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These are the user uploaded subtitles that are being translated: 1 00:00:03,120 --> 00:00:04,279 - Mars. 2 00:00:04,280 --> 00:00:05,679 The god of war 3 00:00:05,680 --> 00:00:08,919 and the source of man's science fictional demise. 4 00:00:08,920 --> 00:00:12,720 It has fired our imagination for thousands of years. 5 00:00:12,721 --> 00:00:15,679 We know the dry, barren planet was once flowing 6 00:00:15,680 --> 00:00:17,999 with vast reservoirs of water, 7 00:00:18,000 --> 00:00:20,279 the sky thick and filled with clouds, 8 00:00:20,280 --> 00:00:23,360 and the tantalizing possibility of life. 9 00:00:23,361 --> 00:00:25,800 It is the only other place in our solar system 10 00:00:25,801 --> 00:00:28,481 that man might one day call home. 11 00:01:06,082 --> 00:01:09,201 We Earthlings have fired numerous probes and satellites 12 00:01:09,202 --> 00:01:12,361 towards the red planet, an invasion of sorts, 13 00:01:12,362 --> 00:01:15,001 not for conquest but for knowledge. 14 00:01:15,002 --> 00:01:17,001 What happened to Mars? 15 00:01:17,002 --> 00:01:20,521 Is there or has there ever been life on the planet? 16 00:01:20,522 --> 00:01:24,322 - A fundamental question that needs to be answered, 17 00:01:24,323 --> 00:01:27,201 is life as we know it on Earth, 18 00:01:27,202 --> 00:01:31,361 even the simplest type of microbial life, unique? 19 00:01:31,362 --> 00:01:35,362 If we were to go to Mars and we were to find evidence 20 00:01:35,363 --> 00:01:38,403 of early microbial life or maybe even present life 21 00:01:38,404 --> 00:01:40,522 that somehow survived in the near surface, 22 00:01:40,523 --> 00:01:43,682 would it be the same as the early life 23 00:01:43,683 --> 00:01:45,002 that developed on Earth? 24 00:01:45,003 --> 00:01:47,243 That's a very fundamental question. 25 00:01:47,244 --> 00:01:50,522 Does life emerge generally in planets 26 00:01:50,523 --> 00:01:53,043 where the conditions for life are favorable 27 00:01:53,044 --> 00:01:55,763 if we find out that they were favorable on Mars 28 00:01:55,764 --> 00:01:58,723 or might life take its own unique path 29 00:01:58,724 --> 00:02:01,363 in different environments and turn out differently? 30 00:02:03,844 --> 00:02:06,882 - We have bombarded Mars with satellites and landers, 31 00:02:06,883 --> 00:02:09,923 but there have been more failures than successes. 32 00:02:09,924 --> 00:02:12,724 The Soviets established two Mars orbiters 33 00:02:12,725 --> 00:02:15,163 while NASA landed two Viking landers 34 00:02:15,164 --> 00:02:17,563 carrying complex analytical laboratories 35 00:02:17,564 --> 00:02:20,404 and search for signs of microbial life. 36 00:02:20,405 --> 00:02:22,924 Their findings were inconclusive. 37 00:02:27,804 --> 00:02:31,083 Further missions to Mars still had a high mortality rate, 38 00:02:31,084 --> 00:02:33,203 but the successes were outstanding, 39 00:02:33,204 --> 00:02:35,764 with robotic probes operating for years 40 00:02:35,765 --> 00:02:37,645 beyond their initial missions. 41 00:02:40,804 --> 00:02:43,644 In fact, Mars is a planet occupied solely 42 00:02:43,645 --> 00:02:45,245 by robots on the surface 43 00:02:45,246 --> 00:02:48,005 and satellites peering down from above. 44 00:02:51,966 --> 00:02:54,364 All these instruments perform admirably 45 00:02:54,365 --> 00:02:56,524 in their specified fields of endeavor, 46 00:02:56,525 --> 00:02:58,884 giving us a much clearer picture of the planet 47 00:02:58,885 --> 00:03:00,445 and its history. 