Ozone layer discovered on Venus

From the European Space Agency:

ESA finds that Venus has an ozone layer too

Venus Express

ESA’s Venus Express spacecraft has discovered an ozone layer high in the atmosphere of Venus. Comparing its properties with those of the equivalent layers on Earth and Mars will help astronomers refine their searches for life on other planets.

Venus Express made the discovery while watching stars seen right at the edge of the planet set through its atmosphere. Its SPICAV instrument analysed the starlight, looking for the characteristic fingerprints of gases in the atmosphere as they absorbed light at specific wavelengths.

The ozone was detectable because it absorbed some of the ultraviolet from the starlight.

Ozone is a molecule containing three oxygen atoms. According to computer models, the ozone on Venus is formed when sunlight breaks up carbon dioxide molecules, releasing oxygen atoms.

These atoms are then swept around to the nightside of the planet by winds in the atmosphere: they can then combine to form two-atom oxygen molecules, but also sometimes three-atom ozone molecules.

“This detection gives us an important constraint on understanding the chemistry of Venus’ atmosphere,” says Franck Montmessin, who led the research.

It may also offer a useful comparison for searching for life on other worlds.

Ozone has only previously been detected in the atmospheres of Earth and Mars. On Earth, it is of fundamental importance to life because it absorbs much of the Sun’s harmful ultraviolet rays. Not only that, it is thought to have been generated by life itself in the first place.

The build-up of oxygen, and consequently ozone, in Earth’s atmosphere began 2.4 billion years ago. Although the exact reasons for it are not entirely understood, microbes excreting oxygen as a waste gas must have played an important role.

Along with plant life, they continue to do so, constantly replenishing Earth’s oxygen and ozone.

As a result, some astrobiologists have suggested that the simultaneous presence of carbon dioxide, oxygen and ozone in an atmosphere could be used to tell whether there could be life on the planet.

This would allow future telescopes to target planets around other stars and assess their habitability. However, as these new results highlight, the amount of ozone is crucial.

The small amount of ozone in Mars’ atmosphere has not been generated by life. There, it is the result of sunlight breaking up carbon dioxide molecules.

Venus too, now supports this view of a modest ozone build-up by non-biological means. Its ozone layer sits at an altitude of 100 km, about four times higher in the atmosphere than Earth’s and is a hundred to a thousand times less dense.

Theoretical work by astrobiologists suggests that a planet’s ozone concentration must be 20% of Earth’s value before life should be considered as a cause.

These new results support that conclusion because Venus clearly remains below this threshold.

“We can use these new observations to test and refine the scenarios for the detection of life on other worlds,” says Dr Montmessin.

Yet, even if there is no life on Venus, the detection of ozone there brings Venus a step closer to Earth and Mars. All three planets have an ozone layer.

“This ozone detection tells us a lot about the circulation and the chemistry of Venus’ atmosphere,” says Håkan Svedhem, ESA Project Scientist for the Venus Express mission.

“Beyond that, it is yet more evidence of the fundamental similarity between the rocky planets, and shows the importance of studying Venus to understand them all.”

0 0 votes
Article Rating

Discover more from Watts Up With That?

Subscribe to get the latest posts sent to your email.

40 Comments
Inline Feedbacks
View all comments
October 7, 2011 8:33 am

So there is an Atmopshere on Venus with O2?
Incoming high intensity UV can strike that O2 and NOT form O3?
What am I missing here in terms of fundemental science?

REPLY:
Might be some sort of CO2 to O2 to O3 reduction/creation process we don’t understand yet, remember Venus is closer to the sun, so higher energy available for such processes – Anthony

October 7, 2011 8:33 am

Dang, fast typing syndrome. ATMOSPHERE! Not ATMOPSHERE..

Joseph
October 7, 2011 8:38 am

“Might be some sort of CO2 to O2 to O3 reduction/creation process we don’t understand yet, remember Venus is closer to the sun, so higher energy available for such processes – Anthony”
What? I thought those climate boys knew everything there was to know about climate. Was I wrong?

stephen richards
October 7, 2011 8:59 am

Anthony
I think the process is the reverse. 03 to CO² giving of a free radical which can bond with many different elements in the atmosphere. O3 is extremely unstable and therefore decays readily. The energy of radiation doesn’t change at distance. planck’s constant x mù. CME impact, however, could be more energetic.

Pierre
October 7, 2011 9:08 am

Sorry to be off topic but could someone tell me whether the latest Sunspots mean that we are not entering a Maunder Min.
Also when counting sunspots these days and comparing them I assume that scientists are aware of the methods used in the past and account for those limitations in comparing numbers…is that correct?
Sorry for the layman questions…

wobble
October 7, 2011 9:13 am

Of course Venus has an ozone layer. They never used air conditioners and hairspray on Venus.

Captain Fatty
October 7, 2011 9:22 am

Now to look for the holes at the poles…

vboring
October 7, 2011 9:36 am

and we’re somehow destroying it, too.

