I had to share this animation, taken from a press release made by NASA this morning, and YouTube’d by the ever-awesome Phil Plait (who has a great blog post about it here). It’s an exceptionally clear and powerful illustration of just what that high-tech toy known as the Kepler Space Telescope is doing way up there in orbit. Kepler was only just launched in March, and this data is the result of a quick test of her abilities on a previously discovered planetary system — specifially, the roughly Jupiter-sized planet known as HAT-P-7b, which is so close to its own star that it completes an orbit in a mere 2.2 days. Measuring the exceedingly miniscule changes in the brightness of a distant star sounds like an awfully difficult means of inferring the existance of extra-solar planets (and it is!), but the animation does a spectacular job of illustrating just what the results mean. The first big drop in brightness shown is the planet transiting its star. The second is, amazingly, the star occulting the planet. And the remaining fluctuations? Those are the phases of HAT-P-7b as it orbits — just like the amount of light we see reflected off the Moon changes as it goes from new moon to full to new again!
This data shows that Kepler will be sensitive enough to detect Earth-sized planets, once her planet seeking begins in earnest. Most of the over 350 known extrasolar planets are broiling gas giants, but little rocky planets like ours are predicted to be more numerous. They’re out there, and Kepler will find them.
And once we do … then what?
We can use what we know about a star to determine where its habitable zone is — that Goldilocks region of not-too-hot and not-too-cold needed for liquid water to be present. We can determine approximately how old the system is, and thus whether or not there’s been enough time for life to evolve. And once we have a good candidate, we can do something like what LCROSS (Lunar CRater Observation and Sensing Satellite) did last week when it turned its instruments to Earth:
Yes, it’s more graphs. No shiny animation to accompany them this time, but this is still pretty cool. These are measurements taken by LCROSS’s spectrometers, showing the spectra of our planet’s reflected light. There’s lots of methane (CH4), and ozone (O3), and carbon dioxide (CO2), and other things you can find on plenty of lifeless planets. But there’s also oxygen gas (O2), which is something you generally don’t find unless there’s some process continually producing it. Oxygen is unstable, and it gets eaten up pretty quickly by various chemical processes, but here on Earth we have organisms to replenish it. Which brings us to something else showing up in this spectral analysis — a signature that could be attributed to the large amount of vegetation that covers the Earth’s surface.
This is why science is just so damn cool.






