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It is well established that coupling and s … 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 Planetary Evolution, 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. Participants will be able to participate in live exercises through new online computing resources hosted by the Computational Infrastructure for Geodynamics (CIG).onal Infrastructure for Geodynamics (CIG). +
John.naliboff@nmt.edu +
CSDMS 2025: Exploring Earth's Surface with Models, Data & AI +
New Mexico Institute of Mining and Technology +
Naliboff +
Clinic +
New Mexico +
Coupling models of lithospheric deformation and surface processes with the Advanced Solver for Planetary Evolution, Convection, and Tectonics (ASPECT) - Part 1 +
United States +
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13:49:28, 24 January 2025 +
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22:34:03, 11 June 2025 +
