A thoroughly sporadic column from astronomer Mike Brown on space and science, planets and dwarf planets, the sun, the moon, the stars, and the joys and frustrations of search, discovery, and life. With a family in tow. Or towing. Or perhaps in mutual orbit.



Showing posts with label Europa. Show all posts
Showing posts with label Europa. Show all posts

Sea salt (part 3)

[You should probably start with Part 1]

The first thing that you notice when you look at a spectrum of Europa -- from the Earth, from a spacecraft, it doesn’t really matter – is the ice. Ice is everywhere. The spectrum of ice is a very distinctive looking thing, with a quickly recognizable pattern of regions where the sunlight reflects strongly from the surface and regions where there is less reflectance (and remember the regions here means spectral regions, which means, essentially, we stare at one small spot on the surface, put the light through a prism to spread it all out, and see which colors of the rainbow are present and which are absent. In our case our rainbow is in infrared light that your eye can’t see, but the idea is still the same).

Sea Salt (part 2)

[don’t miss part 1] 

One of the biggest problems with trying to figure out what is on the surface of Europa was that the spectrograph on the Galileo spacecraft didn’t have a very fine view of the reflected light coming off the surface. The analogy I used in Part 1 was that Galileo was looking at fingerprints where you could only discern the rough pattern and not the individual ridges. You couldn’t use those fingerprints to know for sure who had smudged your crystal, though you might be able to rule out some people and you might become more suspicious of others.

There are two main reasons that the views from Galileo were not as fine as we would like. First Galileo was old when it arrived at Jupiter. Serious work began on the spacecraft in 1977, and with typical delays and atypical space shuttle accidents, it was finally launched, via a space shuttle, in 1989. Even the trip to Jupiter took longer than initially planned -- the shuttle accident spawned new rules which required the use of a less powerful rocket to launch Galileo from the orbiting shuttle -- so Galileo could not go directly to Jupiter but instead had to get gravity sligshots off of Venus and Earth before finally heading towards Jupiter and arriving in 1995, nearly twenty years after construction began. It was old on the first day it took data at Jupiter. (It was intentionally crashed into Jupiter in 2002 to prevent, among other things, an accidental crash into Europa, which would clearly disturb the whales).  Not surprisingly, the old technology was not as good as current technology in seeing precise spectral fingerprints.

Sea Salt (part 1)

Ever wonder what it would taste like if you could lick the icy surface of Jupiter’s Europa? The answer may be that it would taste a lot like that last mouthful of water that you accidentally drank when you were swimming at the beach on your last vacation. Just don’t take too long of a taste. At nearly 300 degrees (F) below zero your tongue will stick fast.

The composition of the surface of Europa has been hotly debated since the Galileo mission attempted to make detailed measurements more than a decade ago. Galileo’s tool for measuring the composition was spectroscopy – looking at the sunlight that reflects off of the surface of Europa and seeing which molecules leave characteristic fingerprints in that reflected sunlight. It’s a powerful technique, one that led to the initial discovery of water ice on the Galilean satellite, the discovery of frozen methane on distant bodies like Eris and Pluto and Makemake, and is even used on the Earth to map out mineral deposits for potential exploitation.