<p>What determines how long a planet will keep its atmosphere is the strength of the planet's gravity versus the random thermal motion of the molecules in its atmosphere.  </p>

<p>The atmosphere is a gas, and all gasses have molecules that move around with velocities that are dependent on the temperature.  High-temperature gasses move faster, and low-temperature gasses move more slowly.  Each molecule of gas will have a velocity $v_{\text{gas}, \text{average}}=\sqrt{\frac{3k_BT}{m_{\text{gas}}}}$.</p>

<p>In addition, each individual molecule is pulled to the Earth by gravity.  Heavier gasses, such as water, carbon dioxide, and oxygen, are pulled more than lighter gasses, such as hydrogen and helium.  The escape velocity of the planet is given by $v_{\text{escape}}=\sqrt{\frac{2GM_{\text{planet}}}{R_{\text{planet}}}}$.</p>

<p>If a gas molecule has a high enough thermal energy, then if it is at the top of the atmosphere, it could fly off into space, the thermal motion overcoming gravity's pull.  The lighter it is, the less thermal energy it needs to have.  Of course, this all depends on probability and statistics, but, in general, if $v_{\text{gas}}\ge0.2 \times v_{\text{escape}}$, that species of gas will be reduced to 1/2 its initial amount after 1 billion years.  </p>

<p><a href="https://i.sstatic.net/FnN6w.gif" rel="noreferrer"><img src="https://i.sstatic.net/FnN6w.gif" alt="Here is a flowchart describing whether or not a gas will escape."></a></p>

<p>Solar wind consists of charged particles and high energy photons, which are deflected by a planet's magnetic field.  However, in the case of a planet like Mars, without a magnetic field, the particles interact with the atmosphere.  They tend to split molecules apart, resulting in lighter gasses (a process called "photodissociation").  These gasses, being bound less strongly by gravity, are more free to fly off into space under thermal motion.  As more and more gas leaves the planet, the atmosphere becomes thinner and thinner until, ultimately, only the heavy gasses are left.  In addition, when a molecule is split, the energy imparted to it by the impact may be enough to eject it from the atmosphere (a process called "sputtering").</p>

<p>Planets (and moons) that are closer to the sun are subject to more intense solar radiation, and also have higher atmospheric temperatures.  This is why distant moons, such as Titan, have thick atmospheres of hydrocarbons.  Planets close to the sun, such as Venus, can retain their atmospheres for a variety of reasons.  Firstly, Venus's atmosphere is primarily carbon dioxide, which is much heavier than Hydrogen, and more difficult to split via photodissociation than water.  Planets like Earth also have hydrogeological cycles which can recycle gas from rocks and water back into the atmosphere.</p>

<p>For more information on this, read up on <a href="https://en.wikipedia.org/wiki/Atmospheric_escape" rel="noreferrer">Jeans Escape</a>.  A good set of notes for beginners can be found <a href="http://www.astronomynotes.com/solarsys/s3.htm" rel="noreferrer">here</a>.</p>

CC BY-SA 3.0
2016-10-13T05:30:56.200Z
If you have a formula handy for the relative importance of gravity and distance to the Sun, I'd appreciate it. Titan also has no magnetic field and has lighter molecules, but that is all made up by being further from the Sun (or by continuous out gassing replenishing the atmosphere?)
LocalFluff
CC BY-SA 3.0
2016-10-13T17:26:58.557Z
@LocalFluff That should help you out.  Ultimately the reason Titan has an atmosphere is because it is further away from the sun, and thus cooler.  I don't know how the strength of the solar wind varies with distance, but you could probably calculate the average temperature of a planet based on the flux it receives over its surface.
Phiteros
CC BY-SA 3.0
2016-10-13T18:11:23.673Z
Is it not possible that molecules are getting bigger by solar wind? I thought for example that uv radiation is making O3 out of O2, is this the only molecule which get bigger?
Marijn 
CC BY-SA 3.0
2016-10-13T19:01:42.460Z
O3 is very unstable, so it would decay quickly.  But the main molecule that gets photodissociated is water, which turns into H2 and O2.  The H2 is very, very light, so escapes quite easily.
Phiteros
CC BY-SA 3.0
2016-10-12T21:00:39.773Z
2016-10-22T21:06:46.850Z
2016-10-22T21:06:46.850Z
Phiteros
<p>At least in the case of Mars, the solar wind carries a magnetic field by the planet.  In the Martian atmosphere are ionized particles created from interactions with UV light, cosmic rays, etc.  The moving magnetic field creates an electric field that accelerates the ions away from the planet.  This effect was <a href="http://www.nasa.gov/press-release/nasa-mission-reveals-speed-of-solar-wind-stripping-martian-atmosphere" rel="nofollow">very recently measured</a> by the MAVEN spacecraft:</p>

