WEBVTT 00:00:04.530 --> 00:00:08.350 Susan: If you've ever spent time looking at satellite imagery of our planet, you 00:00:08.350 --> 00:00:12.110 might think that we know everything there is to know about the shape and depth 00:00:12.500 --> 00:00:14.519 or bathymetry of the global seafloor. 00:00:15.329 --> 00:00:18.509 After all, you can see details like canyons and seamounts. 00:00:20.290 --> 00:00:21.960 But what happens when you zoom in? 00:00:23.260 --> 00:00:24.790 These features begin to blur. 00:00:27.370 --> 00:00:29.620 The reality is, we don't yet have. 00:00:29.915 --> 00:00:35.155 A complete and detailed map of our planet's ocean floor, all 360 00:00:35.165 --> 00:00:36.765 million square kilometers of it. 00:00:38.535 --> 00:00:42.084 But more detailed maps of the seafloor are essential in our modern world. 00:00:42.925 --> 00:00:46.094 Understanding the shape and depth of the seafloor has implications 00:00:46.095 --> 00:00:50.435 for everything from safe navigation to ecosystem management and better 00:00:50.435 --> 00:00:52.294 understanding of Earth's climate system. 00:00:55.414 --> 00:00:59.034 To create high resolution maps that reveal underwater terrain in greater 00:00:59.034 --> 00:01:03.394 detail, Ocean explorers often use a tool called multibeam sonar. 00:01:05.315 --> 00:01:08.465 Here to tell us more is Derek Sowers, mapping operations manager 00:01:08.555 --> 00:01:09.755 for Ocean Exploration Trust. 00:01:11.955 --> 00:01:15.625 So Derek, we're here today to talk a bit about multibeam sonar mapping. 00:01:15.865 --> 00:01:19.775 Can you tell us a bit about how multibeam sonar generally works? 00:01:20.434 --> 00:01:23.074 Derek: Yeah, so with any sonar, essentially we're measuring 00:01:23.164 --> 00:01:24.164 the two way travel time. 00:01:24.304 --> 00:01:27.414 We send a, uh, acoustic pulse, a sound signal from the ship 00:01:27.920 --> 00:01:31.040 down to the seafloor, it bounces back and we listen for the echo. 00:01:31.510 --> 00:01:35.700 If we measure that two way travel time, we can derive the depth of 00:01:35.700 --> 00:01:36.960 the seafloor underneath the ship. 00:01:36.960 --> 00:01:38.560 So that's generally how the sonar works. 00:01:38.570 --> 00:01:42.150 For a multi beam sonar essentially you're doing that with many 00:01:42.150 --> 00:01:45.029 individual beams that are kind of in a fan shape underneath the ship. 00:01:46.190 --> 00:01:50.700 A good analogy for a multibeam sonar is basically a line of lasers 00:01:50.790 --> 00:01:55.539 in a row, moving along and sort of scanning the seafloor and building a 00:01:55.550 --> 00:01:57.410 map of the terrain as it moves along. 00:01:57.980 --> 00:02:01.020 But instead of light, we're using sound to do that. 00:02:01.755 --> 00:02:04.755 Susan: I understand that one of the benefits of multibeam sonar 00:02:04.755 --> 00:02:08.185 is that we can get incredible detail through high resolution. 00:02:08.555 --> 00:02:09.694 Um, can you tell us what that 00:02:09.694 --> 00:02:10.114 Derek: means? 00:02:10.215 --> 00:02:13.144 When most people look on Google Earth, they see that, oh, it looks 00:02:13.144 --> 00:02:14.534 like the ocean's already been mapped. 00:02:14.535 --> 00:02:15.565 We know where everything is. 00:02:16.605 --> 00:02:18.755 But it's really a matter of scale and resolution. 00:02:18.755 --> 00:02:21.874 So as you zoom in on those maps, you'll see that you don't really have 00:02:21.884 --> 00:02:23.454 fine detail like you would on land. 00:02:24.844 --> 00:02:28.405 We can get a general sense of the shape of the oceans from measurements 00:02:28.405 --> 00:02:33.185 made by satellites orbiting the Earth, but those are limited to between two 00:02:33.185 --> 00:02:34.805 and four kilometers in resolution. 00:02:35.985 --> 00:02:40.045 When you map from a ship using a multibeam sonar, you can map places in the deep 00:02:40.045 --> 00:02:43.975 sea to more like 50 meters resolution, so a much clearer picture of the seafloor. 00:02:45.965 --> 00:02:48.845 Susan: So how much of the seafloor has been mapped to that resolution? 00:02:50.385 --> 00:02:52.324 Derek: Only about 25 percent thus far. 00:02:52.454 --> 00:02:56.945 Um, so we're talking about publicly available data, um, but with collected 00:02:56.945 --> 00:02:58.394 with a modern multibeam system. 