This site is only a doorway

Everything here is gathered from things other people actually researched, thought through, and built: books, papers, historical records, and the people behind them. If something here catches your interest, go look at the original sources listed at the bottom of the page. They carry more depth than a page like this ever can.

How Do We Know There Is an Ocean Under the Ice of Saturn's Moon Enceladus?

Category: Space & Astronomy

Nobody has ever dug through the ice of Enceladus, a small moon of Saturn only about 500 km (310 miles) across. Yet scientists say a liquid ocean lies under it. How can anyone know that from a spacecraft flying past?

The short answer: the moon sprays water into space, the spray is salty, and the moon wobbles too much to be frozen solid all the way through. This article follows those three clues in order, then looks at what has been found on the ocean floor, and ends with what nobody knows yet.

1. A small icy moon was caught spraying water into space

Enceladus (say "en-SELL-uh-dus") is only about 500 km (310 miles) across[1]. The Cassini spacecraft was exploring Saturn, and its observations in 2005 revealed a huge cloud of water vapor above the moon's south polar region[2]. The source turned out to be long cracks that scientists nicknamed "tiger stripes"[2]. Water jets come out of these relatively warm cracks[1].

This is not a stream of liquid water. What flies out is water vapor and tiny grains of ice. The question is where it comes from: ice that is simply warmed and evaporated near the cracks, or a pool of liquid water below? Three kinds of measurement, made at different times, answer it one after another.

2. The ice grains are salty, which points to liquid water below

Cassini flew through the spray and sampled it. A team reported in 2011 that salt-rich ice grains made up more than 99 percent of the mass of the solid material being thrown out[3]. That percentage describes the mass of the ejected solids. It does not say how salty the ocean is[3].

Salt in ice grains is what you would expect if the grains were frozen droplets of salt water. The team concluded that "a salt-water reservoir with a large evaporating surface provides nearly all of the matter in the plume"[3].

That settles that salt water exists somewhere. It does not say whether it is a small pocket under the south pole or a sea around the whole moon. For that, scientists needed to weigh the moon and watch it move.

3. The moon's pull and wobble show how big the ocean is

A tiny tug on the spacecraft: evidence for a sea under the south pole

Cassini passed within 100 km of Enceladus three times in 2010 and 2012. The moon's gravity changed the spacecraft's speed by only about 0.2 to 0.3 millimeters per second (roughly 0.01 inch per second), and that change showed up in its radio signal[4]. Reading the pattern, the researchers found that mass was distributed as if liquid water lay about 30 to 40 km (19 to 25 miles) below the ice surface in the southern hemisphere[4]. That figure is the depth down to the water, not the thickness of the ocean.

In 2014 the best fit was a regional sea reaching from the south pole to about 50 degrees south latitude, although the data could not rule out a global ocean[4].

A wobble that is too big: an ocean around the whole moon

The next clue came from pictures. Researchers measured the positions of craters and other landmarks in Cassini images taken over more than seven years, and worked out how much Enceladus wobbles back and forth as it orbits Saturn. The result was 0.120 degrees, give or take 0.014 degrees (the paper's 2σ uncertainty, roughly 95 percent confidence)[5].

That may sound tiny, but it is too large for a moon that is solid from the surface to the core. A simple way to picture it: try to twist the shell of a hard-boiled egg and the whole egg turns with it, but the shell of a raw egg can slip around the liquid inside. If the ice shell were rigidly attached to the core, the wobble would be much smaller than the one measured[6]. The authors concluded that the wobble "implies the presence of a global ocean rather than a localized polar sea"[5]. NASA announced this in 2015[6].

How thick is the ice? Estimates differ

NASA now describes the ice shell as roughly 1 to 5 km (0.6 to 3 miles) thick at the south pole and about 20 to 25 km (12 to 16 miles) thick on average[1]. The 30 to 40 km figure above is the depth to water in the 2014 gravity study, so the numbers are not directly comparable. Treat any single number for the shell as an estimate that research keeps updating.

One puzzle remains. The wobble paper notes that keeping a global ocean liquid is "problematic according to many thermal models"[5]. NASA's release says what keeps the ocean from freezing is still unknown, and suggests heating caused by Saturn's pull as one possibility[6]. The ocean was found first. The full explanation is still being worked on.

4. Silica and hydrogen hint at hot water meeting rock on the ocean floor

Once there is an ocean, the next question is what its bottom is like. Two clues came from the spray.

The first is silica, the main ingredient of sand and glass. Cassini found extremely small silica grains, 2 to 8 nanometers in radius, in Saturn's E ring, the thin ring of ice fed by Enceladus[7]. A nanometer is one billionth of a meter. The narrow range of sizes pointed to hot-water reactions above 90 °C (194 °F)[7]. A university press release describes the grains forming when hot, mineral-laden water rises from the rocky interior and meets colder water[8]. The 90 °C figure is a lower limit, not a measurement of the water temperature.

The second is hydrogen. In 2015, Cassini made its deepest dive through the plume, and its mass spectrometer found a significant amount of molecular hydrogen[9]. NASA says this supports earlier evidence that warm, mineral-laden water flows out of seafloor vents[9]. Silica and hydrogen are different substances found by different instruments, and both suggest the same thing: hot water reacting with rock on the ocean floor.