48 00:03:00,446 --> 00:03:02,965 The science was following the water, 49 00:03:02,966 --> 00:03:05,966 what happened and where it is now. 50 00:03:08,005 --> 00:03:10,605 - Thanks to the specific instrumentation 51 00:03:10,606 --> 00:03:13,965 on board the mission, we are able to tell us 52 00:03:13,966 --> 00:03:16,204 what kind of ice did we find. 53 00:03:16,205 --> 00:03:18,204 And the result is that there is a mix 54 00:03:18,205 --> 00:03:21,446 of CO2 ice, or carbon dioxide ice, 55 00:03:21,447 --> 00:03:22,805 and water ice. 56 00:03:22,806 --> 00:03:24,966 And it's very important to characterize it, 57 00:03:24,967 --> 00:03:28,046 especially for the water ice, or frozen water, 58 00:03:28,047 --> 00:03:30,485 because one of the main objective 59 00:03:30,486 --> 00:03:33,646 of any mission to Mars is to trace the water 60 00:03:33,647 --> 00:03:35,766 on Mars in every form. 61 00:03:35,767 --> 00:03:39,125 Liquid, if possible, solid, water vapor. 62 00:03:39,126 --> 00:03:41,406 So it's very important to study the ice 63 00:03:41,407 --> 00:03:45,646 because it's one of reservoirs of water on the planet. 64 00:03:45,647 --> 00:03:47,326 - The science was conclusive. 65 00:03:47,327 --> 00:03:49,246 There was water on Mars. 66 00:03:49,247 --> 00:03:52,525 There were ancient lakes and rivers, even an ocean. 67 00:03:52,526 --> 00:03:54,486 We needed to learn more. 68 00:03:55,886 --> 00:03:58,327 With the advancement of analytical technology, 69 00:03:58,328 --> 00:04:00,086 computer power, and robotics, 70 00:04:00,087 --> 00:04:02,407 a new rover was constructed. 71 00:04:02,408 --> 00:04:05,566 Big, complex, and heavy, it required a new way 72 00:04:05,567 --> 00:04:07,608 to land on Mars safely. 73 00:04:08,687 --> 00:04:10,366 Engineers came up with a system 74 00:04:10,367 --> 00:04:12,968 that couldn't be fully tested here on Earth. 75 00:04:15,968 --> 00:04:18,447 It required a lot of things to happen correctly, 76 00:04:18,448 --> 00:04:20,886 on time, and in order. 77 00:04:20,887 --> 00:04:22,566 This was the sky crane 78 00:04:22,567 --> 00:04:24,286 and the rover, Curiosity, 79 00:04:24,287 --> 00:04:26,087 was the first to try it out. 80 00:04:26,968 --> 00:04:29,286 A controlled reentry with heat shield, 81 00:04:29,287 --> 00:04:32,567 aerobraking with a parachute, all pretty standard. 82 00:04:32,568 --> 00:04:36,087 Then a rocket-powered sky crane drops from the aeroshell 83 00:04:36,088 --> 00:04:38,487 and gently descends toward the surface, 84 00:04:38,488 --> 00:04:41,687 spooling out the rover below on cables. 85 00:04:41,688 --> 00:04:44,207 The rover touches down, cuts the cables, 86 00:04:44,208 --> 00:04:48,088 and release the sky crane to fly off and crash harmlessly. 87 00:04:48,808 --> 00:04:52,007 The Curiosity rover has been an astounding success, 88 00:04:52,008 --> 00:04:54,527 traversing the terrain for over 10 years, 89 00:04:54,528 --> 00:04:58,007 taking samples, drilling, and studying rock formations, 90 00:04:58,008 --> 00:05:00,567 zapping samples with a powerful laser, 91 00:05:00,568 --> 00:05:02,849 and photographing its progress. 92 00:05:03,849 --> 00:05:05,728 - Now, in the belly of that rover 93 00:05:05,729 --> 00:05:07,248 is an instrument called SAM. 94 00:05:07,249 --> 00:05:08,729 It's an instrument suite that has 95 00:05:08,730 --> 00:05:10,528 a couple different instruments in it that allow us 96 00:05:10,529 --> 00:05:12,769 to look at different types of gases. 97 00:05:12,770 --> 00:05:16,008 It helps us understand the chemical composition 98 00:05:16,009 --> 00:05:20,409 of the atmosphere and of minerals that might be found 99 00:05:20,410 --> 00:05:23,409 in the rocks and the soils on the surface. 100 00:05:23,410 --> 00:05:26,888 In particular, it helps us identify organic molecules 101 00:05:26,889 --> 00:05:27,928 that might be present. 