Open-source modular solutions for flexural isostasy: gFlex v1.0

Isostasy is one of the oldest and most widely applied concepts in the geosciences, but the geoscientific community lacks a coherent, easy-to-use tool to simulate flexure of a realistic (i.e., laterally heterogeneous) lithosphere under an arbitrary set of surface loads. Such a model is needed for stu...

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Published in:Geoscientific Model Development
Main Author: Wickert, Andrew D.
Format: Article in Journal/Newspaper
Language:English
Published: 2016
Subjects:
Online Access:https://publishup.uni-potsdam.de/opus4-ubp/frontdoor/index/index/docId/45807
https://doi.org/10.5194/gmd-9-997-2016
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spelling ftubpotsdam:oai:kobv.de-opus4-uni-potsdam:45807 2023-05-15T16:38:19+02:00 Open-source modular solutions for flexural isostasy: gFlex v1.0 Wickert, Andrew D. 2016 https://publishup.uni-potsdam.de/opus4-ubp/frontdoor/index/index/docId/45807 https://doi.org/10.5194/gmd-9-997-2016 eng eng https://publishup.uni-potsdam.de/opus4-ubp/frontdoor/index/index/docId/45807 https://doi.org/10.5194/gmd-9-997-2016 info:eu-repo/semantics/closedAccess Institut für Geowissenschaften article doc-type:article 2016 ftubpotsdam https://doi.org/10.5194/gmd-9-997-2016 2022-07-28T20:48:56Z Isostasy is one of the oldest and most widely applied concepts in the geosciences, but the geoscientific community lacks a coherent, easy-to-use tool to simulate flexure of a realistic (i.e., laterally heterogeneous) lithosphere under an arbitrary set of surface loads. Such a model is needed for studies of mountain building, sedimentary basin formation, glaciation, sea-level change, and other tectonic, geodynamic, and surface processes. Here I present gFlex (for GNU flexure), an open-source model that can produce analytical and finite difference solutions for lithospheric flexure in one (profile) and two (map view) dimensions. To simulate the flexural isostatic response to an imposed load, it can be used by itself or within GRASS GIS for better integration with field data. gFlex is also a component with the Community Surface Dynamics Modeling System (CSDMS) and Landlab modeling frameworks for coupling with a wide range of Earth-surface-related models, and can be coupled to additional models within Python scripts. As an example of this in-script coupling, I simulate the effects of spatially variable lithospheric thickness on a modeled Iceland ice cap. Finite difference solutions in gFlex can use any of five types of boundary conditions: 0-displacement, 0-slope (i.e., clamped); 0-slope, 0-shear; 0-moment, 0-shear (i.e., broken plate); mirror symmetry; and periodic. Typical calculations with gFlex require << 1 s to similar to 1 min on a personal laptop computer. These characteristics - multiple ways to run the model, multiple solution methods, multiple boundary conditions, and short compute time - make gFlex an effective tool for flexural isostatic modeling across the geosciences. Article in Journal/Newspaper Ice cap Iceland University of Potsdam: publish.UP Geoscientific Model Development 9 3 997 1017
institution Open Polar
collection University of Potsdam: publish.UP
op_collection_id ftubpotsdam
language English
topic Institut für Geowissenschaften
spellingShingle Institut für Geowissenschaften
Wickert, Andrew D.
Open-source modular solutions for flexural isostasy: gFlex v1.0
topic_facet Institut für Geowissenschaften
description Isostasy is one of the oldest and most widely applied concepts in the geosciences, but the geoscientific community lacks a coherent, easy-to-use tool to simulate flexure of a realistic (i.e., laterally heterogeneous) lithosphere under an arbitrary set of surface loads. Such a model is needed for studies of mountain building, sedimentary basin formation, glaciation, sea-level change, and other tectonic, geodynamic, and surface processes. Here I present gFlex (for GNU flexure), an open-source model that can produce analytical and finite difference solutions for lithospheric flexure in one (profile) and two (map view) dimensions. To simulate the flexural isostatic response to an imposed load, it can be used by itself or within GRASS GIS for better integration with field data. gFlex is also a component with the Community Surface Dynamics Modeling System (CSDMS) and Landlab modeling frameworks for coupling with a wide range of Earth-surface-related models, and can be coupled to additional models within Python scripts. As an example of this in-script coupling, I simulate the effects of spatially variable lithospheric thickness on a modeled Iceland ice cap. Finite difference solutions in gFlex can use any of five types of boundary conditions: 0-displacement, 0-slope (i.e., clamped); 0-slope, 0-shear; 0-moment, 0-shear (i.e., broken plate); mirror symmetry; and periodic. Typical calculations with gFlex require << 1 s to similar to 1 min on a personal laptop computer. These characteristics - multiple ways to run the model, multiple solution methods, multiple boundary conditions, and short compute time - make gFlex an effective tool for flexural isostatic modeling across the geosciences.
format Article in Journal/Newspaper
author Wickert, Andrew D.
author_facet Wickert, Andrew D.
author_sort Wickert, Andrew D.
title Open-source modular solutions for flexural isostasy: gFlex v1.0
title_short Open-source modular solutions for flexural isostasy: gFlex v1.0
title_full Open-source modular solutions for flexural isostasy: gFlex v1.0
title_fullStr Open-source modular solutions for flexural isostasy: gFlex v1.0
title_full_unstemmed Open-source modular solutions for flexural isostasy: gFlex v1.0
title_sort open-source modular solutions for flexural isostasy: gflex v1.0
publishDate 2016
url https://publishup.uni-potsdam.de/opus4-ubp/frontdoor/index/index/docId/45807
https://doi.org/10.5194/gmd-9-997-2016
genre Ice cap
Iceland
genre_facet Ice cap
Iceland
op_relation https://publishup.uni-potsdam.de/opus4-ubp/frontdoor/index/index/docId/45807
https://doi.org/10.5194/gmd-9-997-2016
op_rights info:eu-repo/semantics/closedAccess
op_doi https://doi.org/10.5194/gmd-9-997-2016
container_title Geoscientific Model Development
container_volume 9
container_issue 3
container_start_page 997
op_container_end_page 1017
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