<blockquote>
  <p>MAVEN has been examining how solar wind and ultraviolet light strip
  gas from of the top of the planet's atmosphere. New results indicate
  that the loss is experienced in three different regions of the Red
  Planet: down the "tail," where the solar wind flows behind Mars, above
  the Martian poles in a "polar plume," and from an extended cloud of
  gas surrounding Mars. The science team determined that almost 75
  percent of the escaping ions come from the tail region, and nearly 25
  percent are from the plume region, with just a minor contribution from
  the extended cloud.</p>
</blockquote>

<p>The dominant effect could be different other places.  For instance, the moons of Jupiter have to deal with the dynamo generated from the Jovian magnetic field.  And in a case like Io, the atmospheric stripping doesn't happen as quickly as expected because apparently every time Io goes behind Jupiter and loses sunlight, its atmosphere <a href="http://arstechnica.com/science/2016/08/jupiters-moon-io-loses-its-atmosphere-when-eclipsed/" rel="nofollow">condenses out and falls to the surface</a>!</p>

CC BY-SA 3.0
2016-10-13T10:20:53.003Z
final sentence ... "whoa!"
Fattie
CC BY-SA 3.0
2016-10-12T22:01:07.880Z
2016-10-12T22:01:07.880Z
Dave
<p>It is said that because Mars doesn't have a magnetic field its atmosphere disappeared, but how can solar wind cause that?</p>

<p>That the protons and electrons can changes molecules in an atmosphere I can understand, but how can solar wind cause molecules to escape from gravity?</p>

<p>Or is it that the atmosphere didn't escape in outer space but in contrary the molecules became too heavy, so they got solid and were pulled to the planet's surface?</p>

CC BY-SA 3.0
2016-10-13T17:30:40.553Z
Related: http://astronomy.stackexchange.com/questions/639/why-has-venuss-atmosphere-not-been-stripped-away-by-solar-wind
called2voyage
CC BY-SA 4.0
2020-03-22T17:20:58.857Z
It doesn't. See Venus.
AtmosphericPrisonEscape
<planet>
How does the solar wind destroy the atmosphere of a planet lacking a magnetic field?
Marijn 
# How does the solar wind destroy the atmosphere of a planet lacking a magnetic field?

(Asked by: username_0 on 2016-10-12)

It is said that because Mars doesn't have a magnetic field its atmosphere disappeared, but how can solar wind cause that?

That the protons and electrons can changes molecules in an atmosphere I can understand, but how can solar wind cause molecules to escape from gravity?

Or is it that the atmosphere didn't escape in outer space but in contrary the molecules became too heavy, so they got solid and were pulled to the planet's surface?

**Tags:** planet
> **Comments:**
> **username_1**: Related: http://astronomy.stackexchange.com/questions/639/why-has-venuss-atmosphere-not-been-stripped-away-by-solar-wind  
> **username_2**: It doesn't. See Venus.  

---

## 2 answers

### Answer by username_3 on 2016-10-12. Score: 9

What determines how long a planet will keep its atmosphere is the strength of the planet's gravity versus the random thermal motion of the molecules in its atmosphere.

The atmosphere is a gas, and all gasses have molecules that move around with velocities that are dependent on the temperature. High-temperature gasses move faster, and low-temperature gasses move more slowly. Each molecule of gas will have a velocity $v\_{\text{gas}, \text{average}}=\sqrt{\frac{3k\_BT}{m\_{\text{gas}}}}$.

In addition, each individual molecule is pulled to the Earth by gravity. Heavier gasses, such as water, carbon dioxide, and oxygen, are pulled more than lighter gasses, such as hydrogen and helium. The escape velocity of the planet is given by $v\_{\text{escape}}=\sqrt{\frac{2GM\_{\text{planet}}}{R\_{\text{planet}}}}$.