102 00:05:27,929 --> 00:05:30,649 - So, the sort of evidence we're looking for, 103 00:05:30,650 --> 00:05:32,288 sort of signatures of past life 104 00:05:32,289 --> 00:05:33,209 that we would be looking for 105 00:05:33,210 --> 00:05:35,288 would be signature of microbial life. 106 00:05:35,289 --> 00:05:38,888 So, not realistically looking for dinosaur bones 107 00:05:38,889 --> 00:05:39,770 and that kind of thing. 108 00:05:39,771 --> 00:05:41,288 If life ever existed on Mars, 109 00:05:41,289 --> 00:05:45,010 we expect it to have been microbial, microorganisms. 110 00:06:10,570 --> 00:06:13,689 - Orbiters including Mars Odyssey and Mars Express 111 00:06:13,690 --> 00:06:16,570 have been hunting down life as well, from orbit. 112 00:06:19,531 --> 00:06:21,530 - After 10 years of mission, 113 00:06:21,531 --> 00:06:23,930 we have achieve a global view of Mars 114 00:06:23,931 --> 00:06:26,611 and then we know what every location on the surface, 115 00:06:26,612 --> 00:06:28,971 if you find some special minerals or not. 116 00:06:28,972 --> 00:06:30,771 So we have really the global view 117 00:06:30,772 --> 00:06:33,890 that tell us the history of Mars. 118 00:06:33,891 --> 00:06:36,411 Mars Express has, for the first time, 119 00:06:36,412 --> 00:06:38,411 detected methane. 120 00:06:38,412 --> 00:06:40,570 And also it comes from pressure in the atmosphere, 121 00:06:40,571 --> 00:06:42,731 vary from the place to another, 122 00:06:42,732 --> 00:06:44,651 from a season to another. 123 00:06:44,652 --> 00:06:47,570 And this discovery, it's been very debated 124 00:06:47,571 --> 00:06:49,331 in the scientific community 125 00:06:49,332 --> 00:06:52,690 because, in fact, methane should not be there 126 00:06:52,691 --> 00:06:55,691 because it's being destroyed in the atmosphere 127 00:06:55,692 --> 00:06:57,612 by the ultraviolet radiation. 128 00:06:57,613 --> 00:07:00,491 So if methane is there, there must be a source 129 00:07:00,492 --> 00:07:02,891 of methane and for the time being, 130 00:07:02,892 --> 00:07:05,853 the origin of this source is largely unknown. 131 00:07:06,653 --> 00:07:09,972 - However, with Curiosity prowling around Gale Crater, 132 00:07:09,973 --> 00:07:12,973 it too detected seasonal methane. 133 00:07:13,812 --> 00:07:16,131 - Now, methane has been found previously 134 00:07:16,132 --> 00:07:19,252 in the Martian atmosphere by both Earth-based telescopes 135 00:07:19,253 --> 00:07:21,171 and space-born orbiters, 136 00:07:21,172 --> 00:07:23,332 but this is the first time that we've actually seen 137 00:07:23,333 --> 00:07:26,371 a sharp increase and decrease in the abundance of methane 138 00:07:26,372 --> 00:07:28,131 in the atmosphere in Gale Crater. 139 00:07:28,132 --> 00:07:30,612 But what this really means is that present day Mars 140 00:07:30,613 --> 00:07:32,133 is an active environment. 141 00:07:33,454 --> 00:07:37,413 - The big question is what is the origin of this methane 142 00:07:37,414 --> 00:07:38,932 now being released? 143 00:07:38,933 --> 00:07:41,973 The two principles areas are first, 144 00:07:41,974 --> 00:07:43,253 by analogy with the Earth, 145 00:07:43,254 --> 00:07:45,973 it could be released unproduced initially, 146 00:07:45,974 --> 00:07:47,892 primarily by biology. 147 00:07:47,893 --> 00:07:50,012 This would be microbial activity 148 00:07:50,013 --> 00:07:53,333 acting on certain chemicals below the surface 149 00:07:53,334 --> 00:07:56,013 and then producing methane as a byproduct. 150 00:07:56,813 --> 00:07:58,973 But of course we can't stay with certitude 151 00:07:58,974 --> 00:08:02,613 that it is biologically produced. 152 00:08:02,614 --> 00:08:06,733 And so we also consider geochemical mechanisms 153 00:08:06,734 --> 00:08:10,093 in which carbon dioxide is actually combining 154 00:08:10,094 --> 00:08:12,693 with water and producing methane 155 00:08:12,694 --> 00:08:14,774 under very high temperatures and pressures. 