WEBVTT FILE 1 00:00:00.030 --> 00:00:03.330 My name is Kelsey Young and I'm a Planetary scientist at the NASA Goddard 2 00:00:03.330 --> 00:00:06.569 Space Flight Center and so switching gears a little bit we're gonna talk 3 00:00:06.569 --> 00:00:09.809 about the moon for the next few minutes and so what we're gonna do is talk about 4 00:00:09.809 --> 00:00:13.290 the Lunar Reconnaissance Orbiter which is one of NASA's spacecrafts orbiting 5 00:00:13.290 --> 00:00:16.109 the moon right now and we're also going to talk about how that Lunar 6 00:00:16.109 --> 00:00:19.650 Reconnaissance Orbiter spacecraft pertains to NASA's ARTEMIS program which 7 00:00:19.650 --> 00:00:24.600 is NASA's plan right now to put the first woman in the next man on the lunar 8 00:00:24.600 --> 00:00:29.970 surface so what we want to do first if we could start this video over is take 9 00:00:29.970 --> 00:00:34.020 sort of a tour of the moon the reason for doing that is kind of highlighting 10 00:00:34.020 --> 00:00:38.190 NASA's LRO or Lunar Reconnaissance Orbiter spacecraft which has been 11 00:00:38.190 --> 00:00:41.610 orbiting the moon now for over a decade collecting data from a number of 12 00:00:41.610 --> 00:00:44.730 different instrument suites so we're gonna through the lens of those 13 00:00:44.730 --> 00:00:48.030 different instruments on the LRO spacecraft take a look at what we're 14 00:00:48.030 --> 00:00:51.870 able to learn on the moon now as we prepare to put people and boots on the 15 00:00:51.870 --> 00:00:55.020 ground back on the lunar surface it's a really exciting time to be a lunar 16 00:00:55.020 --> 00:01:01.620 geologist so sort of our first stop on the tour is the Oriental impact Basin so 17 00:01:01.620 --> 00:01:04.860 this is a really compelling impact crater feature that we can learn a lot 18 00:01:04.860 --> 00:01:09.390 about through the lens of this GRAIL data set or a data set looking at the 19 00:01:09.390 --> 00:01:12.960 gravity of the lunar surface so we can actually peer through the subset and 20 00:01:12.960 --> 00:01:16.439 look at that gravity information which can help us prepare for human 21 00:01:16.439 --> 00:01:20.430 spaceflight on the lunar surface we're now going continuing on our tour to the 22 00:01:20.430 --> 00:01:24.030 lunar South Pole which is where we're going to be sending astronauts as a part 23 00:01:24.030 --> 00:01:27.299 of the ARTEMIS program and those highlighted areas are actually areas 24 00:01:27.299 --> 00:01:31.740 where we think there might be water ice on the lunar surface which is where we 25 00:01:31.740 --> 00:01:36.390 want to send humans to look at how to use that ice to potentially stay 26 00:01:36.390 --> 00:01:40.200 long-term so we're kind of zooming in to the South Pole here and this is a really 27 00:01:40.200 --> 00:01:44.100 exciting time because hopefully we're gonna have astronauts walking around in 28 00:01:44.100 --> 00:01:49.049 Shackleton crater or nearby on the South Pole of the moon but we're zooming back 29 00:01:49.049 --> 00:01:53.369 away we're gonna return to talk about the South Pole later in this talk as we 30 00:01:53.369 --> 00:01:58.140 again prepare for that ARTEMIS program so what you're seeing here is again just 31 00:01:58.140 --> 00:02:02.399 like Oriental we're seeing big impact craters and the biggest of them all is 32 00:02:02.399 --> 00:02:05.939 the South Pole Achan basin on the lunar far side we 33 00:02:05.939 --> 00:02:09.090 don't know the exact age of this structure but it's a really high 34 00:02:09.090 --> 00:02:11.910 priority science objective for when we go back to the lunar 35 00:02:11.910 --> 00:02:16.560 surface so we're now continuing to spin around moving away from the South Pole 36 00:02:16.560 --> 00:02:20.070 even though we'll be going back with humans soon and we're gonna zoom in on 37 00:02:20.070 --> 00:02:24.900 another really compelling structure here a lot of lunar science focuses on Impact 38 00:02:24.900 --> 