Carry the computation · Engineering note
A minimal computing workflow reaches saved output
The reported test completes the configured build, submission and time-stepping path and records restart output.
Explore the simulation ↗A CONNECTED PROJECT
Many physical worlds.
A common foundation.
Atmosphere, impact and subsurface investigations share the work of configuring models, inspecting outputs and checking interpretations.
These are related research capabilities, with distinct assumptions and open questions.
THE CONNECTED WORK
Build the execution path
Carry the computation · Engineering note
A scene script produces a saved test movie
The Manim setup produces a playable movie and retains its source, establishing the rendering path.
Explore the simulation ↗Carry the computation · Engineering note
A fair compute choice still needs a matched benchmark
The research note identifies workload constraints; it provides no measured runtime or cost comparison.
Explore the simulation ↗THE CONNECTED WORK
Create and compare model worlds
Understand the physics
Saved diagnostics trace a growing atmospheric disturbance
Saved pressure, ascent, cloud-water and rainfall diagnostics connect disturbance growth to the evolving model weather.
Explore the simulation ↗Carry the computation
Model weather leaves a reusable record for further analysis
Saved time series and jet diagnostics preserve the atmospheric evolution for checks beyond the finished film.
Explore the simulation ↗Vary the conditions
Controlled ocean setups separate added energy from warming
Comparing carbon-dioxide changes with fixed and warming oceans separates the energy and temperature responses within an idealized model.
Explore the simulation ↗Carry the computation
The early impact pressure is close to an analytical reference
The early-impact model produces a peak shock pressure close to the analytical reference, while the final crater remains outside the calculation.
Explore the simulation ↗THE CONNECTED WORK
Generate observations. Test the interpretation.
Create observations
Different underground models fit the same synthetic magnetic survey
Smooth and compact inversions fit the signal but place magnetic susceptibility differently, leaving the underground structure unresolved.
Explore the simulation ↗Create observations
A close gravity fit leaves depth unresolved
Recovered mass is close to the synthetic target, but a near-target data fit does not recover the bed-depth geometry.
Explore the simulation ↗THE CONNECTED WORK
Recognize where the result is not ready.
Carry the computation · Unresolved
Mass imbalance prevents an accepted eductor result
The later run retains substantial mass imbalance and unacceptable residuals, leaving the flow calculation unresolved.
Explore the simulation ↗