5. Ingredients for life may be present, but no one has found life

On Earth, some microbes live on hydrogen and turn it into methane[9]. A similar kind of chemistry could be possible in the ocean of Enceladus. But the lead scientist of the instrument team put it carefully: finding hydrogen "is not demonstration of finding life, but it shows the potential for the existence of life" there[9]. NASA states that Cassini is not able to detect life, and has found no evidence that Enceladus is inhabited[9].

In 2023 a team reported that ice grains from the E ring contain phosphate, a form of phosphorus, which living things on Earth need to build their cells. They estimated the ocean holds more than 100 times as much phosphate as Earth's oceans[10]. The team says there is no evidence that the ocean is actually inhabited[10].

So the honest summary is this: scientists have strong evidence for liquid water beneath the ice, a source of chemical energy, and some of the chemical ingredients that life on Earth uses. Having the ingredients is not the same as having a meal being cooked, and whether anything lives in that ocean is an open question.

How could we find out more, and how can you explore the idea?

  • Future missions. The European Space Agency is studying a mission to land on Enceladus, with a launch listed for 2042. It is still under study, so the plan is not fixed. Its goals include sampling the plume and searching for signs of life[11].
  • Spin two eggs. With an adult, boil one egg and let it cool completely. Spin it and a raw egg on a large plate or tray, then gently stop each with a fingertip and let go. The cooked egg usually stays stopped. The raw egg may start turning again, because the liquid inside is still moving. Scientists reasoned in a similar way about the ice shell, though the real wobble is far too small to see. Wash your hands after handling raw egg.
  • Read the original. NASA's page on Cassini at Enceladus and the 2015 global-ocean announcement are short and readable. Try to spot which clue each one is about.

Sources

This article is a personal summary based on the public sources listed below.

  1. NASA Science, "Enceladus." https://science.nasa.gov/saturn/moons/enceladus/ (Read in full. It gives the diameter of about 500 km, the tiger-stripe jets, and the ice shell estimates of 1 to 5 km at the south pole and 20 to 25 km on average. The page also says the moon has most of the chemical ingredients needed for life; this article does not go beyond the narrower statements in sources 9 and 10.)
  2. NASA Science, "Cassini at Enceladus." https://science.nasa.gov/mission/cassini/science/enceladus/ (Read in full. It supports the 2005 observations of the water vapor cloud and the tiger stripes. It gives no exact date for the first plume pictures.)
  3. ESA Cassini-Huygens, summary of Postberg et al. (2011), Nature 474, 620. https://sci.esa.int/web/cassini-huygens/-/48835-postberg-f-et-al-2011 (Only the abstract, as reproduced by ESA, was read, not the full paper. It supports the 99 percent of ejected solid mass and the salt-water reservoir conclusion.)
  4. ESA Cassini-Huygens, "Icy moon Enceladus has underground sea" (2014), on Iess et al., Science. https://sci.esa.int/web/cassini-huygens/-/53938-icy-moon-enceladus-has-underground-sea (Read in full. It supports the three flybys, the 0.2 to 0.3 mm/s velocity change, the 30 to 40 km depth, and the regional sea out to 50 degrees south. The page reports the flybys as three passes within 100 km; the 2010 and 2012 years are from the same page.)
  5. Thomas et al., "Enceladus's measured physical libration requires a global subsurface ocean," Icarus (2016); preprint abstract. https://arxiv.org/abs/1509.07555 (Only the abstract on arXiv was read. It gives 0.120 ± 0.014 degrees (2σ), the global-ocean conclusion, and the remark about thermal models. The seven-year image span comes from source 6.)
  6. NASA, "Cassini Finds Global Ocean in Saturn's Moon Enceladus" (September 15, 2015). https://www.nasa.gov/news-release/cassini-finds-global-ocean-in-saturns-moon-enceladus/ (Read in full. It supports the more-than-seven-years image measurement, the "wobble would be far smaller" statement, and the unknown heat source. The raw-egg picture in section 3 is this article's own and is not from NASA.)
  7. ESA Cassini-Huygens, summary of Hsu et al. (2015), Nature 519, 207. https://sci.esa.int/web/cassini-huygens/-/55568-hsu-et-al-2015 (Only the ESA summary was read. It supports silica grains of 2 to 8 nm in radius, reactions above 90 °C, and the E ring.)
  8. Heidelberg University press release (March 11, 2015) on the silica grains. https://uni-heidelberg.de/presse/news2015/pm20150311_saturn-moons-ocean-may-have-hydrothermal-activity.html (Read in full. It supports the picture of hot mineral-rich water meeting cold water. It describes the largest grains as 6 to 9 nm across, which is consistent with source 7 once radius and diameter are told apart.)
  9. NASA Science, news on the hydrogen finding at Enceladus (April 2017), based on Waite et al., Science 356, 155. https://science.nasa.gov/?p=154218 (The NASA page was read in full. The Science paper itself could not be opened, so details such as the exact date and altitude of the 2015 flyby are left out.)
  10. Freie Universität Berlin, planetary sciences news on phosphates at Enceladus (June 14, 2023), on Postberg et al., Nature. https://geo.fu-berlin.de/en/geol/fachrichtungen/planet/news/Postberg_Phosphates_Enceladus.html (Read in full. It supports phosphate levels more than 100 times those of Earth's oceans and the statement that there is no evidence the ocean is inhabited. The remark that living things on Earth use phosphorus is a general fact not taken from this page.)
  11. ESA, "L4 to Enceladus." https://www.science.esa.int/web/cm25/l4-to-enceladus (Read in full. It lists a launch of 2042 and says the mission is under study.)

Update history

  • First published.