00:02:28.680 cratering and Volcanology and one of those big impact craters right here is 39 00:02:28.680 --> 00:02:34.110 the Tycho structure the LRO spacecraft affords us really high-resolution 40 00:02:34.110 --> 00:02:37.770 pictures of the lunar surface which is great for when we're preparing to send 41 00:02:37.770 --> 00:02:41.460 humans back to the surface and to give you a sense for how high-resolution it 42 00:02:41.460 --> 00:02:45.540 is that Boulder right there on the top of that central peak is a hundred meters 43 00:02:45.540 --> 00:02:49.500 across and we're able to get really crisp resolution on it and those images 44 00:02:49.500 --> 00:02:53.540 are great for science and they're also great to prep for human exploration 45 00:02:53.540 --> 00:02:58.620 continuing on we're gonna head to a more volcanic feature called Aristarchus 46 00:02:58.620 --> 00:03:03.090 plateau where we see yes impact craters but also some volcanic deposits as well 47 00:03:03.090 --> 00:03:06.990 this has long been a really compelling science target for lunar science we have 48 00:03:06.990 --> 00:03:10.200 a lot left to learn about that and through instrumentation on the LRO 49 00:03:10.200 --> 00:03:13.770 spacecraft it can give us a sense for what that surface is made out of and we 50 00:03:13.770 --> 00:03:18.720 can start to pick apart how these landscapes form but it's not just kind 51 00:03:18.720 --> 00:03:22.709 of going forward it's also learning a lot about where we've already been we've 52 00:03:22.709 --> 00:03:27.060 learned a lot about lunar science and in the last decade in the last decades and 53 00:03:27.060 --> 00:03:30.870 one example of that is zooming in on where humans have been on the lunar 54 00:03:30.870 --> 00:03:35.310 surface and one of those places is the Taurus Littrow valley which is where 55 00:03:35.310 --> 00:03:39.570 astronauts explore the lunar surface through the Apollo 17 mission so what 56 00:03:39.570 --> 00:03:44.220 you'll see here is data from the LRO spacecraft so high you can actually see 57 00:03:44.220 --> 00:03:47.340 the traverses that the Apollo astronauts took on the moon you see there are three 58 00:03:47.340 --> 00:03:52.770 e bas or spacewalks that they took here and zooming in even further I love this 59 00:03:52.770 --> 00:03:56.940 you can actually see the lander where the astronauts landed and you know of 60 00:03:56.940 --> 00:04:00.870 course left their their landing stage there and as you traverse over here you 61 00:04:00.870 --> 00:04:04.739 can actually see the rover which is what the astronauts used to of course drive 62 00:04:04.739 --> 00:04:07.800 around and explore on the lunar surface we're hopefully going to be doing this 63 00:04:07.800 --> 00:04:11.910 again really really soon and one of our last stops on the tour is actually 64 00:04:11.910 --> 00:04:15.540 heading up we've been to the South Pole now we're heading to the North Pole and 65 00:04:15.540 --> 00:04:19.320 the North Pole is also a really compelling science target we have a lot 66 00:04:19.320 --> 00:04:22.099 to learn about potentially using volatile x' we might 67 00:04:22.099 --> 00:04:26.060 find therefore in situ resource utilization and so you can see there's a 68 00:04:26.060 --> 00:04:28.970 lot of compelling science to be left on the moon and the Lunar Reconnaissance 69 00:04:28.970 --> 00:04:33.650 Orbiter is a great way that can tell us about what to expect through its whole 70 00:04:33.650 --> 00:04:38.479 host of diverse set of instruments so we'll continue on here 71 00:04:38.479 --> 00:04:43.789 this is actually a crater on the lunar far side and this is actually a data set 72 00:04:43.789 --> 00:04:48.229 that was taken before the Lunar Reconnaissance Orbiter got to the moon 73 00:04:48.229 --> 00:04:52.280 so you can see it's pretty fuzzy we really didn't have crisp data this is 74 00:04:52.280 --> 00:04:56.419 interesting scientifically right Lunar Reconnaissance Orbiter gave us a lot