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(Created page with "{{Presenters temp |CSDMS meeting event title=CSDMS 2023: Patterns and Processes Across Scales |CSDMS meeting event year=2023 |CSDMS meeting presentation type=Clinic |CSDMS meeting first name=John |CSDMS meeting last name=Naliboff |CSDMS meeting institute=New Mexico Institute of Mining and Technology |Country member=United States |CSDMS meeting state=New Mexico |CSDMS meeting email address=John.naliboff@nmt.edu |CSDMS meeting title presentation=Coupling models of lithosph...")
 
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{{Presenters presentation
{{Presenters presentation
|CSDMS meeting abstract presentation=It is well established that coupling and strong feedbacks may occur between solid Earth deformation and surface processes across a wide range of spatial and temporal scales. As both systems on their own encapsulate highly complex and nonlinear processes, fully-coupled simulations require advanced numerical techniques and a flexible platform to explore a wide range of scenarios. Here, we will demonstrate how the Advanced Solver for Problems in Earth's Convection and Tectonics (ASPECT) can be coupled with Fastscape to examine feedbacks between lithospheric deformation and landscape evolution. The clinic will cover the fundamental equations being solved, how to design coupled simulations in ASPECT, and examples of coupled continental extension and landscape evolution.
|CSDMS meeting abstract presentation=It is well established that coupling and strong feedbacks may occur between solid Earth deformation and surface processes across a wide range of spatial and temporal scales. As both systems on their own encapsulate highly complex and nonlinear processes, fully-coupled simulations require advanced numerical techniques and a flexible platform to explore a multitude of scenarios. Here, we will demonstrate how the Advanced Solver for Problems in Earth's Convection and Tectonics (ASPECT) can be coupled with FastScape to examine feedbacks between lithospheric deformation and landscape evolution. The clinic will cover the fundamental equations being solved, how to design coupled simulations in ASPECT, and examples of coupled continental extension and landscape evolution.
|CSDMS meeting youtube code=0
|CSDMS meeting youtube code=0
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|CSDMS meeting participants=0

Revision as of 15:14, 7 December 2022

CSDMS 2023: Patterns and Processes Across Scales


Coupling models of lithospheric deformation and surface processes with the Advanced Solver for Problems in Earth's Convection and Tectonics (ASPECT)



John Naliboff

New Mexico Institute of Mining and Technology, United States
John.naliboff@nmt.edu


Abstract
It is well established that coupling and strong feedbacks may occur between solid Earth deformation and surface processes across a wide range of spatial and temporal scales. As both systems on their own encapsulate highly complex and nonlinear processes, fully-coupled simulations require advanced numerical techniques and a flexible platform to explore a multitude of scenarios. Here, we will demonstrate how the Advanced Solver for Problems in Earth's Convection and Tectonics (ASPECT) can be coupled with FastScape to examine feedbacks between lithospheric deformation and landscape evolution. The clinic will cover the fundamental equations being solved, how to design coupled simulations in ASPECT, and examples of coupled continental extension and landscape evolution.

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Of interest for:
  • Terrestrial Working Group
  • Geodynamics Focus Research Group