Skip to content
Science Astronomy Atmosphere

Vol. Science · Astronomy · Thermal escape

Which gases
can a world keep?

A gas molecule is always moving. The most probable speed in a Maxwell distribution is √(2kT/m). The mean speed is √(8kT/(π m)). Leaving the world takes vesc = √(2GM/r), the same escape speed as the escape desk. A classroom rule of thumb says a gas is retained over geologic time if escape speed exceeds about six times that mean speed. It is an approximation. The Jeans parameter is the sharper number: λ = vesc² / vmp² = GMm / (kT r). Hot, light gases leak. Cold, heavy gases stay. The temperature that belongs in the formula is the exobase, or the upper atmosphere, not the weather at the surface. How much sunlight a world receives is the habitable zone. That equilibrium temperature is a different number.

Classroom schematic. The six-times line is the sorting rule in Catling and Zahnle’s 2009 picture, not a measured lifetime. Thermal Jeans escape is only one leak. Solar-wind sputtering, photochemical escape, hydrodynamic escape, and impact erosion are named below and are not calculated. A gas above the line can still be missing if it was never supplied. A gas under the line can still be present if ice or chemistry keeps replacing it. Not a climate model, not an escape-rate model, and not a claim that a world is habitable.

Interactive · Escape speed and ten gases

Log temperature · log escape speed · a gas line is six times the mean thermal speed

  • Other worlds
  • Selected

Worlds · fact-sheet GM and radius · cited upper-atmosphere temperature

K

Ten gases · this world

Why Titan has air and the Moon does not

Similar escape speeds. Different temperatures.

Titan’s surface escape speed on this page is 2.641 km/s. The Moon’s is 2.375 km/s, and the Moon Fact Sheet prints 2.38 km/s. Those are close. The upper atmospheres are not. Titan’s exobase in the cited table is about 1500 km up, where escape has fallen to 2.099 km/s, and the temperature used here is 150 K. Nitrogen’s mean speed there is 0.337 km/s. Escape is 6.24 times that mean speed, just over the rough line. λ is 49.5. Methane is lighter, and on this button it sits under the line. The atmosphere that Cassini measured is mostly nitrogen. Methane is the minor gas that photochemistry and escape both eat, and something has to replace it.

The Moon has no thick-atmosphere exobase. The fact sheet’s black-body temperature is 270.4 K, and the equatorial day runs from 95 K to 390 K. At 270.4 K, nitrogen’s mean speed is 0.452 km/s and escape is only 5.25 times that. λ is 35.1. That is under six. Carbon dioxide and argon sit just over the line at 270.4 K, and the hot end of the fact-sheet range pulls them back toward it. The entire lunar atmosphere is about 25,000 kg. There is no cold, massive nitrogen column. The solar wind reaches the surface. Sputtering and a missing supply finish what the thermal tail starts.

Pluto is the caution. New Horizons found an upper atmosphere near 65–68 K, colder than the models expected, with the exobase near 1710 km. At 65 K this desk’s nitrogen ratio is 3.50 and λ is 15.6, under the rough line, and the escape speed there is 0.775 km/s. Pluto still has an atmosphere. Nitrogen ice resupplies it, and λ of about 16 is a slow Jeans leak, not a hydrodynamic wind. Gladstone and colleagues wrote that the cold upper atmosphere shuts off the enhanced escape those models had expected. The six-times line does not know about resupply.

What this means

The Earth button is the sanity check. Surface escape, from the fact sheet’s GM and volumetric mean radius, is 11.186 km/s. About 11.2 km/s. At 500 km and 1000 K the Jeans escape speed is 10.771 km/s. Hydrogen’s mean speed is 4.583 km/s, a ratio of 2.35, and λ is 7.03. Catling and Kasting’s chapter gets λ about 7 for atomic hydrogen at 1000 K at the exobase. Nitrogen’s ratio is 12.4 and λ is 195. Oxygen’s ratio is 13.2 and λ is 223. Hydrogen is in the thermal tail. Nitrogen and oxygen are not.

Six times the mean speed is a rule of thumb. Catling and Zahnle, Scientific American, 2009: Jeans escape is considered important if the mean thermal velocity at the exobase exceeds about a sixth of the escape speed. Their figure plots that comparison. Catling and Kasting say the same thing as “average speed,” and their schematic draws root-mean-square lines. Root-mean-square speed is √(3kT/m), a bit faster than the mean. This page uses the mean, √(8kT/(π m)), because that is the speed the six-times sentence names. Six mean speeds is λ of about 45.8, because λ divides by the most probable speed, not the mean. A world can sit near the line either way. Treat the line as a sort, not a clock.