Sam Hall
October 7, 2011 9:40 am

So, if we put more CO2 in the atmosphere, it will increase our radiation shield and help close the ozone hole?

Gail Combs
October 7, 2011 9:53 am

Pierre says:
October 7, 2011 at 9:08 am
Sorry to be off topic but could someone tell me whether the latest Sunspots mean that we are not entering a Maunder Min….
_____________________________________________________________________
Try layman’s sunspot count and do not miss Dr Lief Svalgaard’s comments about the counting methods at the very bottom of the site. http://www.landscheidt.info/?q=node/50

Jimmy Haigh
October 7, 2011 9:53 am

Luvverly jubbly! Lots of luvverly PhD’s in this I can tell you. Come aahn! Coma aahn!, Roll up, roll up. Two for a paahnd.

Ray
October 7, 2011 10:11 am

Here’s another reason to maintain a high concentration of CO2 in the atmosphere and not try to scrub it all away (which would actually kill all life on the planet, except for some bacteria).

October 7, 2011 10:18 am


Max Hugoson says:
October 7, 2011 at 8:33 am
So there is an Atmopshere on Venus with O2?
Incoming high intensity UV can strike that O2 and NOT form O3?
What am I missing here in terms of fundemental science?
REPLY: Might be some sort of CO2 to O2 to O3 reduction/creation process we don’t understand yet, remember Venus is closer to the sun, so higher energy available for such processes – Anthony

O2 exists in the nightside mesosphere of Venus, caused by recombination of O atoms swept around from the dayside. Having O2 and O in close proximity means that it isn’t a surprise to find O3 there. Formation of O2 by Photodissociation of CO2 has been known in the atmospheres of Venus & Mars for some time. This also explains the existence of CO in the Venusian atmosphere. In our stratosphere 70% of the CO is formed this way with the attendant formation of O which will lead to O3 but the photodissociation of O2 is a bigger contributor here. By the way the UV photons aren’t more energetic at Venus than at Earth, there are just a few more of them.
REPLY: Thanks, but I never suggested they were more energetic just more total energy at the Venusian surface . The inverse square law does hold for light, whether we consider it as a wave or a photon is irrelevant. The inverse square law is dependant on the area over which the power is dissipated. See here; http://hyperphysics.phy-astr.gsu.edu/hbase/vision/isql.html#c1 So whether you treat light like a wave or a photon, there’s more for a given area on Venus. – Anthony

George E. Smith;
October 7, 2011 10:26 am

“”””” Ozone has only previously been detected in the atmospheres of Earth and Mars. On Earth, it is of fundamental importance to life because it absorbs much of the Sun’s harmful ultraviolet rays. Not only that, it is thought to have been generated by life itself in the first place. “””””
Well I would say that the “news” in this story is the amazing revelation that life produces the earth’s ozone.
We have of course the “ozone layer” in the upper atmosphere; izzat the upper troposphere or the stratosphere ? Well it doesn’t matter much; it’s a thin layer that can only exist in a narrow altitude range. So quick quiz; list the ten most well known species of life in that ozone layer.
Then of course we have lower atmospheric ozone that is readily detectable after typical lightning and thunderstorms. Well you don’t even need lightning to get ozone; the sparks that accompany carbon brushes intermittently contacting the copper bars of electric motor commutators are a well known cause of ozone; apparently the lightning (or thunder) scares nearby life forms, causing them to emit ozone; maybe an event commonly known as a f**t .
So life causes ozone; and we never would have guessed that before this paper.
A rather well known chemist has argued that the ozone layer is simply the evidence that Oxygen (O2) is doing its job of protecting us for the far UV from the sun; which breaks up O2 to form atomic oxygen. Atomic oxygen of course is ferociously reactive, and eagerly latches onto a nearby O2 to form Ozone. Apparently (I’m not a chemist) one of the two O-O bonds in Ozone is a rather weak ionic bond, rather than the (apparently) stronger covalent bond; so that ozone is readily destroyed by longer wavelength sunlight (mid spectrum). It would seem that the narrow altitude range of the ozone layer lies high enough for the far (Vaccuum) UV from the sun to survive and break up O2 to form atomic Oxygen, faster than the longer wavelengths can destroy the resultant ozone. So the causative life forms for these processes must live in a very restricted survival range.
Who would have guessed

October 7, 2011 10:47 am

Would not the water bound to sulfur be a more likely source for the 03? Even the ice moons have very tenuous oxygen atmospheres. The source for oxygen in atmospheres appears to be due to the photodissection of H2O, and not a sign of life per se.