156 00:08:14,775 --> 00:08:16,693 And that methane can then be released 157 00:08:16,694 --> 00:08:18,294 in the atmosphere separately. 158 00:08:19,534 --> 00:08:21,933 - Now, at this point we don't have enough evidence 159 00:08:21,934 --> 00:08:24,654 to tell us whether or not the organics refining 160 00:08:24,655 --> 00:08:27,813 are biological or nonbiological in origin. 161 00:08:27,814 --> 00:08:31,133 There are several viable nonbiological explanations, 162 00:08:31,134 --> 00:08:33,454 including this organic material could've come down 163 00:08:33,455 --> 00:08:35,974 from space, from meteorites or comets, 164 00:08:35,975 --> 00:08:39,654 or organics can be formed by geological reactions 165 00:08:39,655 --> 00:08:41,334 in the rock itself. 166 00:08:41,335 --> 00:08:43,374 Now what's exciting about this discovery 167 00:08:43,375 --> 00:08:45,455 is it gives us new hope in the search 168 00:08:45,456 --> 00:08:46,975 for chemical evidence of life. 169 00:08:46,976 --> 00:08:48,574 We found the organic material. 170 00:08:48,575 --> 00:08:50,775 Now the next step is trying to figure out 171 00:08:50,776 --> 00:08:51,855 what its origin is. 172 00:08:51,856 --> 00:08:53,574 Main engine start. 173 00:08:53,575 --> 00:08:56,174 Ignition and lift off 174 00:08:56,175 --> 00:08:58,574 of the Atlas V with MAVEN, 175 00:08:58,575 --> 00:09:01,494 looking for clues about the evolution of Mars 176 00:09:01,495 --> 00:09:03,095 through its atmosphere. 177 00:09:04,736 --> 00:09:07,455 - The latest NASA orbiter mission is MAVEN. 178 00:09:07,456 --> 00:09:11,895 Launched in November 2013, it made orbit 10 months later. 179 00:09:17,616 --> 00:09:19,736 - MAVEN is the Mars Atmosphere 180 00:09:19,737 --> 00:09:21,856 and Volatile Evolution Mission. 181 00:09:21,857 --> 00:09:25,575 Our goal is to study the role that lost to space 182 00:09:25,576 --> 00:09:27,616 has played in the history of the atmosphere. 183 00:09:27,617 --> 00:09:29,135 Where did the water go? 184 00:09:29,136 --> 00:09:32,535 Where did the CO2 go from the early planet? 185 00:09:32,536 --> 00:09:35,535 These are important questions to understand 186 00:09:35,536 --> 00:09:39,575 how Mars went from an early warm, wet environment 187 00:09:39,576 --> 00:09:42,216 to the cold, dry environment we see today. 188 00:09:44,457 --> 00:09:47,776 - There's evidence of water flowing on Mars 189 00:09:47,777 --> 00:09:51,095 at one point in time, perhaps even oceans on Mars. 190 00:09:51,096 --> 00:09:55,136 And what happened that it's so barren at this point in time? 191 00:09:55,137 --> 00:09:58,696 And a key part of that is the atmosphere 192 00:09:58,697 --> 00:10:01,257 and it's a much thinner atmosphere than what scientists 193 00:10:01,258 --> 00:10:03,096 believe it was at one point in time, 194 00:10:03,097 --> 00:10:06,096 so the stripping away of that upper atmosphere, 195 00:10:06,097 --> 00:10:07,816 that's what MAVEN is going after, 196 00:10:07,817 --> 00:10:09,697 the climate change at Mars. 197 00:10:13,418 --> 00:10:16,057 - One of these processes is called sputtering, 198 00:10:16,058 --> 00:10:18,536 where atoms are knocked away from the atmosphere 199 00:10:18,537 --> 00:10:21,457 due to impacts from energetic particles. 200 00:10:21,458 --> 00:10:24,657 The sun constantly emits high energy photons. 201 00:10:24,658 --> 00:10:26,457 When these enter a planet's atmosphere 202 00:10:26,458 --> 00:10:28,096 it can crash into a molecule, 203 00:10:28,097 --> 00:10:31,778 knocking loose an electron and turning it into an ion. 204 00:10:31,779 --> 00:10:34,618 When this happens in the presence of a magnetic field, 205 00:10:34,619 --> 00:10:37,937 the ions are captured and spin around the field. 