WEBVTT FILE 1 00:00:00.100 --> 00:00:09.180 [ music ] 2 00:00:09.200 --> 00:00:13.080 Narrator: NASA's newest Mars spacecraft, MAVEN, is currently on a mission 3 00:00:13.100 --> 00:00:18.180 to determine how Mars lost its early atmosphere, and with it, its water. 4 00:00:18.200 --> 00:00:23.170 Jakosky: The questions that MAVEN is trying to answer deal with the history of the Martian climate. 5 00:00:23.190 --> 00:00:27.830 From the previous missions we have a lot of evidence that that climate has changed over time, 6 00:00:27.850 --> 00:00:32.210 that early Mars was warmer, wetter than present-day Mars. 7 00:00:32.230 --> 00:00:36.440 What we're trying to answer with MAVEN is, "Where did all that water go?" 8 00:00:36.460 --> 00:00:43.600 "Where did the carbon dioxide from an early thick atmosphere go?" And we're doing this by studying the top of the atmosphere. 9 00:00:43.620 --> 00:00:48.290 Since we are the first mission really looking at all pieces of the puzzle on the upper atmosphere, 10 00:00:48.310 --> 00:00:52.830 almost everything we're seeing and how it relates to everything else is brand new. 11 00:00:52.850 --> 00:00:58.250 As an example, one of the things we measured very early in the mission, right after we went into orbit, 12 00:00:58.270 --> 00:01:04.020 before we even got into our final science mapping orbit, was the distribution of hydrogen, 13 00:01:04.040 --> 00:01:11.020 oxygen, and carbon as a cloud surrounding the planet, the very extended upper atmosphere. 14 00:01:11.040 --> 00:01:19.280 Narrator: In this ultraviolet image, carbon and oxygen cling tightly to Mars, while hydrogen, the lightest element, extends well above the planet. 15 00:01:19.300 --> 00:01:25.830 Understanding the escape of hydrogen is important, because hydrogen is the primary ingredient in water. 16 00:01:25.850 --> 00:01:29.230 While previous Mars orbiters have peered down at the planet's surface, 17 00:01:29.250 --> 00:01:36.780 MAVEN is spending part of its time gazing at the stars, observing the Martian atmosphere through a series of stellar occultations. 18 00:01:36.800 --> 00:01:40.480 Jakosky: The imaging ultraviolet spectrograph, the IUVS instrument, 19 00:01:40.500 --> 00:01:45.900 can determine properties of the upper atmosphere all the way down to the lower atmosphere, 20 00:01:45.920 --> 00:01:51.330 by looking at a star, as the star sets behind the planet as seen from the spacecraft. 21 00:01:51.350 --> 00:01:59.580 And by looking at the diminution, the weakening of the starlight as it sets, we can measure the composition of the upper atmosphere. 22 00:01:59.600 --> 00:02:03.980 Narrator: The relative motion of the stars allows MAVEN to look at columns of the atmosphere, 23 00:02:04.000 --> 00:02:07.230 revealing how its composition changes with altitude. 24 00:02:07.250 --> 00:02:14.190 At the same time, MAVEN's orbit passes close to the Martian polar caps, giving it north-to-south coverage of the planet. 25 00:02:14.210 --> 00:02:19.180 Mars itself rotates once a day beneath MAVEN, providing east-to-west coverage. 26 00:02:19.200 --> 00:02:22.980 This combination allows MAVEN to observe the entire atmosphere. 27 00:02:23.000 --> 00:02:30.780 Jakosky: My goal with MAVEN is to put together a data set that the Mars science community can spend the next decade or two working on. 28 00:02:30.800 --> 00:02:36.180 We're making very few measurements that have never been made at all before at Mars, 29 00:02:36.200 --> 00:02:41.400 but what we're doing is, we're making them in parts of the atmosphere where they haven't been measured, 30 00:02:41.420 --> 00:02:47.600 we're making comprehensive measurements for a full year rather than, for example with the Viking lander, 31 00:02:47.620 --> 00:02:52.980 a one-time entry, one profile. We're going to get hundreds and hundreds of profiles, 32 00:02:53.000 --> 00:02:58.460 and be able to see how the upper atmosphere responds to the changing solar conditions, 33 00:02:58.480 --> 00:03:05.120 and really put together a picture of the upper atmosphere that we haven't been able to put together before. 34 00:03:05.140 --> 00:03:12.650 [ music ] 35 00:03:12.670 --> 00:03:26.470 [ satellite beeping ]