October 7, 2011 11:02 am

REPLY: Thanks, but I never suggested they were more energetic just more total energy at the Venusian surface . The inverse square law does hold for light, whether we consider it as a wave or a photon is irrelevant. The inverse square law is dependant on the area over which the power is dissipated. See here; http://hyperphysics.phy-astr.gsu.edu/hbase/vision/isql.html#c1 So whether you treat light like a wave or a photon, there’s more for a given area on Venus. – Anthony
You said: “Might be some sort of CO2 to O2 to O3 reduction/creation process we don’t understand yet, remember Venus is closer to the sun, so higher energy available for such processes”
The point is that there isn’t more energy available for the process, a single photon in the UV does the job (0.116 to 0.195 μm) that’s the same energy here or on Venus. The process is understood
CO2 + hν -> CO + O, when the O makes it round to the dark side it can recombine to form O2 and O3. The whole process takes place at an altitude of 100km above the Venusian surface.
REPLY: Phil you are reading too much into this. I wasn’t suggesting we don’t understand the process of CO2 disassociation, only that we might not understand the process as it exists on Venus in that atmosphere. All we know is that there is ozone there. We don’t know if the process is the same as Earth/Mars or has other attributes. I’m also not arguing the energy of a single photon, just the total energy over area. My short and intended to be helpful comment obviously is turning into a Phil phest. – Anthony

October 7, 2011 11:06 am

The interesting question here (to me, anyway) is why didn’t Venus evolve sulfate-reducing microbes such as the cyanobacteria present on Archaean earth (before the atmosphere became polluted with the by-product of such bio-chemistry – oxygen)?

Another Gareth
October 7, 2011 11:07 am

“Ozone is a molecule containing three oxygen atoms. According to computer models, the ozone on Venus is formed when sunlight breaks up carbon dioxide molecules, releasing oxygen atoms.”
Interesting. I wonder if it would be practical to turn CO2 into CO and then into other substances; eg CO2 into CO into Methanol. I guess if it was it would already be being done but it appears research is ongoing – New Scientist: Catalyst could help turn CO2 into fuel.

October 7, 2011 11:13 am

George E. Smith; says:
October 7, 2011 at 10:26 am
“”””” Ozone has only previously been detected in the atmospheres of Earth and Mars. On Earth, it is of fundamental importance to life because it absorbs much of the Sun’s harmful ultraviolet rays. Not only that, it is thought to have been generated by life itself in the first place. “””””
Well I would say that the “news” in this story is the amazing revelation that life produces the earth’s ozone.

Hi George, the point is that the oxygen in the earth’s atmosphere was produced by life and photodissociation of the O2 is the major source of O3 on Earth. In the primaeval atmosphere there would have been much less ozone.

mwhite
October 7, 2011 11:18 am

“Might be some sort of CO2 to O2 to O3 reduction/creation process we don’t understand yet, remember Venus is closer to the sun, so higher energy available for such processes – Anthony”
“According to computer models, the ozone on Venus is formed when sunlight breaks up carbon dioxide molecules”
Computer models again.
Mars isn’t so close to the sun.

Kelvin Vaughan
October 7, 2011 11:30 am

wobble says:
October 7, 2011 at 9:13 am
Of course Venus has an ozone layer. They never used air conditioners and hairspray on Venus.
No but they burnt fossil fuels and look what happened to the atmosphere!

ShrNfr
October 7, 2011 11:57 am

Neat. Of course, our real problems come from the owezone liar we have in the US at present.

October 7, 2011 12:24 pm

REPLY: Phil you are reading too much into this. I wasn’t suggesting we don’t understand the process of CO2 disassociation, only that we might not understand the process as it exists on Venus in that atmosphere. All we know is that there is ozone there.
We know a bit more than that, we know that there is CO2, CO, O, O2, UV photons of the right energy and now O3. Their locations are where we would expect be based on our understanding of CO2 photodissociation and O atom recombination reactions.

Hoser
October 7, 2011 12:38 pm

This post reports O3 formed from CO2. The fate of oxygen atoms was discussed. What happens to the carbon atoms? If protons from the solar wind can hit the atmosphere, there might be some slight production of organic molecules (perhaps formaldehyde). Based on density, methane would tend to rise in all that CO2 and break up. However, propane and larger (and alcohols, etc.) might sink. It might be interesting to look in IR for alcohols, aldehydes, and ketones. Nitrogen and sulfur are also available. It appears the European Venus-Express satellite should be able to see organic compounds. ESA publications report hydroxyl and C-O bands have been found.
http://www.springerlink.com/content/r37p8qrn876j54x1/
http://www2.chemistry.msu.edu/faculty/reusch/VirtTxtJml/Spectrpy/InfraRed/infrared.htm
http://www.wellesley.edu/Chemistry/chem211lab/Orgo_Lab_Manual/Appendix/Instruments/InfraredSpec/Chem211%20IR%20Lit%20Value%20Table.pdf
http://en.wikipedia.org/wiki/Venus_Express#Spectrometer
http://www.spacedaily.com/reports/Venus_Express_Provides_First_Detection_Of_Hydroxyl_In_Atmosphere_Of_Venus_999.html
CO
http://sci.esa.int/science-e/www/object/index.cfm?fobjectid=42249
Solar wind
http://sci.esa.int/science-e/www/object/index.cfm?fobjectid=39669

October 7, 2011 2:15 pm

Hoser, the CO2 produces CO and O, you don’t need to worry about C. Not much chance of complex organics up there with that much UV photons flying around.

Verified by MonsterInsights