Free · Physics models

Ideal Downhill Slide and Level Runout

Model acceleration from rest on a straight snowy incline followed by level frictional stopping.

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How to use this calculator

  1. Enter the known values in the units shown. Results update as you type.
  2. Where results are editable, change one to solve backwards. Lock a value to hold it fixed.
  3. Use the worked example to check the method. Reset restores the starting fields.

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Formula and method

With coefficient 0.1, level runout deceleration is −0.980665 m/s²; a 30-degree slope over two seconds gives downhill speed about 8.11 m/s.

Resolve gravity down the slope and friction uphill; integrate constant acceleration, then use kinetic energy for level runout.

Worked example

Enter these known values and leave the other values blank.

Type of sled
Waxed wood on wet snow
Sliding time
2 sec
Hill length
8.108 m
Hill height
4.054 m
How fast will the sled go at the bottom?
29.19 km/h
Distance to stop
33.52 m
Time to stop
8.268 sec

Assumptions and limitations

  • The model starts from rest, uses constant kinetic friction and transitions instantly onto level ground. The selected slope must accelerate the sled downhill.
  • Friction choices are approximate captured surface scenarios, not measured site properties. Static starting friction, bumps, changing snow and air drag are omitted.
  • The speed and distance tiers are numerical context only; they do not determine whether a real slope or runout is safe.
  • Clear the unknown numerical field before using a supported inverse; selection controls retain their captured branches.

Common questions

What assumptions matter for this model?

The model starts from rest, uses constant kinetic friction and transitions instantly onto level ground. The selected slope must accelerate the sled downhill.

What does this model leave out?

The speed and distance tiers are numerical context only; they do not determine whether a real slope or runout is safe.

References

Model requirements: The chosen incline must give positive downhill acceleration from rest. Authored accessible explanations preserve each captured diagram mode and its geometric relationships.

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