WEBVTT FILE 1 00:00:01.230 --> 00:00:06.180 On January 15 2022, the uninhabited volcanic island 2 00:00:06.210 --> 00:00:09.870 Hunga Tonga-Hunga Ha'apai erupted violently, creating 3 00:00:09.870 --> 00:00:14.220 worldwide shockwaves, sonic booms, tsunamis and powerful 4 00:00:14.220 --> 00:00:16.980 winds all while blanketing surrounding islands and two 5 00:00:16.980 --> 00:00:21.870 centimeters of ash. It was a fatal eruption, and its impact 6 00:00:21.870 --> 00:00:24.810 on nearby communities was further compounded by the 7 00:00:24.810 --> 00:00:29.790 disruption caused to emergency services. NASA has been 8 00:00:29.790 --> 00:00:33.240 following the Pacific Islands unusual evolution for years. 9 00:00:33.330 --> 00:00:36.600 Using historical observations and satellite data of the 10 00:00:36.600 --> 00:00:39.930 January eruption, scientists have shed a new light on why 11 00:00:39.930 --> 00:00:43.470 this explosion is so unique and how such a small island is 12 00:00:43.470 --> 00:00:45.900 making such a huge impact across the planet. 13 00:00:46.920 --> 00:00:51.360 It gave us a window into a rapid paced life history of an island 14 00:00:51.510 --> 00:00:54.750 that we can compare to hundreds of other islands in the oceans 15 00:00:54.900 --> 00:00:58.500 over time. And these islands are sensitive indicators for the 16 00:00:58.500 --> 00:01:01.410 activities of climate environmental change, and we can 17 00:01:01.410 --> 00:01:04.620 project them forward even to other planets. So what an 18 00:01:04.620 --> 00:01:05.340 opportunity 19 00:01:06.570 --> 00:01:09.810 geologic record suggests that while the volcano may have 20 00:01:09.810 --> 00:01:13.530 produced massive explosive eruptions in the past, eruption 21 00:01:13.530 --> 00:01:16.170 of this magnitude wasn't expected so soon. 22 00:01:16.870 --> 00:01:20.650 This was what we call a volcanic explosivity index six eruption, 23 00:01:20.920 --> 00:01:24.970 nothing like it's it's Krakataua in the 19th century. And so what 24 00:01:24.970 --> 00:01:28.600 happened was this beautiful little island 100 meters tall, 25 00:01:28.690 --> 00:01:33.010 growing forming, by the nature of the way volcanoes and in 26 00:01:33.010 --> 00:01:38.380 water interact, was explosively changed forever. And literally, 27 00:01:38.380 --> 00:01:43.390 the entire base of the volcano fell hundreds of meters in to a 28 00:01:43.390 --> 00:01:47.980 shallow magma reservoir of liquid rock chamber, literally 29 00:01:48.010 --> 00:01:51.280 under the ocean, and then allowed the explosive 30 00:01:51.280 --> 00:01:55.240 interaction of a massive Pacific Ocean seawater with this hot 31 00:01:55.240 --> 00:01:59.650 rock 1300 degrees Kelvin. That's super hot, hotter than your 32 00:01:59.650 --> 00:02:03.640 oven. And that explosion with the pressure move the water, the 33 00:02:03.640 --> 00:02:07.270 rock, the small amounts of ash that were part of building the 34 00:02:07.270 --> 00:02:10.300 island, all the way into the atmosphere and triggered a large 35 00:02:10.300 --> 00:02:14.680 tsunami, a 15 meter high super wave that traveled out hundreds 36 00:02:14.680 --> 00:02:18.430 of miles, buried some local islands as part of the Tonga 37 00:02:18.460 --> 00:02:21.790 archipelago, but allowed us to see the power of mother nature's 38 00:02:21.790 --> 00:02:26.530 volcanoes. When water and liquid rock come together to shape our 39 00:02:26.530 --> 00:02:26.950 planet. 