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Demonstration Project: Leveraging Output from a High-Resolution 3D Hydrodynamic-Sediment Transport Model to Run Landlab's Simple Submarine Diffuser

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Type:	Resource
Storage:	The size of this resource is 1.4 MB
Created:	Mar 13, 2025 at 9:27 p.m.
Last updated:	Mar 14, 2025 at 1:45 p.m.
Published date:	Mar 14, 2025 at 1:46 p.m.
DOI:	10.4211/hs.f06cc2e465434767839d507872a7c62f
Citation:	See how to cite this resource

Sharing Status:	Published
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Abstract

The purpose of this demonstration project is to show how to (a) use the ROMS (Regional Ocean Modeling System) data component to estimate hydrodynamic and sedimentary information for a marine environment based on output from a high-resolution 3D hydrodynamic-sediment transport model, and (b) use this information to run the Simple Submarine Diffuser from Landlab to disperse sediment on continental shelves. This use case is for the Beaufort Sea shelf, Alaska, USA. This notebook focuses on providing an example of how to use the data component and other tools; future work will include considering best practices for linking short-term dynamics with long-term shelf evolution.

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:

WGS 84 EPSG:4326

Coordinate Units:

Decimal degrees

Place/Area Name:

Alaskan Beaufort Sea shelf

Longitude

-150.2655°

Latitude

70.5040°

Temporal

Start Date:
End Date:

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Credits

Funding Agencies

This resource was created using funding from the following sources:

Agency Name	Award Title	Award Number
U.S. National Science Foundation	Collaborative Research: Facility: CSDMS: Engaging a thriving community of practice in Earth-surface dynamics	2148762

How to Cite

Undzis, B., J. Moriarty (2025). Demonstration Project: Leveraging Output from a High-Resolution 3D Hydrodynamic-Sediment Transport Model to Run Landlab's Simple Submarine Diffuser, HydroShare, https://doi.org/10.4211/hs.f06cc2e465434767839d507872a7c62f

This resource is shared under the Creative Commons Attribution CC BY.

http://creativecommons.org/licenses/by/4.0/

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