Although Titan is often cited as resembling the early Earth, the differences are striking. Temperature is the most obvious, with an average of 95 Kelvin (-178 degrees Celsius), keeping water at the surface firmly frozen. Our planet was tectonically active in its infancy, roiled not only by widespread volcanism but also asteroid impacts, especially during the period known as the Late Heavy Bombardment some 4.1 to 3.8 billion years ago. Throw in the fact that the Earth had high concentrations of carbon dioxide -- Titan does not -- and it's clear that we can't make too broad a comparison between the two worlds. What we do have on Titan, however, is an atmosphere that teems with chemical activity, fueled by light from the Sun and the charged particle environment in the moon's orbit around Saturn. So we do have a chemistry here that is capable of turning simple organics into more complex ones. Thus the findings from a new study of archival data using the Atacama Large...
New Insights into Long-Period Comets
The Voyagers' continuing interstellar mission reminds us of how little we know about space just outside our own Solar System. We need to learn a great deal more about the interstellar medium before we venture to send fast spacecraft to other stars. And indeed, part of Breakthrough Starshot's feasibility check re small payloads and sails will be to assess the medium and determine what losses are acceptable for a fleet of such vehicles. The definitive work on the matter is Bruce Draine's Physics of the Interstellar and Intergalactic Medium, and thus it's no surprise that Draine has been involved as a consultant with Starshot. As we saw yesterday, we have only one spacecraft returning data from outside the heliosphere (soon to be joined by Voyager 2), making further precursor missions explicitly designed to study 'local' gas and dust conditions a necessity. Another reminder of the gaps in our knowledge comes from an analysis of WISE data. The Wide-field Infrared Survey Explorer...
Go Voyager
It's worth thinking about why Voyager 1 and 2, now coming up on their 40th year of operation, are still sending back data. After all, mission longevity becomes increasingly important as we anticipate missions well outside the Solar System, and the Voyagers are giving us a glimpse of what can be done even with 1970's technology. We owe much of their staying power to their encounters with Jupiter, which demanded substantial protection against the giant planet's harsh radiation, a design margin still used in space missions today. The Voyagers were the first spacecraft to be protected against external electrostatic charges and the first with autonomous fault protection, meaning each spacecraft had the ability to detect problems onboard and correct them. We still use the Reed-Solomon code for spacecraft data to reduce data transmission errors, and we all benefited from Voyager's programmable attitude and pointing capabilities during its planetary encounters. Pioneer 6 was a doughty...
Exomoons: Rare in Inner Stellar Systems?
Exomoons -- moons around planets in other star systems -- are an exhilarating and at the same time seemingly inevitable prospect. There is little reason to assume our Solar System is unique in its menagerie of moons, with the gas giants favoring us particularly with interesting mission targets, and then there's that fascinating double system at Pluto/Charon. If we visualize what we expect to find in any given stellar system, surely moons are part of the mix, and investigations like the Hunt for Exomoons with Kepler will doubtless find them. An actual exomoon detection would be a triumph for exoplanet science, especially given how recently it was that we nailed down the first confirmed exoplanet, 51 Pegasi b, in 1995 (or, if you prefer, the 1992 detection of terrestrial-mass planets orbiting the pulsar PSR B1257+12). We're new at this, and what huge strides we've made! Given the small size of the transit signal and its changing relation to the body it orbits, exomoons offer a...