00:02:58.485 --> 00:02:59.535 So we have a long way to go. 00:02:59.600 --> 00:03:03.070 So 75 percent of the world's ocean is still really to be explored and mapped in 00:03:03.070 --> 00:03:04.640 this kind of detail for the first time. 00:03:05.290 --> 00:03:08.960 And then if you want to get even closer with that, either towing something 00:03:08.960 --> 00:03:12.550 that has a sonar on it or putting down a vehicle like a submersible 00:03:12.579 --> 00:03:16.099 that can get really close to the seafloor, uh, you can map, uh, down 00:03:16.099 --> 00:03:19.670 to a centimeter scale level and really reveal all the nooks and crannies. 00:03:21.750 --> 00:03:22.260 Susan: Wow. 00:03:22.380 --> 00:03:23.360 That's amazing. 00:03:24.940 --> 00:03:29.990 So I've heard we have better maps of Mars than we do of our own sea floor. 00:03:29.990 --> 00:03:30.620 Is that true? 00:03:31.780 --> 00:03:32.430 Derek: It is true. 00:03:32.460 --> 00:03:36.130 And the main reason that is true is because we can directly visualize 00:03:36.130 --> 00:03:39.940 the surface of Mars through the imagery we can gather, whereas we 00:03:39.940 --> 00:03:43.649 can't actually directly see the seafloor because we have these giant 00:03:43.650 --> 00:03:45.560 beautiful oceans obstructing our view. 00:03:45.960 --> 00:03:49.789 So the way we have to see the seafloor on Earth is to use sound through the 00:03:49.789 --> 00:03:51.350 sonars that we've been discussing. 00:03:52.540 --> 00:03:57.585 Susan: So, as you've said, So much of the ocean isn't mapped to high resolution, 00:03:57.695 --> 00:04:00.265 and there's so much still to be explored. 00:04:00.355 --> 00:04:02.734 It's going to take us years to do this. 00:04:03.165 --> 00:04:05.484 Why is high resolution mapping so 00:04:05.485 --> 00:04:05.965 Derek: important? 00:04:06.584 --> 00:04:10.894 For one thing, the oceans cover 71 percent of our planet, so if we don't have a good 00:04:11.015 --> 00:04:16.459 map for the majority of that then we're really missing out on understanding our 00:04:16.470 --> 00:04:21.050 planet and how it's evolved over time and the processes that are continuing to shape 00:04:21.050 --> 00:04:25.839 our planet, such as new seafloor being created, old seafloor being subducted 00:04:25.880 --> 00:04:28.870 into the trenches and disappearing, being recycled back into the earth. 00:04:29.510 --> 00:04:33.740 Um, this ties in with, uh, geologic hazards, natural hazards, 00:04:33.750 --> 00:04:37.540 such as tsunamis, underwater landslides, earthquakes. 00:04:38.349 --> 00:04:42.240 So these are things that really affect the safety of the coastal zone for many of us. 00:04:43.350 --> 00:04:46.580 Any infrastructure we put in the ocean, we need to have good maps so we can 00:04:47.250 --> 00:04:50.850 do proper sighting of things like wind farms or telecommunication cables. 00:04:51.740 --> 00:04:54.669 And then more in terms of understanding the ecosystem of the ocean. 00:04:54.670 --> 00:04:59.220 If we don't have a good base map, then that's kind of the fundamental first step 00:04:59.250 --> 00:05:03.119 of understanding the marine environment, understanding marine habitats, what 00:05:03.130 --> 00:05:07.289 species can live where, and, you know, that's, we can't even begin to 00:05:07.289 --> 00:05:09.070 do that without a map to begin with. 00:05:09.070 --> 00:05:12.825 Susan: Can you tell us a bit about how multibeam sonar 00:05:12.825 --> 00:05:17.335 fits into the full exploration strategy, the modern exploration 00:05:17.335 --> 00:05:17.865 Derek: strategy? 00:05:18.034 --> 00:05:19.394 Sure, yeah, it's a great question. 00:05:19.425 --> 00:05:22.775 I mean, I think it's basically, uh, multibeam sonar mapping 00:05:22.775 --> 00:05:27.184 is considered, like, the first step in exploring the ocean. 00:05:27.185 --> 00:05:30.094 So, you've got to go out and get a good base map before 00:05:30.094 --> 00:05:31.294 you do further exploration. 