in 75 00:04:56.419 --> 00:05:00.139 terms of the resolution of data we have on the moon but think about planning a 76 00:05:00.139 --> 00:05:03.680 mission to the moon with people with data sets like these it's really the 77 00:05:03.680 --> 00:05:06.620 data obtained by the Lunar Reconnaissance Orbiter that enables us 78 00:05:06.620 --> 00:05:11.240 to plan for NASA's Artemis program here is a picture of the same exact spot on 79 00:05:11.240 --> 00:05:14.690 the lunar surface with the data obtained with the Lunar Reconnaissance Orbiter 80 00:05:14.690 --> 00:05:20.030 spacecraft so just to flip back and forth there the LRO spacecraft enables 81 00:05:20.030 --> 00:05:23.810 us to answer these high-priority science questions like the age of the South Pole 82 00:05:23.810 --> 00:05:27.650 lake and basin and allow us to also prepare for when we're gonna want to 83 00:05:27.650 --> 00:05:32.509 send people there it can also not just give us this this great visual imagery 84 00:05:32.509 --> 00:05:35.960 but other missions we've sent to the lunar surface can allow us to peer 85 00:05:35.960 --> 00:05:40.430 beneath the surface so while we want to use these photos and images to design 86 00:05:40.430 --> 00:05:43.940 traverse plans and to answer science questions we also want to probe beneath 87 00:05:43.940 --> 00:05:47.750 the surface and the GRAIL mission actually enabled us to get a look at the 88 00:05:47.750 --> 00:05:52.639 gravity of the lunar surface which helps us understand how that how that moon 89 00:05:52.639 --> 00:05:58.550 evolved and also where it's going in the future so here is actually a look at the 90 00:05:58.550 --> 00:06:03.139 Apollo 11 mission we just passed the 50th anniversary of that mission you can 91 00:06:03.139 --> 00:06:07.729 actually see each kind of stage of that mission there and actually you can even 92 00:06:07.729 --> 00:06:11.719 see the boot tracks that Neil Armstrong took on the lunar surface this really 93 00:06:11.719 --> 00:06:15.380 allows us to place the science scientific samples the geology samples 94 00:06:15.380 --> 00:06:19.849 and even greater context than we ever had before and allow us to really get a 95 00:06:19.849 --> 00:06:23.449 look at where they sampled and here's a great example of looking at the Traverse 96 00:06:23.449 --> 00:06:28.370 of that Neil Armstrong and Buzz Aldrin took we're able to take those Apollo 11 97 00:06:28.370 --> 00:06:32.270 samples and understand even more about them now that we know exactly where they 98 00:06:32.270 --> 00:06:34.980 went and actly what the context of those samples 99 00:06:34.980 --> 00:06:38.670 are so you're able to see the crater that Neil Armstrong and Buzz Aldrin 100 00:06:38.670 --> 00:06:41.940 actually had to change last minute their landing site because they had to skim 101 00:06:41.940 --> 00:06:44.940 right over the rim of that crater that they didn't know was there because they 102 00:06:44.940 --> 00:06:52.050 didn't have data that like we're looking at right now so just to give you another 103 00:06:52.050 --> 00:06:56.760 sense of the type of data that LRO is able to collect obviously what you're 104 00:06:56.760 --> 00:06:59.940 noticing here is changing in the middle of the screen there you see a bright 105 00:06:59.940 --> 00:07:03.750 flash and sort of a white spot up here on the image that's actually a new 106 00:07:03.750 --> 00:07:07.080 impact crater that formed since the lifetime of the Lunar Reconnaissance 107 00:07:07.080 --> 00:07:11.280 Orbiter orbiting the moon so the first time it took a picture of this area that 108 00:07:11.280 --> 00:07:15.240 crater was not there the next time it imaged that area the crater was there 109 00:07:15.240 --> 00:07:19.680 what this is telling us is in many ways the moon is still an active place there 110 00:07:19.680 --> 00:07:23.190 are surface processes that are changing the surface of this our nearest 111 00:07:23.190 --> 00:07:28.710 celestial neighbor in