206 00:10:37,938 --> 00:10:41,738 Conveniently, the sun generates a giant magnetic field 207 00:10:41,739 --> 00:10:44,377 that is carried by the solar wind. 208 00:10:44,378 --> 00:10:47,297 As the magnetic field sweeps past the planet, 209 00:10:47,298 --> 00:10:49,659 these ions are carried away. 210 00:10:50,578 --> 00:10:52,017 Depending on where they form, 211 00:10:52,018 --> 00:10:54,177 other ions will not be carried away 212 00:10:54,178 --> 00:10:56,577 but will hit the top of the atmosphere. 213 00:10:56,578 --> 00:10:58,817 These ions crash into other molecules 214 00:10:58,818 --> 00:11:00,618 and fling atoms everywhere. 215 00:11:00,619 --> 00:11:03,937 Some of these atoms can be knocked or sputtered into space 216 00:11:03,938 --> 00:11:06,059 causing atmospheric loss. 217 00:11:10,899 --> 00:11:13,979 As this process continues over billions of years, 218 00:11:13,980 --> 00:11:15,898 Mars' atmosphere has disappeared 219 00:11:15,899 --> 00:11:18,578 and along with it, the water. 220 00:11:18,579 --> 00:11:21,899 How much water has Mars lost this way? 221 00:11:24,819 --> 00:11:27,979 - We use the world's three majors telescopes 222 00:11:27,980 --> 00:11:29,979 for infrared astronomy. 223 00:11:29,980 --> 00:11:31,938 From the ground we could actually take a snapshot 224 00:11:31,939 --> 00:11:34,819 of the whole hemisphere of the planet on a single night. 225 00:11:35,579 --> 00:11:37,779 - Water naturally carries a heavy isotope 226 00:11:37,780 --> 00:11:40,498 of hydrogen deuterium, which remains trapped 227 00:11:40,499 --> 00:11:44,620 in the water cycle while normal hydrogen is lost to space. 228 00:11:44,621 --> 00:11:46,860 Detecting the amount of deuterium enrichment 229 00:11:46,861 --> 00:11:49,700 tells us how much water has been lost. 230 00:11:50,940 --> 00:11:54,340 - Now we know that Mars' water is much more enriched 231 00:11:54,341 --> 00:11:55,819 than terrestrial ocean water 232 00:11:55,820 --> 00:11:58,899 in the heavy form of water, the deuterated form. 233 00:11:58,900 --> 00:12:02,299 Immediately that permits us to estimate the amount of water 234 00:12:02,300 --> 00:12:04,540 Mars has lost since it was young. 235 00:12:13,540 --> 00:12:16,060 - So in the ancient past, when you have some indications 236 00:12:16,061 --> 00:12:18,261 that water was flowing on the surface, 237 00:12:18,262 --> 00:12:20,140 but how much water was there? 238 00:12:20,141 --> 00:12:22,900 Talking about oceans, I'm talking about small rivers, 239 00:12:22,901 --> 00:12:23,940 little rain. 240 00:12:23,941 --> 00:12:26,940 So these definitions of how much water was on the planet, 241 00:12:26,941 --> 00:12:28,220 it was very undefined. 242 00:12:28,221 --> 00:12:32,061 - A major question has been how much water did Mars 243 00:12:32,062 --> 00:12:34,020 actually have when it was young 244 00:12:34,021 --> 00:12:35,781 and how did it lose that water? 245 00:12:35,782 --> 00:12:39,140 - The findings indicate that only 13% of an ancient ocean 246 00:12:39,141 --> 00:12:41,020 remains on the planet today, 247 00:12:41,021 --> 00:12:43,781 now stored in the polar ice caps. 248 00:12:43,782 --> 00:12:47,820 87% of this ocean has been lost to space. 249 00:12:47,821 --> 00:12:50,781 This means that early Mars would have looked much different 250 00:12:50,782 --> 00:12:53,461 than it does today, with a significant portion 251 00:12:53,462 --> 00:12:55,782 of its surface covered by water. 252 00:12:55,783 --> 00:12:57,782 - So the really interesting question is 253 00:12:57,783 --> 00:13:00,462 could it form a sea or an ocean? 254 00:13:00,463 --> 00:13:01,862 And indeed, it would. 