If a gas molecule has a high enough thermal energy, then if it is at the top of the atmosphere, it could fly off into space, the thermal motion overcoming gravity's pull. The lighter it is, the less thermal energy it needs to have. Of course, this all depends on probability and statistics, but, in general, if $v\_{\text{gas}}\ge0.2 \times v\_{\text{escape}}$, that species of gas will be reduced to 1/2 its initial amount after 1 billion years.

[![Here is a flowchart describing whether or not a gas will escape.](https://i.sstatic.net/FnN6w.gif)](https://i.sstatic.net/FnN6w.gif)

Solar wind consists of charged particles and high energy photons, which are deflected by a planet's magnetic field. However, in the case of a planet like Mars, without a magnetic field, the particles interact with the atmosphere. They tend to split molecules apart, resulting in lighter gasses (a process called "photodissociation"). These gasses, being bound less strongly by gravity, are more free to fly off into space under thermal motion. As more and more gas leaves the planet, the atmosphere becomes thinner and thinner until, ultimately, only the heavy gasses are left. In addition, when a molecule is split, the energy imparted to it by the impact may be enough to eject it from the atmosphere (a process called "sputtering").

Planets (and moons) that are closer to the sun are subject to more intense solar radiation, and also have higher atmospheric temperatures. This is why distant moons, such as Titan, have thick atmospheres of hydrocarbons. Planets close to the sun, such as Venus, can retain their atmospheres for a variety of reasons. Firstly, Venus's atmosphere is primarily carbon dioxide, which is much heavier than Hydrogen, and more difficult to split via photodissociation than water. Planets like Earth also have hydrogeological cycles which can recycle gas from rocks and water back into the atmosphere.

For more information on this, read up on [Jeans Escape](https://en.wikipedia.org/wiki/Atmospheric_escape). A good set of notes for beginners can be found [here](http://www.astronomynotes.com/solarsys/s3.htm).

> **Comments:**
> **username_4**: If you have a formula handy for the relative importance of gravity and distance to the Sun, I'd appreciate it. Titan also has no magnetic field and has lighter molecules, but that is all made up by being further from the Sun (or by continuous out gassing replenishing the atmosphere?)  
> **username_3**: @LocalFluff That should help you out.  Ultimately the reason Titan has an atmosphere is because it is further away from the sun, and thus cooler.  I don't know how the strength of the solar wind varies with distance, but you could probably calculate the average temperature of a planet based on the flux it receives over its surface.  
> **username_0**: Is it not possible that molecules are getting bigger by solar wind? I thought for example that uv radiation is making O3 out of O2, is this the only molecule which get bigger?  
> **username_3**: O3 is very unstable, so it would decay quickly.  But the main molecule that gets photodissociated is water, which turns into H2 and O2.  The H2 is very, very light, so escapes quite easily.  

---

### Answer by username_5 on 2016-10-12. Score: 4

At least in the case of Mars, the solar wind carries a magnetic field by the planet. In the Martian atmosphere are ionized particles created from interactions with UV light, cosmic rays, etc. The moving magnetic field creates an electric field that accelerates the ions away from the planet. This effect was [very recently measured](http://www.nasa.gov/press-release/nasa-mission-reveals-speed-of-solar-wind-stripping-martian-atmosphere) by the MAVEN spacecraft:

> MAVEN has been examining how solar wind and ultraviolet light strip
> gas from of the top of the planet's atmosphere. New results indicate
> that the loss is experienced in three different regions of the Red
> Planet: down the "tail," where the solar wind flows behind Mars, above
> the Martian poles in a "polar plume," and from an extended cloud of
> gas surrounding Mars. The science team determined that almost 75
> percent of the escaping ions come from the tail region, and nearly 25
> percent are from the plume region, with just a minor contribution from
> the extended cloud.

The dominant effect could be different other places. For instance, the moons of Jupiter have to deal with the dynamo generated from the Jovian magnetic field. And in a case like Io, the atmospheric stripping doesn't happen as quickly as expected because apparently every time Io goes behind Jupiter and loses sunlight, its atmosphere [condenses out and falls to the surface](http://arstechnica.com/science/2016/08/jupiters-moon-io-loses-its-atmosphere-when-eclipsed/)!

> **Comments:**
> **username_6**: final sentence ... "whoa!"  

---