00:05:31.294 --> 00:05:36.284 And then, that map usually reveals The logical next step, so you'll usually 00:05:36.284 --> 00:05:41.205 make discoveries of interesting features, new terrain that you didn't expect to 00:05:41.205 --> 00:05:44.905 see, or maybe you are searching for a specific feature, you want to see where 00:05:44.905 --> 00:05:49.025 you think deep sea corals are going to be, or undersea volcano, or a shipwreck 00:05:49.064 --> 00:05:53.224 that you discover, so you usually reveal those things through mapping, and then the 00:05:53.225 --> 00:05:57.525 next step is to go and explore features of interest in more detail using things 00:05:57.525 --> 00:06:02.024 like remotely operated vehicles, or autonomous underwater vehicles, that's 00:06:02.205 --> 00:06:06.670 giving you that close up imagery, and better understanding and the ability 00:06:06.670 --> 00:06:11.060 to take biological or geological samples, you know, to further understand 00:06:11.130 --> 00:06:12.720 what's going on in these ecosystems. 00:06:15.600 --> 00:06:17.860 Susan: Derek, how do you decide where you're going to map? 00:06:18.520 --> 00:06:22.590 Derek: We're putting a lot of effort into exploring America's undersea territory. 00:06:22.590 --> 00:06:27.260 So there's about 3 billion acres that we have yet to explore that's actually U. 00:06:27.260 --> 00:06:27.699 S. 00:06:27.700 --> 00:06:28.330 territory. 00:06:29.470 --> 00:06:32.880 So it's really like doing the Lewis and Clark expedition, except about 00:06:32.880 --> 00:06:34.590 six times over and underwater. 00:06:35.360 --> 00:06:36.230 It's a huge mission. 00:06:36.500 --> 00:06:37.880 We're part of that effort. 00:06:38.359 --> 00:06:41.890 That's a NOAA wide initiative as well to go out and explore our 00:06:41.890 --> 00:06:43.669 own country's undersea territory. 00:06:44.929 --> 00:06:48.289 And beyond that, we're interested in the rest of the world's oceans as well. 00:06:49.470 --> 00:06:53.540 So, we decide those priorities mostly in consultation with scientists 00:06:53.540 --> 00:06:57.830 around the world that really have driving science questions, wanting 00:06:57.830 --> 00:07:00.850 to understand and expand our knowledge of the marine environment. 00:07:03.400 --> 00:07:06.759 It's important as an exploration program, we're trying to go to 00:07:06.759 --> 00:07:08.519 places that haven't been explored. 00:07:09.500 --> 00:07:13.799 Our mission is to go get the first look at places where we know almost nothing. 00:07:17.745 --> 00:07:21.185 Susan: What's one of the biggest surprises you've ever had, uh, in mapping 00:07:21.185 --> 00:07:21.795 Derek: the seafloor? 00:07:22.055 --> 00:07:26.005 Uh, I think one of the biggest surprises I personally had was one of my first 00:07:26.084 --> 00:07:28.915 mapping expeditions that I was leading. 00:07:28.925 --> 00:07:30.594 I was, uh, off the southeast U. 00:07:30.594 --> 00:07:30.715 S. 00:07:30.715 --> 00:07:34.455 coast, so not far off one of the most populated parts of the U. 00:07:34.455 --> 00:07:34.745 S. 00:07:35.254 --> 00:07:40.094 Uh, and we had known there was deep sea coral mounds out there, but the 00:07:40.134 --> 00:07:42.025 full extent had never been mapped yet. 00:07:42.465 --> 00:07:46.400 And so, this one expedition I was just shocked at the number of mounds, 00:07:46.430 --> 00:07:50.230 we found thousands and thousands of mounds in just like 10 days of 00:07:50.230 --> 00:07:52.380 mapping with the deep water multibeam. 00:07:53.229 --> 00:07:57.149 So really, just seeing this vast landscape that would probably be a national 00:07:57.149 --> 00:07:58.720 park if it was unlanded, honestly. 00:07:59.690 --> 00:08:01.040 You just never know what you're going to find. 00:08:01.679 --> 00:08:03.970 So yeah, there's many, many stories like that. 00:08:10.760 --> 00:08:11.210 So that 00:08:11.210 --> 00:08:14.280 Susan: said, Derek, what do you see as the future for mapping 00:08:14.280 --> 00:08:14.990 Derek: the seafloor? 00:08:15.585 --> 00:08:20.765 I think we'll greatly see an expansion of the use of uncrewed systems to map 00:08:21.295 --> 00:08:26.545 larger areas more quickly with a lower carbon footprint and in higher resolution. 00:08:26.575 --> 00:08:29.215 So this will reveal a whole new level of understanding 00:08:29.215 --> 00:08:31.174 of what our oceans look like. 00:08:32.005 --> 00:08:36.444 We'll have much greater insights into the habitat they provide for life on 00:08:36.444 --> 00:08:40.624 Earth, and hopefully we become better stewards of the marine environment 00:08:40.644 --> 00:08:41.884 with all this new understanding. 00:08:44.104 --> 00:08:44.854 Susan: Excellent goal. 00:08:46.004 --> 00:08:48.084 Thank you for your time and for what you 00:08:48.084 --> 00:08:48.724 Derek: do for a living. 00:08:49.400 --> 00:08:50.020 My pleasure. 00:08:50.070 --> 00:08:51.360 Thanks for the interview.