WEBVTT FILE 1 00:00:00.610 --> 00:00:03.350 There’s one thing that stands between us 2 00:00:03.350 --> 00:00:06.480 and the harsh environment of space — our atmosphere. 3 00:00:06.480 --> 00:00:10.900 The part of Earth that sustains all life. 4 00:00:10.900 --> 00:00:17.750 But here, in the closest town to the North Pole, it’s slowly leaking away. 5 00:00:17.750 --> 00:00:20.640 A team headed there to launch rockets into the leak. 6 00:00:20.640 --> 00:00:23.830 But it’s not the lack of atmosphere that they’re concerned about. 7 00:00:23.830 --> 00:00:27.130 The leak is a natural process that will take billions of years. 8 00:00:27.130 --> 00:00:30.430 So we’re not going to run out any time soon. 9 00:00:30.430 --> 00:00:34.310 It’s part of the larger story of how a planet’s atmosphere changes over time — 10 00:00:34.310 --> 00:00:39.940 a key factor in the search for life on other planets. 11 00:00:39.940 --> 00:00:43.630 We have 35 residents and 60 of our team together 12 00:00:43.630 --> 00:00:47.090 in a town that is completely isolated — there’s a plane twice a week 13 00:00:47.090 --> 00:00:50.300 and there’s a thousand polar bears nearby 14 00:00:50.300 --> 00:00:51.460 This is Doug Rowland, 15 00:00:51.460 --> 00:00:56.560 a NASA scientist, who’s taken his team to Ny-Alesund on the island of Svalbard. 16 00:00:56.560 --> 00:01:01.770 The island lies beneath one of two regions near Earth’s poles called the cusps. 17 00:01:01.770 --> 00:01:04.190 It’s where we can access space directly. 18 00:01:04.190 --> 00:01:07.880 And where a hundred tons of atmosphere escapes into space each day. 19 00:01:07.880 --> 00:01:11.380 This escape gives clues to how long an atmosphere will last 20 00:01:11.380 --> 00:01:15.540 and ultimately whether it says around long enough to sustain life. 21 00:01:15.540 --> 00:01:19.430 We’re trying to understand is how did Earth’s atmosphere evolve over time 22 00:01:19.430 --> 00:01:25.580 and how do other planets that might be like Earth or more dissimilar to Earth, how did their atmospheres evolve. 23 00:01:25.580 --> 00:01:31.000 So Doug joined forces with Joran Moen –  a professor at the University of Oslo – 24 00:01:31.000 --> 00:01:34.170 who started the “Grand Challenge Initiative – Cusp”. 25 00:01:34.170 --> 00:01:39.210 It’s an international mission to launch 12 rockets into the Earth’s northern cusp. 26 00:01:39.210 --> 00:01:48.930 And Doug — he’s the mission leader for the first two rockets of the campaign. 27 00:01:48.930 --> 00:01:50.150 We don’t want to waste our rocket. 28 00:01:50.150 --> 00:01:53.110 It takes us 3 years to make the rocket and only 15 minutes to use it 29 00:01:53.110 --> 00:01:54.640 and I don’t want to waste my shot here. 30 00:01:54.640 --> 00:02:00.810 He’s using a sounding rocket, which is different from the bigger rockets that carry satellites and humans into space. 31 00:02:00.810 --> 00:02:04.470 It’s a small, suborbital rocket that flies briefly into space, 32 00:02:04.470 --> 00:02:08.670 collects real-time data for around 15 minutes, then falls back to Earth. 33 00:02:08.670 --> 00:02:13.300 It’s affordable, quick to build, and can launch towards a precise point. 34 00:02:13.300 --> 00:02:17.620 The major advantage is that you can launch into a target on the sky. 35 00:02:17.620 --> 00:02:22.060 But there’s a limited launch window and only one chance to get the launch right. 