26 AUSTRALIAN SKY & TELESCOPE July 2017
COMET:
ESA / ROSETTA / MPS FOR OSIRIS TEAM; CREW: ESA / J. MAI
quickly. Crucially, Rosetta’s images show that the two lobes
are layered — and that the layers in one lobe do not align
with those in the other. The densities of the two lobes might
be different as well. These differences suggest that the lobes
formed independently and then became stuck together.
Comet 67P’s density is so low, about half that of water ice
or about the density of flour, that it would float in water. The
porosity is very high, about 70%, but only on relatively small
scales. The portion of the interior probed by the CONSERT
experiment, which sent radio signals back and forth between
Philae and Rosetta through the nucleus, is uniform on scales
larger than 10 metres. So there don’t seem to be any large
cavities inside the part of the nucleus probed by radio waves.
Watching the comet change
By measuring the gravitational field’s effect on Rosetta as it
orbited, we could measure the comet’s mass very precisely. It’s
9.982 trillion kilograms. And we were able to determine that
the nucleus lost about 0.2% of that (18 billion kilograms)
over just two years. This mass was lost as heat from the
months-long close exposure to the Sun penetrated the
nucleus to sublimate (go from ice to gas) buried ices. The
escaping gases also dragged out dust, creating the classic gas
and dust tails well known to comet watchers.
We also found that 67P’s rotation period decreased by
about 21 minutes during Rosetta’s extended visit. A day on
the comet lasted about 12.4 hours before perihelion (August
13, 2015) and was around 12 hours afterward. Apparently
the nucleus spins faster with every 6½-year-long loop around
the Sun. Most likely, escaping gas exerted asymmetric forces
due to the comet’s unique shape and the strikingly different
‘seasons’ that each lobe experiences.
The axis of rotation is orientated as if the comet were
spinning sideways. That is, one side of the ‘duck’ is the northern
STHE LAST WORD Paolo Fermi, ESA’s head of mission operations,
sends the final command to Rosetta on September 30, 2016, as mission
manager Patrick Martin (white shirt) and others look on.
WCOMET ENCOUNTER Rosetta’s view of Comet 67P/Churyumov-
Gerasimenko, taken on January 31, 2015, shows a misshapen
nucleus packed with features and a strong jet of gas and dust.
Discovery September 11, 1969
Discoverers Klim Churyumov, Svetlana Gerasimenko
Orbital period 6.45 years
Perihelion 186 × 10^6 km (1.24 a.u.)
Aphelion 851 × 10^6 km (5.69 a.u.)
Orbital eccentricity 0.64
Orbital inclination 7.04°
Obliquity (to orbit) 52°
Overall size 4.3 × 2.6 × 2.1 km
Large lobe 4.1 × 3.5 × 1.6 km
Small lobe 2.5 × 2.1 × 1.6 km
Volume 18.7 km^3
Mass 9.982 × 10^12 kg
Density 0.53 g/cm^3
Rotation period 12.40 hours (June 2014)
12.06 hours (September 2016)
Surface temperature –93° to 53°C
Water vapor output 300 g/s (June 2014, August 2016)
300 kg/s (August 2015)
Dust-to-gas ratio 4 ± 2 (by mass)
Comet 67P/Churyumov-Gerasimenko
at a glance
ROSETTA RESULTS