Air resistance and terminal velocity
Thrown at 30 m/s and 45°, a ball would land 92 m away in a vacuum; with air pushing back, our model ball lands at about 60 m.
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Air pushes back
Put your hand out of a car window and you feel air resistance, also called drag. It always points against the motion, and it grows quickly with speed. For a ball, a bike or a car moving at ordinary speeds through air, OpenStax College Physics gives the drag force as FD = ½ C ρ A v². Here ρ is the density of the air, A is the area facing the flow, C is a drag coefficient that depends on the shape, and v is the speed. Wind tunnel tests give C about 0.45 for a sphere, 0.28 for a streamlined family car and about 1.0 for a skydiver lying flat.
The v² is the important part. Double the speed and the drag becomes four times larger. A slow ball hardly notices the air; a fast one is pushed hard. That is why air resistance matters little for a gently tossed beanbag and a great deal for a hit baseball or a fast car, where OpenStax notes that more than half the engine’s power at highway speed goes into pushing air aside.
A lopsided path
Launch the model ball in the lab at 30 m/s and 45° with air resistance on. Without air it would fly 91.7 m. With air it lands at about 60.0 m, a third shorter. The path is no longer a symmetric parabola. It climbs at a steep angle and then drops more steeply than it rose, because the ball has lost much of its horizontal speed by the time it comes down. The highest point also moves closer to the landing spot.
Now switch to Mars. Mars has air, but NASA puts its surface density at about 0.016 kg/m³, compared with about 1.2 kg/m³ on Earth, so the drag is roughly 75 times weaker. The kept paths for Mars with and without air almost overlap. On the Moon there is essentially no air at all, and the lab draws exactly the same path whether the switch is on or off.
Terminal velocity
Think about a skydiver jumping from a plane. At first the speed is low, so drag is small and the skydiver accelerates at almost g. As the speed rises, drag grows, and the net downward force shrinks. Eventually drag equals weight. The forces balance, the acceleration drops to zero and the speed stops increasing. This top speed is the terminal velocity. Setting ½ C ρ A v² equal to m g gives vt = √(2 m g ÷ ρ C A).
OpenStax works two examples. A 75 kg skydiver diving head first, with a frontal area of about 0.18 m² and C ≈ 0.70, reaches about 98 m/s, roughly 350 km/h. An 85 kg skydiver spread flat, with about 0.70 m² of area and C ≈ 1.0, reaches only about 44 m/s. Our model ball in the lab has a terminal velocity of about 35 m/s, which is why fast launches lose so much range. Opening a parachute increases A and C enormously, and the terminal velocity drops to a speed you can land at.
- Drag F = ½ C ρ A v² grows with the square of speed.
- Air shortens the range and makes the path lopsided.
- Mars has thin air; the Moon has almost none.
- At terminal velocity drag equals weight and the speed stops rising.
- You double your speed through air. The drag force becomes about…
- 2 times
- 4 times
- half
- Which way does air resistance point?
- Always down
- Against the motion
- Along the motion
- With air, the ball’s path compared with the no-air parabola is…
- longer and symmetric
- shorter and steeper on the way down
- exactly the same
- On the Moon, switching air resistance on in the lab…
- shortens the range a lot
- changes nothing
- makes the ball go further
- Without air, how far does a ball launched at 30 m/s and 45° go on Earth, in metres? (one decimal)
- At terminal velocity, the net force on a falling skydiver is…
- equal to the weight
- zero
- upward
- OpenStax’s head-first skydiver reaches about 98 m/s. About how many km/h is that? (whole number)
- Why does a spread-flat skydiver fall slower than a head-first one?
- Less weight
- More area and a larger drag coefficient
- Thinner air
- Roughly how many times thinner is the air at the surface of Mars than on Earth?
- 2 times
- About 75 times
- About 1,000 times
- Opening a parachute lowers the terminal velocity mainly by…
- reducing the mass
- increasing area and drag coefficient
- reducing gravity
Sources for this course (12)
- OpenStax College Physics 2e, chapters 2 (Kinematics)
- 3.4 (Projectile motion)
- 5.2 (Drag forces) (openstax.org/books/college-physics-2e)
- NIST CODATA standard acceleration of gravity g_n = 9.80665 m/s² exact (physics.nist.gov/cgi-bin/cuu/Value?gn)
- NASA Moon Fact Sheet (surface gravity 1.62 m/s², nssdc.gsfc.nasa.gov/planetary/factsheet/moonfact.html)
- NASA Mars Fact Sheet (3.69 m/s² equator, 3.73 m/s² pole, surface air density about 0.016 kg/m³, nssdc.gsfc.nasa.gov/planetary/factsheet/marsfact.html)
- NASA, The Apollo 15 Hammer-Feather Drop (science.nasa.gov/resource/the-apollo-15-hammer-feather-drop, quoting NASA SP-289)
- Galileo, Two New Sciences (1638)
- inclined-plane account via PBS LearningMedia/NOVA "Galileo's Inclined Plane"
- long-jump take-off angle about 21°: Linthorne, Guzman and Bridgett, Journal of Sports Sciences 23(7)
- 2005, and Linthorne, Biomechanics of the long jump
- OpenStax College Physics 2e 17.2 (sound 343 m/s at 20 °C).
Checked: 2026-10-17