1 00:00:07,173 --> 00:00:10,110 TCarta is a marine remote sensing company. 2 00:00:10,110 --> 00:00:13,980 So what that means is we specialize in using Earth observation 3 00:00:13,980 --> 00:00:16,983 data, such as satellites, in order to map 4 00:00:17,083 --> 00:00:20,620 and identify features underneath the ocean. 5 00:00:21,087 --> 00:00:25,392 So we primarily specialize in coastal areas, areas where the water is shallow. 6 00:00:25,859 --> 00:00:27,260 That's the most dynamic area, 7 00:00:27,260 --> 00:00:30,263 and it's also the area where our technology works the best. 8 00:00:30,330 --> 00:00:34,034 TCarta, our primary products are going to be satellite-derived bathymetry, 9 00:00:34,267 --> 00:00:35,735 which, if you think about topography, 10 00:00:35,735 --> 00:00:37,804 bathymetry is just topography under the water. 11 00:00:37,804 --> 00:00:40,707 So basically elevation or depth of the water. 12 00:00:40,707 --> 00:00:45,111 We use ICESat-2, primarily the ATL-03 geolocated photon data product. 13 00:00:45,278 --> 00:00:46,780 That's our primary input. 14 00:00:46,780 --> 00:00:49,783 Even though ICESat’s original mission did not include bathymetry 15 00:00:49,783 --> 00:00:53,720 as one of its core sort of missions and therefore data products, 16 00:00:53,720 --> 00:00:58,491 the 532-nanometer blue-green laser is ideal for underwater mapping. 17 00:00:58,758 --> 00:01:01,561 And so there's been a lot of really good pioneering research on that that we kind 18 00:01:01,561 --> 00:01:04,764 of took along with us to create our the bathymetry product. 19 00:01:04,998 --> 00:01:08,068 After we've extracted bathymetry point measurements of ICESat-2, 20 00:01:08,435 --> 00:01:11,137 we typically are integrating those with a multispectral 21 00:01:11,137 --> 00:01:12,939 or hyperspectral satellite image. 22 00:01:12,939 --> 00:01:15,909 And that's what allows us to, basically delineate 23 00:01:15,909 --> 00:01:19,612 continuous seafloor models from these kind of disparate point data sets. 24 00:01:21,181 --> 00:01:24,551 And then we do have a large customer base of commercial users. 25 00:01:24,551 --> 00:01:25,852 So things like, 26 00:01:25,852 --> 00:01:29,556 engineering firms, you know, if they want to build a new hotel 27 00:01:29,656 --> 00:01:33,159 in an area where there's lots of protected structures, 28 00:01:33,159 --> 00:01:36,763 such as reefs or seagrass patches, having a seafloor classification model 29 00:01:36,763 --> 00:01:40,233 where they can develop their plan around low impact 30 00:01:40,233 --> 00:01:44,871 decisions can be very valuable, as well as quantifying volumetric change 31 00:01:44,871 --> 00:01:47,340 it might need to do in order to build something like an island. 32 00:01:47,340 --> 00:01:51,244 There are many, many places in the world that do not have sufficient in-situ data 33 00:01:51,244 --> 00:01:54,914 or depth measurements in order to to calibrate and validate these models. 34 00:01:55,348 --> 00:01:58,351 You know, kind of one of the reasons why we need to map these areas. 35 00:01:58,351 --> 00:02:02,489 And so having this data on its own won't satisfy the requirement 36 00:02:02,489 --> 00:02:06,926 for having a continuous map of, say, some really remote Pacific atoll, 37 00:02:07,227 --> 00:02:11,030 but having these point measurements, and then extrapolating across what we call 38 00:02:11,030 --> 00:02:14,567 the image space or within the image that we're using, it's really powerful. 39 00:02:15,001 --> 00:02:16,469 And, you know, some of these places, 40 00:02:16,469 --> 00:02:19,439 the last time anybody took a depth measurement was Captain Cook. 41 00:02:19,739 --> 00:02:22,008 Our motivation, or TCarta’s motivation, for joining 42 00:02:22,008 --> 00:02:24,310 ICESat-2’s Applied User Program and mission 43 00:02:24,310 --> 00:02:28,815 was basically exactly what I was talking about, is solving for 44 00:02:29,115 --> 00:02:32,252 that need for measurements of the water column 45 00:02:32,252 --> 00:02:35,955 that are recent or accurate and cover lots of different benthic types. 46 00:02:36,322 --> 00:02:39,659 You know, there's an insane amount of Earth observation, 47 00:02:39,692 --> 00:02:44,397 multispectral imagery around the world, from freely available data 48 00:02:44,430 --> 00:02:46,633 you know, Maxar commercial data, 49 00:02:46,633 --> 00:02:49,936 you know, Planet Labs, lots of, Airbus, lots of commercial data as well. 50 00:02:50,303 --> 00:02:53,540 But if you don't have anything to kind of confirm the results of your model 51 00:02:53,540 --> 00:02:56,776 or inform your model, depending on the approach you take, 52 00:02:56,809 --> 00:02:59,579 it's really hard to convey to the end users that this is a good product. 53 00:02:59,579 --> 00:03:02,015 It's also hard for us to have confidence in our product as well. 54 00:03:04,484 --> 00:03:07,387 We already have seen a global impact from using ICESat-2 data. 55 00:03:07,387 --> 00:03:12,759 So, I believe at this point, we've donated over 250,000 square kilometers of 56 00:03:12,859 --> 00:03:16,396 coastal bathymetry to Seabed 2030, 57 00:03:16,396 --> 00:03:19,399 which is a Nippon Foundation nonprofit effort. 58 00:03:19,432 --> 00:03:23,536 That's a really cool kind of amount, kind of effort across the globe 59 00:03:23,536 --> 00:03:26,940 for lots of different hydrographic offices and commercial agencies 60 00:03:26,940 --> 00:03:30,944 to procure and donate data to this effort to map the seafloor, 61 00:03:31,811 --> 00:03:34,447 regardless of depth, to a certain accuracy by 2030. 62 00:03:34,447 --> 00:03:39,185 And so using ICESat-2 informed data sets, we have been able to donate 63 00:03:39,185 --> 00:03:42,355 a large quantity of data to that effort, which is now made 64 00:03:42,355 --> 00:03:45,825 publicly available at a 100-meter or 90-meter resolution.