1 00:00:00,000 --> 00:00:00,867 [Upbeat Music] 2 00:00:00,867 --> 00:00:02,268 Narrator: Where are you right now? 3 00:00:02,268 --> 00:00:04,571 Or better yet, how do you know where you are? 4 00:00:05,305 --> 00:00:08,808 Most likely you are using an app that is using a GPS 5 00:00:08,842 --> 00:00:11,444 to pinpoint where exactly you are on Earth. 6 00:00:12,245 --> 00:00:15,181 But what you might not know is that behind your favorite navigation 7 00:00:15,181 --> 00:00:16,349 app is an invisible 8 00:00:16,349 --> 00:00:20,687 infrastructure of systems working together to provide you an accurate location, 9 00:00:21,287 --> 00:00:24,491 and that the foundation of these systems is a TRF 10 00:00:24,491 --> 00:00:26,793 or terrestrial reference frame. 11 00:00:27,861 --> 00:00:31,998 Dr. Stephen Merkowitz: So reference frame is fundamental 12 00:00:32,032 --> 00:00:37,771 to any kind of mapping, location, positioning, navigation application. 13 00:00:37,804 --> 00:00:42,976 Narrator: That's Dr. Stephen Merkowitz, NASA's Space Geodesy Project Manager 14 00:00:43,076 --> 00:00:45,345 Simply put, geodesy is the science 15 00:00:45,345 --> 00:00:47,914 of measuring and understanding the shape of the Earth, 16 00:00:48,348 --> 00:00:52,619 its orientation in space and gravity, and how they change over time. 17 00:00:53,019 --> 00:00:57,891 Dr. Stephen Merkowitz: Earth is constantly changing shape, and the land masses are constantly moving. 18 00:00:57,924 --> 00:01:02,095 It's at small levels, so it's not something you would feel, you know, yourself. 19 00:01:02,228 --> 00:01:04,197 So we're constantly measuring 20 00:01:04,197 --> 00:01:07,801 what's happening with the Earth as a whole and the Earth's surface. 21 00:01:08,034 --> 00:01:11,671 Narrator: To do this, NASA and international partners monitor measurement 22 00:01:11,671 --> 00:01:15,475 stations dotted across the globe that help us determine where, 23 00:01:15,742 --> 00:01:18,812 how much and in which direction our planet is changing. 24 00:01:19,646 --> 00:01:22,582 Dr. Stephen Merkowitz: Since the Earth's surface is always moving, any measurement 25 00:01:22,682 --> 00:01:24,851 isn't just in a fixed coordinate system. 26 00:01:24,851 --> 00:01:26,319 It needs to take into account 27 00:01:26,319 --> 00:01:27,620 the fact that it's related 28 00:01:27,620 --> 00:01:31,491 to the landmass and where that landmass is at any given time. 29 00:01:31,524 --> 00:01:34,427 Narrator: And just like a coordinate system plotted on a piece of paper, 30 00:01:34,627 --> 00:01:38,565 the TRF has an origin or in this case, the center mass of the 31 00:01:38,565 --> 00:01:40,200 Earth - called the geocenter. 32 00:01:41,801 --> 00:01:44,104 Because of this, many Earth observing satellites 33 00:01:44,104 --> 00:01:48,675 orbit around the center mass of the Earth, not the Earth's geographic center. 34 00:01:49,042 --> 00:01:52,245 So it's critical for scientists to pinpoint where that is 35 00:01:52,245 --> 00:01:54,647 to make sure our Earth observations are accurate. 36 00:01:54,681 --> 00:01:57,250 Dr. Stephen Merkowitz: One complication is that the center mass of the Earth 37 00:01:57,851 --> 00:02:00,186 is constantly changing over time 38 00:02:00,353 --> 00:02:02,555 with respect to the Earth's surface. 39 00:02:02,555 --> 00:02:06,759 Narrator: Earthquakes, volcanoes, or even atmospheric pressure changes all impact 40 00:02:06,759 --> 00:02:09,395 where exactly the center mass of the Earth is. 41 00:02:10,363 --> 00:02:14,400 But by using a network of ground stations equipped with telescopes and lasers 42 00:02:14,400 --> 00:02:18,705 that fire pulses at specific satellites, scientists can calculate 43 00:02:18,738 --> 00:02:23,710 where the geocenter of the Earth is at any given time to a few millimeters. 44 00:02:23,943 --> 00:02:28,781 Dr. Stephen Merkowitz: This is a very important product that we generate for orbiting satellites, 45 00:02:28,781 --> 00:02:30,717 particularly for missions 46 00:02:30,717 --> 00:02:34,320 that are either doing mapping the gravitational field of the Earth or 47 00:02:35,054 --> 00:02:38,825 mapping the height of the Earth's surface, whether it be land, vegetation, 48 00:02:38,825 --> 00:02:40,293 or sea level. 49 00:02:40,293 --> 00:02:42,362 We make that available to the public, 50 00:02:42,362 --> 00:02:45,498 we use the data there to generate a higher level 51 00:02:45,665 --> 00:02:49,569 of products, geodetic products, that can be used by NASA missions 52 00:02:50,170 --> 00:02:53,439 for many scientific applications. 53 00:02:53,673 --> 00:02:57,277 Since this is a global measurement, NASA can't do it alone. 54 00:02:57,610 --> 00:03:00,079 We rely on the global community to 55 00:03:00,680 --> 00:03:04,551 provide all the data that's needed to provide global coverage. 56 00:03:06,686 --> 00:03:07,520 Narrator: Having an agreed 57 00:03:07,520 --> 00:03:11,257 upon international system is what makes measuring our planet possible, 58 00:03:11,591 --> 00:03:16,029 whether it be from land, sea, air, or even space.