An interactive view of existing simulation results

Change the scenario.
See what the model did.

Explore two studies by moving a control. Each setting reveals an output already produced in the original session, with its assumptions and sources alongside it.

Explore recorded results · 4 FDS scenarios

Change the slope. Inspect the flame.

Switch between the original simulated temperature and flow fields. Watch how the plume lies closer to the fuel in the steeper cases.

Display a field
Gas temperature and the 300 °C flame contour

A viewport into the unchanged original figure. Coordinates follow the model’s slope-aligned frame. The selected snapshots are from different model times, not a synchronized animation.

Recorded spread rate1.79 cm/sFit after the igniter was switched off
Reported mean flame tilt19.2°Across the source’s sampled frames

Reference fuel and zero wind. Steep cases use a longer fuel bed and earlier igniter cutoff; this is not a perfectly isolated single-parameter experiment. Absolute spread rates are unvalidated and the steep cases remain limited by domain size.

Explore recorded results · 6 completed model runs

Turn up the CO₂. What changes?

Choose a concentration and an experiment. The display switches between the actual saved results, with the physical assumptions kept visible.

Which question are we asking?
Temperature rise relative to 280 ppm (K)280 ppm560 ppm1,120 ppm

Dots are the three saved runs. The dashed connector is a visual guide; intermediate concentrations were not simulated here.

Warming vs 280 ppm+1.80 KSlab-ocean equilibrium comparison
Mean model surface temperature17.66 °CYears 9–12 of a 12-year model run

This is an idealized aquaplanet. The slab ocean is 30 m deep; there is no realistic land, sea ice, seasons or ocean circulation. These are conditional model responses, not an Earth climate-sensitivity estimate.

Follow the result back to the study

Each control selects a saved model result. Open the study to inspect its scientific question, inputs, methods, and interpretation.

Read the fire case → · Read the climate case →