (CrossRef)
physical 68-74
publishDate 2019
publishDateSort 2019
publisher Cambridge University Press (CUP)
record_format ai
recordtype ai
series Annals of Glaciology
source_id 49
spelling Konovalov, Yuri V. 0260-3055 1727-5644 Cambridge University Press (CUP) Earth-Surface Processes http://dx.doi.org/10.1017/aog.2019.9 <jats:title>ABSTRACT</jats:title><jats:p>Forced ice-shelf vibration modeling is performed using a full 3-D finite-difference elastic model, which also takes into account sub-ice seawater flow. The sea water flow is described by the wave equation. Ice-shelf flexure therefore results from hydrostatic pressure perturbations in the sub-ice seawater layer. Numerical experiments were undertaken for idealized rectangular ice-shelf geometry. The ice-plate vibrations were modeled for harmonic incoming pressure perturbations and for a wide range of incoming wave frequencies. The spectra showed distinct resonant peaks, which demonstrate the ability of the model to simulate a resonant-like motion. The spectra obtained by the full 3-D model are compared with exact solutions for the elastic thin plate with two fixed edges and two free edges. The spectra are also compared with the spectra modeled by the thin-plate Holdsworth and Glynn model (1978).</jats:p> Ice-shelf vibrations modeled by a full 3-D elastic model Annals of Glaciology
spellingShingle Konovalov, Yuri V., Annals of Glaciology, Ice-shelf vibrations modeled by a full 3-D elastic model, Earth-Surface Processes
title Ice-shelf vibrations modeled by a full 3-D elastic model
title_full Ice-shelf vibrations modeled by a full 3-D elastic model
title_fullStr Ice-shelf vibrations modeled by a full 3-D elastic model
title_full_unstemmed Ice-shelf vibrations modeled by a full 3-D elastic model
title_short Ice-shelf vibrations modeled by a full 3-D elastic model
title_sort ice-shelf vibrations modeled by a full 3-d elastic model
title_unstemmed Ice-shelf vibrations modeled by a full 3-D elastic model
topic Earth-Surface Processes
url http://dx.doi.org/10.1017/aog.2019.9