At the poles of Ceres, scientists have found craters that are permanently in shadow (indicated by blue markings). Such craters are called “cold traps” if they remain below about minus 240 degrees Fahrenheit (minus 151 degrees Celsius). These shadowed craters may have been collecting ice for billions of years because they are so cold. This image was created using data from NASA’s Dawn spacecraft. Credit: NASA/JPL-Caltech/Goddard
Scientists with NASA’s Dawn mission have identified permanently shadowed regions on the dwarf planet Ceres. Most of these areas likely have been cold enough to trap water ice for a billion years, suggesting that ice deposits could exist there now. “The conditions on Ceres are right for accumulating deposits of water ice,” said N Schorghofer. “Ceres has just enough mass to hold on to water molecules, and the permanently shadowed regions we identified are extremely cold – colder than most that exist on the moon or Mercury.”
Permanently shadowed regions do not receive direct sunlight. They are typically located on the crater floor or along a section of the crater wall facing toward the pole. The regions still receive indirect sunlight, but if the temp stays below -240F, the permanently shadowed area is a cold trap – a good place for water ice to accumulate and remain stable. Cold traps were predicted for Ceres but had not been identified until now.
In this study, Schorghofer et al studied Ceres’ northern hemisphere, which was better illuminated than the south. Images from Dawn’s cameras were combined to yield the dwarf planet’s shape, showing craters, plains and other features in three dimensions. Using this input, a sophisticated computer model was used to determine which areas receive direct sunlight, how much solar radiation reaches the surface, and how the conditions change over the course of a year on Ceres.
The researchers found dozens of sizeable permanently shadowed regions across the northern hemisphere. The largest one is inside a 10-mile-wide crater <40 miles from the north pole. Taken together, Ceres’ permanently shadowed regions occupy about 695 square miles. This is a small fraction of the landscape – much less than 1% of the surface area of the northern hemisphere.
The team expects the permanently shadowed regions on Ceres to be colder than those on Mercury or the moon. That’s because Ceres is quite far from the sun, and the shadowed parts of its craters receive little indirect radiation. “On Ceres, these regions act as cold traps down to relatively low latitudes,” said Erwan Mazarico. “On the moon and Mercury, only the permanently shadowed regions very close to the poles get cold enough for ice to be stable on the surface.”
The situation on Ceres is more similar to that on Mercury than the moon. On Mercury, permanently shadowed regions account for roughly the same fraction of the northern hemisphere. The trapping efficiency – the ability to accumulate water ice – is also comparable. About 1 out of every 1,000 water molecules generated on the surface of Ceres will end up in a cold trap during a year on Ceres (1,682 days). That’s enough to build up thin but detectable ice deposits over 100,000 years or so.
“While cold traps may provide surface deposits of water ice as have been seen at the moon and Mercury, Ceres may have been formed with a relatively greater reservoir of water,” said Chris Russell. “Some observations indicate Ceres may be a volatile-rich world that is not dependent on current-day external sources.” http://www.nasa.gov/feature/goddard/2016/dawn-maps-ceres-craters-where-ice-can-accumulate
Recent Comments