ATS coastal modeling: a brief introduction
David Moulton, Yu Zhang, Joel Rowland, Daniil Svyatsky
Los Alamos National Laboratory
Coastal wetland restoration kickoff meeting
April 15th, 2022
Advanced Terrestrial Simulator (ATS): A Multiphysics Model
Builds on several DOE open-source tools
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Surface Processes:
Groundwater:
Land Model/Processes:
Watershed Workflow
A Python package and collection of Jupyter Notebooks
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Soil Type
Land Cover
Elevation
ATS coastal modeling configuration
Los Alamos National Laboratory
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4/15/22
ATS hydro-eco-geomorphologic module
Hydrodynamics
-Diffusive-wave scheme
Subsurface flow
-Density-dependent 3D groundwater flow
Veg dynamics
-Empirical vegetation equation
Sed erosion/deposition
-Mineral sediment settling/trapping
-Erosion due to tidal current
-Organic soil production
Improved representation of hydrodynamics on complex terrain
Distance from the shoreline (m)
Surface elevation (m)
Topographic change in 30 yrs driven by integrated coastal processes
Hourly scale
Yearly scale
Distance from the shoreline (m)
Surface elevation (m)
Saltwater intrusion
-20
Surface elevation (m)
Coastal hydrologic modeling across scales
Transect scale modeling
Improved representation of hydrodynamics on complex terrain
Distance from the shoreline (m)
Surface elevation (m)
Density-depended flow simulation for understanding saltwater intrusion
Density-depended flow simulation for understanding saltwater intrusion
Density-depended flow simulation for understanding saltwater intrusion
0 1000 2000 3000
-50
-50
Distance from the shoreline (m)
Soil thickness (m)
Watershed scale modeling
Regional scale modeling
Soil types (30 m)
Land Cover (30 m)
DEM (10m)
Harbeson site (93.15 km2) HUC-12 #020403030102
Hydrologic response to rainfall storm
LANL-LDRD project
Surface ponding water distribution driven by ELM simulated P-ET
Surface flow
Subsurface flow
DOE-ICoM project
ATS Geochemistry configuration
Alquimia: A geochemistry interface library
Reactive transport modeling
Captures surface-subsurface hydrologic dynamics and their effect on mineral weathering and chemical exports at the watershed scale.
Simulated water depth Copper Creek watershed
Simulated dissolved inorganic carbon in the groundwater Copper Creek watershed
Xu et al., �in prep.
ELM-PFLOTRAN
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Schematic of coupled carbon–nitrogen–phosphorus dynamics in vegetation and soil as represented in ELM
ELM-PFLOTRAN coupling has been explored by Ben Sulman in NGEE-Arctic and his DOE Early Career award.