Other leaks are left out on purpose. Jeans escape is the hot tail of a Maxwell distribution above the exobase. Hydrodynamic escape is a wind: the air flows outward in bulk when heating is strong and λ is only a few. Photochemical escape is a molecule split by sunlight into atoms that are already fast enough. Sputtering is the solar wind, or a magnetosphere, knocking atoms off. Impact erosion is a collision blowing the air above a patch of the world into space. Charge exchange and the polar wind matter for Earth’s hydrogen and helium. Catling and Zahnle say Jeans escape is only about 30 percent of Earth’s hydrogen loss, and almost none of the helium. Helium on the Earth button is under the six-times line. The thermal tail is real and thin. The polar wind does most of the helium leaving.

Uranus is the hot giant. Jupiter, Saturn, and Neptune hold atomic hydrogen at the temperatures on their buttons. Uranus, at the table’s 850 K, does not: the hydrogen ratio is 4.63. Molecular hydrogen, the gas the atmosphere is made of, is at 6.55, just over the line. A hot thermosphere can leak atoms and still keep the molecules. The energy that keeps the giant-planet thermospheres hotter than sunlight alone would make them is a separate problem. This page does not solve it. It only uses the cited temperature.

Literacy · the speeds

Escape speed
vesc = √(2GM/r). The surface figure uses the fact-sheet volumetric radius, so Earth reads 11.186 km/s. The Jeans figure adds a cited exobase altitude. For a gas giant that altitude is added to the equatorial 1-bar radius, because that is the radius the printed escape speed belongs to. Direction does not enter. Mass of the molecule does not enter. The escape desk draws the orbit that goes with this speed.
Two thermal speeds
Most probable speed vmp = √(2kT/m). Mean speed vmean = √(8kT/(π m)), which is √(4/π) ≈ 1.128 times the most probable speed. Root-mean-square speed is √(3kT/m). The six-times rule on this page uses the mean. λ uses the most probable speed, so that λ equals GMm/(kT r).
Jeans parameter
λ = vesc² / vmp² = GMm / (kT r). Gravitational energy over kT. Large λ means the escape speed sits far out on the Maxwell tail, and the leak is slow. Catling and Kasting, following Chamberlain, define it this way. Hydrodynamic escape becomes the better description when λ is only a few.
The six-times line
A gas is marked retained when vesc is at least six times vmean. The chart draws that boundary: each gas line is v = 6 √(8kT/(π m)). A world above a line keeps that gas, by the approximation. Catling and Zahnle draw the same test the other way up, with the dot at one-sixth of escape speed and the lines as the thermal speeds. Dividing every height on this chart by six is their picture.
Exobase
The altitude where the air becomes thin enough that a fast upward molecule is unlikely to hit another one. Below it, collisions share the energy. Above it, a molecule on an escape trajectory leaves. The temperature in the formula is the temperature there. Mercury and the Moon have surface-bounded exospheres, so this desk uses a surface temperature and adds no altitude.
What the rule leaves out
Supply, cold traps, chemistry, magnetic fields, and the four non-thermal paths named above. Titan’s nitrogen is just over the line and the column is huge. The Moon’s nitrogen is just under the line and the column is about 25,000 kg. Pluto’s nitrogen is under the line and the ice keeps putting it back. Equilibrium temperature on the habitable zone desk is the temperature of a bare surface sharing sunlight over the whole globe. It is not this exobase temperature. Earth’s no-greenhouse equilibrium temperature is near 255 K. The exobase used here is 1000 K.

Sources · fact sheets, CODATA, and the papers

Cited, not invented

Classroom picture of thermal escape. Escape speed from fact-sheet GM and radius. Thermal speeds from CODATA k and u and IUPAC abridged atomic weights. The six-times line is Catling and Zahnle’s approximation. λ is GMm/(kT r). Not an escape rate, and not a habitability verdict. Earthrise preview: NASA / Bill Anders (public domain).

Keep going

The speed

Escape

Where √(2GM/r) comes from, and the circular orbit that is slower by √2. Earth’s surface escape is the same 11.186 km/s.

The sunlight

Habitable zone

Flux and equilibrium temperature. That temperature is not the exobase temperature on this page.

The layers

Atmosphere

Earth’s air, from the ground up. The exobase is the top of that stack, and it is hot.

The glow

Blackbody

The same k, in a different formula. A world’s glow is not its exobase temperature.

The collision

Impacts

One of the non-thermal ways an atmosphere can be blown off. A different desk. Not a hazard assessment.

Neighborhood

Solar map

Where these worlds sit. The temperatures on this page are not the map’s.