Hydroelastic analysis of ice shelves under long wave excitation

The transient hydroelastic response of an ice shelf under long wave excitation is analysed by means of the finite element method. The simple model, presented in this work, is used for the simulation of the generated kinematic and stress fields in an ice shelf, when the latter interacts with a tsunam...

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Main Authors: T. K. Papathanasiou, A. E. Karperaki, E. E. Theotokoglou, K. A. Belibassakis
Format: Article
Language:English
Published: Copernicus Publications 2015-08-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/15/1851/2015/nhess-15-1851-2015.pdf
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spelling doaj-9dd4517db9da44f3bac50ff04ecef7e32020-11-24T21:04:24ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812015-08-011581851185710.5194/nhess-15-1851-2015Hydroelastic analysis of ice shelves under long wave excitationT. K. Papathanasiou0A. E. Karperaki1E. E. Theotokoglou2K. A. Belibassakis3Department of Civil Engineering and Surveying & Geoinformatics Engineering, Technological Educational Institute of Athens, Athens, GreeceSchool of Naval Architecture and Marine Engineering, National Technical University of Athens, Zografou Campus, Athens, GreeceDepartment of Mechanics, School of Applied Mathematical and Physical Science, National Technical University of Athens, Zografou Campus, Athens, GreeceSchool of Naval Architecture and Marine Engineering, National Technical University of Athens, Zografou Campus, Athens, GreeceThe transient hydroelastic response of an ice shelf under long wave excitation is analysed by means of the finite element method. The simple model, presented in this work, is used for the simulation of the generated kinematic and stress fields in an ice shelf, when the latter interacts with a tsunami wave. The ice shelf, being of large length compared to its thickness, is modelled as an elastic Euler-Bernoulli beam, constrained at the grounding line. The hydrodynamic field is represented by the linearised shallow water equations. The numerical solution is based on the development of a special hydroelastic finite element for the system of governing of equations. Motivated by the 2011 Sulzberger Ice Shelf (SIS) calving event and its correlation with the Honshu Tsunami, the SIS stable configuration is studied. The extreme values of the bending moment distribution in both space and time are examined. Finally, the location of these extrema is investigated for different values of ice shelf thickness and tsunami wave length.http://www.nat-hazards-earth-syst-sci.net/15/1851/2015/nhess-15-1851-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author T. K. Papathanasiou
A. E. Karperaki
E. E. Theotokoglou
K. A. Belibassakis
spellingShingle T. K. Papathanasiou
A. E. Karperaki
E. E. Theotokoglou
K. A. Belibassakis
Hydroelastic analysis of ice shelves under long wave excitation
Natural Hazards and Earth System Sciences
author_facet T. K. Papathanasiou
A. E. Karperaki
E. E. Theotokoglou
K. A. Belibassakis
author_sort T. K. Papathanasiou
title Hydroelastic analysis of ice shelves under long wave excitation
title_short Hydroelastic analysis of ice shelves under long wave excitation
title_full Hydroelastic analysis of ice shelves under long wave excitation
title_fullStr Hydroelastic analysis of ice shelves under long wave excitation
title_full_unstemmed Hydroelastic analysis of ice shelves under long wave excitation
title_sort hydroelastic analysis of ice shelves under long wave excitation
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2015-08-01
description The transient hydroelastic response of an ice shelf under long wave excitation is analysed by means of the finite element method. The simple model, presented in this work, is used for the simulation of the generated kinematic and stress fields in an ice shelf, when the latter interacts with a tsunami wave. The ice shelf, being of large length compared to its thickness, is modelled as an elastic Euler-Bernoulli beam, constrained at the grounding line. The hydrodynamic field is represented by the linearised shallow water equations. The numerical solution is based on the development of a special hydroelastic finite element for the system of governing of equations. Motivated by the 2011 Sulzberger Ice Shelf (SIS) calving event and its correlation with the Honshu Tsunami, the SIS stable configuration is studied. The extreme values of the bending moment distribution in both space and time are examined. Finally, the location of these extrema is investigated for different values of ice shelf thickness and tsunami wave length.
url http://www.nat-hazards-earth-syst-sci.net/15/1851/2015/nhess-15-1851-2015.pdf
work_keys_str_mv AT tkpapathanasiou hydroelasticanalysisoficeshelvesunderlongwaveexcitation
AT aekarperaki hydroelasticanalysisoficeshelvesunderlongwaveexcitation
AT eetheotokoglou hydroelasticanalysisoficeshelvesunderlongwaveexcitation
AT kabelibassakis hydroelasticanalysisoficeshelvesunderlongwaveexcitation
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