36 00:02:22.060 --> 00:02:27.530 We have these unguided rockets. They go where you point them 37 00:02:27.530 --> 00:02:29.970 unless the wind is blowing because the wind literally just blows them over. 38 00:02:29.970 --> 00:02:31.250 We don’t launch when there’s high winds. 39 00:02:31.250 --> 00:02:35.420 So to measure the winds, they launch balloons with GPS trackers. 40 00:02:35.420 --> 00:02:37.750 They’re released every 15 to 30 minutes. 41 00:02:37.750 --> 00:02:45.610 And then, they’re monitored to see how fast the winds are carrying them. 42 00:02:45.610 --> 00:02:50.200 The ground winds were about 12, 13 meters per second. 43 00:02:50.200 --> 00:02:53.600 Gusting — 17. It’s just way off. 44 00:02:53.600 --> 00:02:56.730 You’re filled with trepidation. Oh my gosh, is this thing that I built, 45 00:02:56.730 --> 00:03:02.500 is it going to work after all this. 46 00:03:02.500 --> 00:03:04.900 So, I think we’re going to scrub for today. 47 00:03:04.900 --> 00:03:09.530 I’d like to thank everyone. I think it was a great performance. Thanks a lot. 48 00:03:09.530 --> 00:03:12.560 This that means we are scrubbing this operation for today 49 00:03:12.560 --> 00:03:18.450 and try again tomorrow. 50 00:03:18.450 --> 00:03:24.750 The mission is named Visualizing Ion Outflow via Neutral Atom Sensing-2, or VISIONS-2. 51 00:03:24.750 --> 00:03:29.130 In short, they’re looking at how oxygen is getting enough energy to escape. 52 00:03:29.130 --> 00:03:31.560 It’s a good test of how atmospheric escape works. 53 00:03:31.560 --> 00:03:37.090 Earth’s gravity should hold onto the oxygen, and yet we see this gas shooting off into space. 54 00:03:37.090 --> 00:03:39.020 We’re trying to figure out how that works.  55 00:03:39.020 --> 00:03:43.780 That is a science question that has been hanging around for four decades. 56 00:03:43.780 --> 00:03:48.810 Fortunately, anyone can see atmospheric escape at the right place and time. 57 00:03:48.810 --> 00:03:53.800 In Svalbard, we have the so-called polar night. It’s dark all 24 hours 58 00:03:53.800 --> 00:03:57.210 This continual darkness is key for witnessing this. 59 00:03:57.210 --> 00:04:02.920 This is the cusp aurora. It’s a type of northern lights that appears between 8:00 a.m. and noon, 60 00:04:02.920 --> 00:04:05.700 and you can only see it when it’s dark during the day. 61 00:04:05.700 --> 00:04:08.310 It looks similar to the aurora that occurs at night. 62 00:04:08.310 --> 00:04:11.710 But when these iridescent colors dance at this hour each day, 63 00:04:11.710 --> 00:04:16.680 a hundred tons of oxygen escapes from Earth’s atmosphere into space. 64 00:04:16.680 --> 00:04:20.660 This is our sport now, to chase the aurora 65 00:04:20.660 --> 00:04:26.360 Working with them is the EISCAT radar and Kjell Henriksen Observatory. 66 00:04:26.360 --> 00:04:28.970 They have additional instruments to find the aurora. 67 00:04:28.970 --> 00:04:33.720 Sometimes it’s cloudy so we use radars to track the the cusp. 68 00:04:33.720 --> 00:04:38.270 We can give advice that this is the right type of aurora. 69 00:04:38.270 --> 00:04:43.160 This is the wall of science — a collection of data from satellites and ground instruments 70 00:04:43.160 --> 00:04:46.070 that helps them predict where the cusp aurora will be.  71 00:04:46.070 --> 00:04:50.280 So, the cusp actually isn’t in a fixed point in space—it kind of moves around 72 00:04:50.280 --> 00:04:55.270 What’s controlling the cusp’s movement is the Sun interacting with Earth.  73 00:04:55.270 --> 00:05:00.670 Our planet is surrounded by a magnetic field that helps us hold on to our atmosphere. 