observable time and we've observed hundreds of these new 112 00:07:28.710 --> 00:07:33.360 impact craters forming in the ten plus years that LRO has been at the moon and 113 00:07:33.360 --> 00:07:37.620 what does this tell us well space is still an active place also you don't 114 00:07:37.620 --> 00:07:40.200 want to be an astronaut that was standing right underneath where that 115 00:07:40.200 --> 00:07:44.370 object hit the surface of the Moon right so it's helping us to predict how often 116 00:07:44.370 --> 00:07:48.750 these small impact craters are formed on the lunar surface and it also tells us 117 00:07:48.750 --> 00:07:52.530 something about the cratering process as well as how to prepare for the type of 118 00:07:52.530 --> 00:07:56.310 hardware we want to design to explore the lunar surface so the moon is a 119 00:07:56.310 --> 00:07:59.700 really dynamic place the Lunar Reconnaissance Orbiter is helping us 120 00:07:59.700 --> 00:08:07.290 explore that here once again is the Taurus Littrow valley so again this is 121 00:08:07.290 --> 00:08:10.980 the site where the Apollo 17 mission visited the moon this is the last time 122 00:08:10.980 --> 00:08:14.310 we had astronauts on the moon and one thing I kind of want to emphasize today 123 00:08:14.310 --> 00:08:17.700 is you know this is the last time we've put boots on the ground on the lunar 124 00:08:17.700 --> 00:08:21.930 surface as I mentioned earlier NASA's Artemis program is seeking to bring them 125 00:08:21.930 --> 00:08:26.040 back in fact today is NASA's Artemis today I'm not sure if you guys saw that 126 00:08:26.040 --> 00:08:30.690 on social media or anything NASA's Artemis Day is as kind of a way 127 00:08:30.690 --> 00:08:33.330 to bring attention to the ARTEMIS program but what really happened today 128 00:08:33.330 --> 00:08:39.000 is the first time that the core stage of the SLS rocket was assembled at the 129 00:08:39.000 --> 00:08:42.639 Michoud NASA Center down in near New Orleans so today is 130 00:08:42.639 --> 00:08:47.019 NASA day and and and why or excuse me today is NASA's ARTEMIS day and and why 131 00:08:47.019 --> 00:08:50.350 do we have ARTEMIS day well again I think this is a great place to talk 132 00:08:50.350 --> 00:08:54.730 about it this is the last time we've had people on the moon and and today a 133 00:08:54.730 --> 00:09:02.709 really big step was just taken to bring us back and so with that lens in mind 134 00:09:02.709 --> 00:09:07.720 here is a picture boots on the ground from that Taurus Littrow valley Apollo 135 00:09:07.720 --> 00:09:11.649 17 landing site so we just saw a picture taken you know from one of the cameras 136 00:09:11.649 --> 00:09:15.250 on the Lunar Reconnaissance Orbiter spacecraft and here is a picture taken 137 00:09:15.250 --> 00:09:20.560 from the ground this is astronaut Jack Schmitt taking a sample on the lunar 138 00:09:20.560 --> 00:09:24.730 surface on the left side there you'll see the lunar roving vehicle this is a 139 00:09:24.730 --> 00:09:28.209 small rover that the astronauts were able to use to travel even greater 140 00:09:28.209 --> 00:09:33.220 distances away from their landing site as well as to store samples and store 141 00:09:33.220 --> 00:09:36.459 sampling equipment I do a lot of fieldwork here on earth I'm a field 142 00:09:36.459 --> 00:09:40.810 geologist by training I would love to have a roving field assistant that would 143 00:09:40.810 --> 00:09:43.899 come with me on all my fieldwork to be able to carry all of my equipment and 144 00:09:43.899 --> 00:09:48.009 especially those heavy rocks once I pick them up so we learned a lot from this 145 00:09:48.009 --> 00:09:50.829 mission we learned a lot from all the Apollo missions we especially learned a 146 00:09:50.829 --> 00:09:55.750 lot from Apollo 17 that guy right there Jack Schmitt was a geologist prior to 147 00:09:55.750 --> 00:09:58.930 becoming an astronaut so we actually put a scientist on the moon in this mission 