The technology

Air-breathing electric propulsion.

Turning VLEO's primary challenge into its primary resource. The atmosphere that pulls satellites down becomes the propellant that keeps them up.

Intake · ActivePropellant · AtmosphericDuration · Hardware-limited
Why VLEO

Closer is better — until drag gets a vote.

Lead with the physics: nearer means sharper data, lower latency, and less radiation. Then meet the constraint that defines the whole problem — atmospheric drag.

Altitude
247km
VLEO
200 km · VLEO800 km · LEO
Resolution
2.4×
Signal
5.9×
Latency
12 ms
Radiation
Low
De-orbit
Weeks
vs 600 km
baseline

Illustrative — physics-based approximations referenced to a 600 km baseline.

At 200 km there is still enough residual atmosphere to slow a satellite measurably. Left unchecked, drag de-orbits a spacecraft in weeks — the very property that makes VLEO self-cleaning is what makes it hard to stay in.

The unlock isn't fighting the atmosphere. It's using it.

The problem

Why conventional propulsion fails at 200 km.

Chemical propulsion

Counteracting continuous drag would need impractical volumes of fuel. Mass budget collapses.

Electric propulsion

Far more efficient — but still carries a finite onboard propellant tank. GOCE ran dry after 4+ years; Tsubame after ~111 days.

How it works

Atmosphere in. Continuous thrust out.

Air-breathing electric propulsion collects the residual atmosphere and uses it as propellant — no tank to run dry.

01

Atmospheric intake

Residual air at 200 km enters the forward intake instead of dragging the satellite down.

02

Collection & compression

Sparse molecules are captured and concentrated into a usable propellant stream.

03

Ionization

The collected gas is ionized — no onboard fuel tank required.

04

Acceleration & thrust

Ions are accelerated to produce continuous thrust that offsets drag.

Mission duration limited only by hardware longevity — not propellant.

Precedent

Governments proved it. We're commercialising it.

2009–2013

ESA GOCE

Flew at ~255 km for 4+ years on ion propulsion until propellant ran out — proving sustained VLEO is possible.

2017–2019

JAXA Tsubame

Demonstrated super-low-altitude operations and air-breathing concepts before decaying after ~111 days.

2025–

Albedo Clarity

Commercial VLEO Earth observation at ~275 km — proving 10 cm-class imagery is achievable today.

The congestion crisis

The orbit above is filling up.

Tracked objects in LEO keep climbing, collision-avoidance manoeuvres are escalating, and the Kessler trajectory is real. The push toward VLEO is structural.

Tracked objects in LEO
thousands
016324864201020152019202220242027*

* projected · illustrative trend

The full comparison

VLEO vs traditional LEO, quantified.

The most data-dense view of the thesis. Every figure is physics-based and referenced; treat them as engineering estimates, not guarantees.

Metric
VLEO · 200 km
LEO · 600–800 km
Ground resolution (same optics)
3× sharper
baseline

Aperture scales linearly with altitude — a 0.5 m mission needs a 0.22 m aperture at 200 km vs 0.88 m at 800 km.

End-to-end latency
~10 ms
~30 ms

Shorter slant range cuts propagation delay toward the sub-30 ms competitive mark.

Signal strength (same EIRP)
9× stronger
baseline

Free-space path loss falls with the inverse square of range.

Radiation exposure
~10× lower
baseline

Below the inner Van Allen belt — less shielding, COTS-friendly electronics.

Natural de-orbit
Weeks
Decades–centuries

Atmospheric drag clears the orbit without disposal manoeuvres.

Your mission

See how these advantages apply to your mission.