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

Wickert, A. D.

doi:https://doi.org/10.5194/gmd-9-997-2016

Articles | Volume 9, issue 3

https://doi.org/10.5194/gmd-9-997-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/gmd-9-997-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 9, issue 3

Model description paper

|

08 Mar 2016

Model description paper |

| 08 Mar 2016

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

A. D. Wickert

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Final revised paper (published on 08 Mar 2016)
Preprint (discussion started on 02 Jun 2015)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC C1871: 'Referee comments', Anonymous Referee #1, 03 Sep 2015
- AC C3476: 'Response to Reviewer #1', Andrew Wickert, 25 Dec 2015
RC C2904: 'Review of the article "Open-source modular solutions for flexural isostasy: gFlex v1.0"', Anonymous Referee #2, 13 Nov 2015
- AC C3488: 'Response to Reviewer #2', Andrew Wickert, 25 Dec 2015

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Andrew Wickert on behalf of the Authors (25 Dec 2015) Author's response Manuscript

ED: Publish as is (06 Jan 2016) by Lutz Gross

AR by Andrew Wickert on behalf of the Authors (28 Jan 2016) Manuscript

Short summary

Earth's lithosphere bends beneath surface loads, such as ice, sediments, and mountain belts. The pattern of this bending, or flexural isostatic response, is a function of both the loads and the spatially variable strength of the lithosphere. gFlex is an easy-to-use program to calculate flexural isostastic response, and may be used to better understand how ice sheets, glaciers, large lakes, sedimentary basins, volcanoes, and other surface loads interact with the solid Earth.