148 00:09:58.930 --> 00:10:03.100 we learned a lot about how to sample on the moon actually if you head over to 149 00:10:03.100 --> 00:10:06.310 that NASA booth but later you can actually see some of the the hardware 150 00:10:06.310 --> 00:10:09.819 that we were able to not the exact hardware that's a museum it's about 151 00:10:09.819 --> 00:10:12.939 mock-ups of the tools that we were able to use on the Apollo on the lunar 152 00:10:12.939 --> 00:10:16.870 surface and Apollo and it was really you know these missions that taught us a lot 153 00:10:16.870 --> 00:10:20.079 about the properties of the lunar surface and and I can tell you that 154 00:10:20.079 --> 00:10:23.319 right now we're taking a lot of these lessons learned that these of these 155 00:10:23.319 --> 00:10:26.680 astronauts taught us and we're applying them to where we're going with the 156 00:10:26.680 --> 00:10:32.589 ARTEMIS program so this is kind of a movie showing illumination conditions at 157 00:10:32.589 --> 00:10:36.850 the lunar South Pole again NASA's ARTEMIS program is going to push the 158 00:10:36.850 --> 00:10:39.550 first woman and the next man on the lunar surface and we're going to the 159 00:10:39.550 --> 00:10:43.779 South Pole so we don't know exactly the x marks the spot on the lunar surface 160 00:10:43.779 --> 00:10:46.779 where these astronauts are going we do know that it'll be near the South Pole 161 00:10:46.779 --> 00:10:51.279 and what these data are showing you is actually the illumination conditions 162 00:10:51.279 --> 00:10:55.749 the pole and so you can see that we're marching through the Year 2024 down here 163 00:10:55.749 --> 00:11:00.100 in 2024 is the year that we've been charged with for when we want to put 164 00:11:00.100 --> 00:11:03.939 these astronauts on the surface and so what you're seeing here is is kind of a 165 00:11:03.939 --> 00:11:08.470 time-lapse of what it will look like in terms of illumination when we are able 166 00:11:08.470 --> 00:11:12.309 to put to put astronauts on the lunar surface so just for a minute 167 00:11:12.309 --> 00:11:15.309 picture that you're one of those astronauts you're landing on the lunar 168 00:11:15.309 --> 00:11:19.269 surface you want to do geology you want to plant the flag you want to learn 169 00:11:19.269 --> 00:11:22.749 about all these science questions that we've talked about that we're learning a 170 00:11:22.749 --> 00:11:26.860 lot about from the Lunar Reconnaissance Orbiter the lighting conditions at the 171 00:11:26.860 --> 00:11:31.300 pole just given orbital dynamics and where the moon is versus the Sun make it 172 00:11:31.300 --> 00:11:36.730 pretty complex to work at the South Pole lighting can be a challenge even in the 173 00:11:36.730 --> 00:11:40.990 Apollo missions the astronauts noted that the sort of semi oblique lighting 174 00:11:40.990 --> 00:11:44.559 angles that they were working with made it hard to judge distance they couldn't 175 00:11:44.559 --> 00:11:48.430 tell how far they were from a site of interest they knew that the crater rim 176 00:11:48.430 --> 00:11:52.120 they wanted to reach was just over there but it looked a lot shorter than the 177 00:11:52.120 --> 00:11:55.839 distance actually was just because of the way the light was playing over their 178 00:11:55.839 --> 00:11:59.980 landing site versus the lighting they're used to operating in on the Earth's 179 00:11:59.980 --> 00:12:03.459 surface in training the South Pole is is a different beast 180 00:12:03.459 --> 00:12:08.079 it's even more complex illumination will be a challenge we're working on right 181 00:12:08.079 --> 00:12:12.459 now how to what kind of challenge that will be how to train the astronauts to 182 00:12:12.459 --> 00:12:15.939 prepare them for that challenge how to make sure the hardware can withstand 183 00:12:15.939 --> 00:12:20.740 that challenge and I really love this image because right now scientists are 184 00:12:20.740 --> 00:12:24.160 preparing for