WEBVTT FILE 1 00:00:00.033 --> 00:00:03.966 [ Music ] 2 00:00:03.966 --> 00:00:06.566 So when we think about ocean worlds, it's good to compare them to what 3 00:00:06.566 --> 00:00:11.300 we know about Earth. In total proportion, Earth is about point-one-percent water. 4 00:00:11.300 --> 00:00:15.200 An ocean world is a body that has, in proportion, about ten times more water 5 00:00:15.200 --> 00:00:16.166 than Earth does. 6 00:00:16.166 --> 00:00:20.433 And when we think of the TRAPPIST planets, those planets have about fifty times 7 00:00:20.433 --> 00:00:23.033 more water in proportion to what Earth does. 8 00:00:23.033 --> 00:00:27.333 Ocean worlds do appear to be common in our galaxy. As far back as the early 2000's, 9 00:00:27.333 --> 00:00:30.966 We had astronomers, some of them still here at NASA Goddard that suggested that we would 10 00:00:30.966 --> 00:00:34.133 have ocean worlds orbiting low-mass stars. 11 00:00:34.133 --> 00:00:39.333 Recently we've looked at about fifty-two exoplanets, and these are low-mass exoplanets 12 00:00:39.333 --> 00:00:43.966 and what we've found is, of these fifty-two planets one out of every four 13 00:00:43.966 --> 00:00:45.666 may be an ocean planet. 14 00:00:45.666 --> 00:00:50.533 And when it comes to these ocean planets, over half of them may be ice-covered 15 00:00:50.533 --> 00:00:54.766 ocean worlds, and so Enceladus and Europa may serve as small-scale analogues 16 00:00:54.766 --> 00:00:56.400 of these planets. 17 00:00:56.400 --> 00:01:01.800 So there are a number of different ways to search for life on planets around other stars, 18 00:01:01.800 --> 00:01:05.533 but the key method is the study of the atmospheres. 19 00:01:05.533 --> 00:01:10.600 We can search for signs of life - biosignatures, we call them, things like oxygen, 20 00:01:10.600 --> 00:01:14.866 water vapor, carbon dioxide, even more unusual biosignatures - 21 00:01:14.866 --> 00:01:20.033 things like chlorofluorocarbons, or other things that are only produced by intelligent life. 22 00:01:20.033 --> 00:01:24.433 By looking for these key constituents of planetary atmospheres that signal life, 23 00:01:24.433 --> 00:01:30.000 We can discover lifeforms on other planets that we could never actually visit in our lifetime. 24 00:01:30.000 --> 00:01:34.133 So this is very analogous to how we study the atmospheres of moons and planets 25 00:01:34.133 --> 00:01:38.133 in our own solar system, and really makes the connection between studying the plumes 26 00:01:38.133 --> 00:01:42.066 of Europa, and the atmospheres of planets around other stars. 27 00:01:42.066 --> 00:01:46.900 What I would like to see is the definition of a habitable zone expanded 28 00:01:46.900 --> 00:01:52.100 We don't want to keep thinking too narrow about liquid on the surface, broaden the scope 29 00:01:52.100 --> 00:01:56.533 and really try to embrace other worlds that might seem too far from their host star, 30 00:01:56.533 --> 00:02:01.066 and frozen out, when they really aren't frozen at all. At great depths, they harbor 31 00:02:01.066 --> 00:02:06.033 a warm, hydrothermal-driven, liquid water environment. 32 00:02:06.033 --> 00:02:27.200 [ Music ]