40 00:02:28.240 --> 00:02:32.800 NASA and ESA satellites clocked wind speeds up to 450 miles per 41 00:02:32.800 --> 00:02:36.250 hour, just hours after the eruption in showed material 42 00:02:36.250 --> 00:02:40.150 rising up to 36 miles, the highest volcanic plume ever 43 00:02:40.150 --> 00:02:44.320 measured. Within two weeks, the main plume of volcanic materials 44 00:02:44.320 --> 00:02:47.440 circled the entire globe injecting dust particles into 45 00:02:47.440 --> 00:02:51.640 the stratosphere that remain for upwards of a year. NASA also 46 00:02:51.640 --> 00:02:54.610 found that the volcano injected a tremendous amount of water 47 00:02:54.610 --> 00:02:57.340 vapor into the Earth's stratosphere. The increase of 48 00:02:57.340 --> 00:03:00.670 water vapor which traps heat could modify atmospheric 49 00:03:00.670 --> 00:03:03.790 chemistry and have a warming effect on the Earth's surface. 50 00:03:06.610 --> 00:03:09.460 So outside of its sheer magnitude, what makes this 51 00:03:09.460 --> 00:03:13.000 eruption so unique? Well, it's really a matter of our ability 52 00:03:13.000 --> 00:03:17.440 to see it. At the end of 2021, the islands volcanic activity 53 00:03:17.440 --> 00:03:21.130 started picking up small underwater eruptions began to 54 00:03:21.130 --> 00:03:24.850 reshape the islands landscape expanding the island. These 55 00:03:24.850 --> 00:03:27.370 shallow water events are classified as cert saying 56 00:03:27.370 --> 00:03:30.820 eruptions were hot magma interacts explosively with 57 00:03:30.820 --> 00:03:34.960 water. In other words, we've been able to see the birth of 58 00:03:34.960 --> 00:03:38.380 the island happen in ways we haven't been able to before. And 59 00:03:38.380 --> 00:03:41.530 with modern satellite technology, we're also able to 60 00:03:41.530 --> 00:03:45.130 see the end of the islands lifecycle in new detail, as we 61 00:03:45.130 --> 00:03:46.780 did with the January eruption. 62 00:03:47.470 --> 00:03:50.170 This has happened in Earth's history in famous places like 63 00:03:50.170 --> 00:03:54.760 Yellowstone Taupo New Zealand, Krakatoa. And now in the island 64 00:03:54.790 --> 00:03:58.750 nation of Tonga, it's a we have an opportunity 21st century 65 00:03:58.750 --> 00:04:02.530 techniques, laser altimeters like ICESat, two satellite 66 00:04:02.530 --> 00:04:05.650 techniques that can see its scales of submitter put those 67 00:04:05.650 --> 00:04:09.520 together and tell a story of the birth and death of this island. 68 00:04:10.800 --> 00:04:12.330 NASA's vantage point of Hunga Tonga-Hunga Ha'apai could even 69 00:04:12.330 --> 00:04:13.470 be used as a means to study other planets in our solar 70 00:04:13.470 --> 00:04:14.790 system, specifically, the role that volcanic islands play in 71 00:04:14.790 --> 00:04:15.570 water planets like Mars and Venus. 72 00:04:15.570 --> 00:04:27.240 We live on an ocean planet. And so these kinds of eruptions are 73 00:04:27.240 --> 00:04:31.620 part of our history, how we got here, as we evolved ourselves in 74 00:04:31.620 --> 00:04:34.710 the context of our planet. And we want to take the lessons that 75 00:04:34.710 --> 00:04:38.430 we learn as we go forward as we continue to watch what's next in 76 00:04:38.430 --> 00:04:41.730 this exciting volcano, and apply it forward to other worlds like 77 00:04:41.730 --> 00:04:45.750 Mars and Venus that may have harbored surface waters as 78 00:04:45.780 --> 00:04:49.800 oceans or seas and understand them in the context of our 79 00:04:49.800 --> 00:04:50.130 Earth. 80 00:04:50.850 --> 00:04:54.450 Using geostationary satellites and observed data, NASA 81 00:04:54.450 --> 00:04:57.540 scientists hope to learn from the continuous evolution of this 82 00:04:57.540 --> 00:04:58.380 special volcano. 83 00:04:58.000 --> 00:05:02.980 The question is Will those come again on Hunga Tonga and then 84 00:05:03.040 --> 00:05:07.540 explode again? We don't know. So we need to use what we saw from 85 00:05:07.540 --> 00:05:11.740 this eruption in 22. To train ourselves for what to be able to 86 00:05:11.740 --> 00:05:16.540 predict. And so this is our chance to learn and then to 87 00:05:16.540 --> 00:05:19.780 apply it to the other ocean worlds nearby that we really 88 00:05:19.780 --> 00:05:20.650 hunger to study.