how to do science in these illumination conditions but more 185 00:12:24.160 --> 00:12:27.639 importantly the operators who are designing Rover hardware and spacesuit 186 00:12:27.639 --> 00:12:31.059 hardware and training the astronauts and how to operate in those conditions are 187 00:12:31.059 --> 00:12:35.620 looking at visuals just like this to prepare us for what that exploration is 188 00:12:35.620 --> 00:12:39.550 going to look like so next time you're kind of outside if you do field work or 189 00:12:39.550 --> 00:12:43.179 even if you just go on a hike imagine trying to do that and you know execute 190 00:12:43.179 --> 00:12:47.290 your traverse plan in these really really variable lighting conditions and 191 00:12:47.290 --> 00:12:50.679 I really just want to stress that the Lunar Reconnaissance Orbiter is the 192 00:12:50.679 --> 00:12:54.370 spacecraft that's really enabled us to get these really great datasets that 193 00:12:54.370 --> 00:12:58.569 help tell us hey there's a lot of science left to learn on the moon we've 194 00:12:58.569 --> 00:13:02.279 gone back and looked at the Apollo landing sites in a lot greater detail 195 00:13:02.279 --> 00:13:05.459 and understood the samples that those astronauts collected and placed them in 196 00:13:05.459 --> 00:13:09.899 even a higher resolution context than we ever had before and I'm a you know I'm a 197 00:13:09.899 --> 00:13:12.990 geologist who thinks about science integration into human spaceflight so 198 00:13:12.990 --> 00:13:15.990 hear a lot about field geology and I especially care about doing field 199 00:13:15.990 --> 00:13:20.069 geology on the moon and so here we are training astronauts designing Hardware 200 00:13:20.069 --> 00:13:24.209 designing sampling and science hardware Institue analytical hardware but also 201 00:13:24.209 --> 00:13:27.629 the hardware that's going to keep our astronauts alive in terms of Rover 202 00:13:27.629 --> 00:13:31.769 spacesuit technology sampling technology and it's these kind of data sets they're 203 00:13:31.769 --> 00:13:36.329 gonna help get us there so again just to reflect back you know we've seen a lot 204 00:13:36.329 --> 00:13:40.499 of amazing imagery of the moon amazing data from the moon the Lunar 205 00:13:40.499 --> 00:13:44.430 Reconnaissance Orbiter spacecraft is kind of what's helping us get there 206 00:13:44.430 --> 00:13:48.629 but we're looking forward to the future and that's the ARTEMIS program like I 207 00:13:48.629 --> 00:13:52.829 mentioned today is ARTEMIS day and again that means that the SLS rocket or the 208 00:13:52.829 --> 00:13:57.420 rocket that's going to launch astronauts that will one day explore the moon has 209 00:13:57.420 --> 00:14:01.350 had its core stage assembled for the first time so what that means is this is 210 00:14:01.350 --> 00:14:06.329 a massive many years in the making step that really gets us one huge, huge, huge 211 00:14:06.329 --> 00:14:09.959 leap forward and in putting in putting humans back on the moon on the ARTEMIS 212 00:14:09.959 --> 00:14:13.230 program and one thing we want to talk about too is that you know the moon is 213 00:14:13.230 --> 00:14:16.920 just the first step there's a lot left to be learned and of course the ultimate 214 00:14:16.920 --> 00:14:20.639 goal is right up here in the corner of the screen we're focusing on the moon 215 00:14:20.639 --> 00:14:24.029 now but all of this is to one day you know get humans to Mars and get more 216 00:14:24.029 --> 00:14:27.629 spacecraft to Mars and so it's an exciting time to be at NASA and it's 217 00:14:27.629 --> 00:14:31.259 certainly exciting time to reflect back on the moon we really kind of 218 00:14:31.259 --> 00:14:34.949 demonstrated 2019 has been the year of the moon with the 50th anniversary of 219 00:14:34.949 --> 00:14:38.220 the Apollo mission but you know I think it's time to look forward to the future 220 00:14:38.220 --> 00:14:42.230 and and the future is kind of right here