hvidy / PIPE-4002-EarthByte-ModelAtlas

SIH repo for work on PIPE-4002
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The flexural isostatic response of climatically driven sea-level changes on continental-scale deltas #14

Open saraemp opened 6 months ago

saraemp commented 6 months ago

-> creator/contributor ORCID (or name)

0000-0002-1270-4377

-> slug

polanco-2023-deltas

-> field of Research (FoR) Codes

3706: Geophysics, 370604: Geodynamics

-> license

CC-BY-4.0

-> model category

model published in study

-> associated publication DOI

http://dx.doi.org/10.5194/egusphere-2023-53

-> title

No response

-> description

No response

-> model authors

No response

-> scientific keywords

No response

-> funder

No response

-> include model code ?

-> model code URI/DOI

10.5281/zenodo.1069573

-> include model output data?

-> model output URI/DOI

No response

-> software framework DOI/URI

10.5281/zenodo.1069573

-> software framework source repository

https://github.com/badlands-model/badlands

-> name of primary software framework (e.g. Underworld, ASPECT, Badlands, OpenFOAM)

Badlands

-> software framework authors

No response

-> software & algorithm keywords

No response

-> computer URI/DOI

No response

-> add landing page image and caption

egusphere-2023-53_Fig5.pdf

-> add an animation (if relevant)

https://github.com/hvidy/PIPE-4002-EarthByte-ModelAtlas/assets/29790931/a3c8f65b-50ec-4cd8-80b3-4e83ff5bb6a0

-> add a graphic abstract figure (if relevant)

egusphere-2023-53_Fig1

-> add a model setup figure (if relevant)

Screen Shot 2023-12-21 at 10 31 53

-> add a description of your model setup

The initial configuration of the modeling domain resembles the topography of a natural source-to-sink system with 3400 m elevation in the headwaters, a length of 4500 km, a downstream-decreasing fluvial channel slope, and successive inflections in gradient associated with the coastal-plain to continental shelf and shelf to slope transitions. To ensure that our simulated drainage basin produces a point-source for sediment input to the marine domain we imposed a longitudinal topographic low in the middle of the model.

github-actions[bot] commented 6 months ago

Thank you for submitting. Please check the output below, and fix any errors, etc.

Creator/Contributor Creator/contributor is Sara Polanco (https://orcid.org/0000-0002-1270-4377)

Model Repository Slug Model repo will be created with name polanco-2023-deltas

Field of Research (FoR) Codes 3706: Geophysics 370604: Geodynamics

License CC-BY-4.0

Model category

Associated Publication Found publication: The flexural isostatic response of climatically driven sea-level changes on continental-scale deltas.

Title Title taken from associated publication The flexural isostatic response of climatically driven sea-level changes on continental-scale deltas

Description Description taken from associated publication abstract Abstract. The interplay between climate-forced sea-level change, sediment erosion and deposition, and flexural adjustments in deep time on passive margin deltas remains poorly understood. We performed a series of conceptual simulations to investigate flexural isostatic responses to high-frequency fluctuations in water and sediment load associated with climatically driven sea-level changes. We model a large drainage basin that discharges to a continental margin to generate a deltaic depocenter, then prescribe synthetic and climatic-driven sea-level curves of different frequencies to assess flexural response. Results show that flexural isostatic adjustments are bidirectional over 100–1000 kyr timescales and are in sync with the magnitude, frequency, and direction of sea-level fluctuations, and that isostatic adjustments play an important role in driving along-strike and cross-shelf river-mouth migration and sediment accumulation. Our findings demonstrate that climate-forced sea-level changes produce a feedback mechanism that results in self-sustaining creation of accommodation into which sediment is deposited and plays a major role in delta morphology and stratigraphic architecture.

Model authors Author list taken from associated publication

The following author(s) were found successfully:

Scientific keywords No keywords given Funder Funder list taken from associated publication

The following funder(s) were found successfully:

Software Framework DOI/URI Found software: badlands-model/pyBadlands: stable release version 2.0.0.

Software Repository https://github.com/badlands-model/badlands

Software Name Badlands

Software Framework Authors Author list taken from software DOI record

The following author(s) were found successfully:

Software & algorithm keywords No keywords given

Computer URI/DOI No URI/DOI given

Landing page image

Animation

Graphic abstract

Model setup figure

Model setup description The initial configuration of the modeling domain resembles the topography of a natural source-to-sink system with 3400 m elevation in the headwaters, a length of 4500 km, a downstream-decreasing fluvial channel slope, and successive inflections in gradient associated with the coastal-plain to continental shelf and shelf to slope transitions. To ensure that our simulated drainage basin produces a point-source for sediment input to the marine domain we imposed a longitudinal topographic low in the middle of the model.

When you have finished adding file descriptions and fixing any identified errors, please add a 'Review Requested' label to this issue.