74 00:05:00.670 --> 00:05:07.070 But at the north and south poles the magnetic field bends inwards, creating a corridor between Earth and space. 75 00:05:07.070 --> 00:05:12.810 When energy is released from the Sun, via. a solar flare or a coronal mass ejection, 76 00:05:12.810 --> 00:05:17.580 all of that energy in the form of radiation rides down the magnetic field lines of the Earth 77 00:05:17.580 --> 00:05:21.280 and is transferred and dumped into the Earth’s atmosphere. 78 00:05:21.280 --> 00:05:24.370 Electrons cascade into Earth’s atmosphere. 79 00:05:24.370 --> 00:05:27.240 They accelerate and collide with oxygen particles 80 00:05:27.240 --> 00:05:31.840 giving them energy to release light and sometimes, enough energy to escape. 81 00:05:31.840 --> 00:05:38.090 Collectively, this forms the cusp aurora and streams of escaping oxygen. 82 00:05:38.090 --> 00:05:40.600 This cusp is in constant motion. 83 00:05:40.600 --> 00:05:44.190 And we’ve got a fixed trajectory—we really can’t aim where the cusp is, 84 00:05:44.190 --> 00:05:46.420 we have to wait for the cusp to come across our line of sight. 85 00:05:46.420 --> 00:05:47.650 Can you guys hear Kjellmar? 86 00:05:47.650 --> 00:05:52.850 We’d like you, as soon as you see an indication that the cusp is moving close, to move it -- the radar dish if we can. 87 00:05:52.850 --> 00:05:57.890 This is EISCAT. It’s been very quiet. Very difficult to launch. 88 00:05:57.890 --> 00:06:02.010 89 00:06:02.010 --> 00:06:04.150 Do you think we’ll launch today? 90 00:06:04.150 --> 00:06:08.260 No. 91 00:06:08.260 --> 00:06:14.040 Probably a 60% chance of launching. 92 00:06:14.040 --> 00:06:18.470 When we kind of started seeing this really good data, this clock started counting down, 93 00:06:18.470 --> 00:06:22.460 and that’s when everyone realized this is going to happen. We’re going to launch 94 00:06:22.460 --> 00:06:27.970 We’re doing everything we can to get that launch off before the aurora goes away, 95 00:06:27.970 --> 00:06:32.480 and it’s really, really challenging and nerve-wracking at that point. 96 00:06:32.480 --> 00:06:38.670 You can see the tension just rise in everybody when that happens. 97 00:06:38.670 --> 00:06:42.490 And so everyone's watching their instruments, getting really excited. 98 00:06:42.490 --> 00:06:59.230 And then at T minus one minute all of us ran out to go see the launch happen. 99 00:06:59.230 --> 00:07:05.970 And we immediately turn around and ran right back in to look at all the data that was coming back from the instruments. 100 00:07:05.970 --> 00:07:12.900 ou know how much time and effort went into it because we all worked on it 101 00:07:12.900 --> 00:07:16.650 and there’s just nothing that compares to that feeling. 102 00:07:16.650 --> 00:07:24.690 Everybody, in every one of those little places, you know, really just so happy to contribute to getting the science. 103 00:07:24.690 --> 00:07:28.170 It's really an incredible experience. 104 00:07:28.170 --> 00:07:32.370 This is a story about what it takes to launch science instruments into space. 105 00:07:32.370 --> 00:07:36.480 But the real adventure will be in the data they sent back. 106 00:07:36.480 --> 00:07:39.940 Hidden within the numbers will be answers that reach far beyond Earth, 107 00:07:39.940 --> 00:07:47.600 shedding light on how atmospheres throughout the universe change, evolve, and perhaps, support life. 108 00:07:47.600 --> 00:07:58.293