255 00:13:01,863 --> 00:13:04,701 In the northern plains, which is a relatively flat region, 256 00:13:04,702 --> 00:13:06,501 but depressed from the rest of the planet, 257 00:13:06,502 --> 00:13:09,742 it would form an ocean that was approximately 258 00:13:09,743 --> 00:13:13,262 20% of the planet's surface area. 259 00:13:13,263 --> 00:13:15,862 And so that is a respectable ocean. 260 00:13:15,863 --> 00:13:19,342 - This ocean had a maximum depth of around 5,000 feet 261 00:13:19,343 --> 00:13:21,062 or around one mile deep. 262 00:13:21,063 --> 00:13:24,141 It's deep, not as deep as the deepest points of our oceans, 263 00:13:24,142 --> 00:13:27,382 but comparable to average depth of the Mediterranean Sea. 264 00:13:28,423 --> 00:13:31,382 - By combining Martian topography with a new estimate 265 00:13:31,383 --> 00:13:34,302 for water loss, the researchers were able to simulate 266 00:13:34,303 --> 00:13:38,623 Mars's ancient ocean and its escape to space. 267 00:13:38,624 --> 00:13:41,743 As Mars lost its atmosphere over billions of years, 268 00:13:41,744 --> 00:13:45,102 it lost the pressure and heat needed to keep water liquid, 269 00:13:45,103 --> 00:13:48,382 causing the ocean to shrink and recede northward. 270 00:13:48,383 --> 00:13:50,743 The remaining water eventually condensed 271 00:13:50,744 --> 00:13:53,222 and froze over the north and south poles, 272 00:13:53,223 --> 00:13:56,222 giving Mars the ice caps that we see today. 273 00:13:56,223 --> 00:14:00,263 - We now know that Mars was wet 274 00:14:00,264 --> 00:14:03,463 for a much longer time than we thought before. 275 00:14:03,464 --> 00:14:06,664 Curiosity shows it was wet for 1.5 billion years, 276 00:14:06,665 --> 00:14:09,664 already much longer than the period of time needed 277 00:14:09,665 --> 00:14:11,464 for life to develop on Earth. 278 00:14:11,465 --> 00:14:14,023 And now we see that Mars must've been wet 279 00:14:14,024 --> 00:14:15,624 for a period even longer. 280 00:14:15,625 --> 00:14:17,503 - It's fascinating that we can learn so much 281 00:14:17,504 --> 00:14:21,064 about 4.5 billion years ago with measurement taken right now 282 00:14:21,065 --> 00:14:23,303 and ultimately we can conclude this idea 283 00:14:23,304 --> 00:14:25,823 of a ocean covering 20% of the planet, 284 00:14:25,824 --> 00:14:27,984 which opens the idea of habitability 285 00:14:27,985 --> 00:14:29,985 and the evolution of life on the planet. 286 00:14:32,745 --> 00:14:34,183 - Building on this knowledge, 287 00:14:34,184 --> 00:14:37,464 scientists are developing the next series of robotic probes 288 00:14:37,465 --> 00:14:40,143 to be sent to Mars in the coming years. 289 00:14:40,144 --> 00:14:43,265 This time, NASA is building on its successes, 290 00:14:43,266 --> 00:14:47,465 utilizing hardware and systems that they know will work. 291 00:14:47,466 --> 00:14:49,824 - We've been to Mars before 292 00:14:49,825 --> 00:14:52,024 with the JPL, Lockheed Martin team. 293 00:14:52,025 --> 00:14:54,584 We've been to the surface of Mars before successfully 294 00:14:54,585 --> 00:14:55,745 with Phoenix. 295 00:14:55,746 --> 00:14:57,985 We know how to operate the arm. 296 00:14:57,986 --> 00:15:01,345 The surface operations are much, much simpler than Phoenix 297 00:15:01,346 --> 00:15:03,425 and we're putting two instruments on the surface 298 00:15:03,426 --> 00:15:04,785 and then we're leaving them there 299 00:15:04,786 --> 00:15:07,745 with no ground-in-the-loop interaction. 300 00:15:07,746 --> 00:15:11,384 Repetitive weekly up link, down link sessions. 301 00:15:11,385 --> 00:15:13,305 We're just made to do this mission. 302 00:15:14,626 --> 00:15:17,626 - The InSight mission is a geophysical mission to Mars. 303 00:15:17,627 --> 00:15:20,305 It's gonna go to Mars and take its vital signs. 304 00:15:20,306 --> 00:15:22,105 It's gonna take its heartbeat, 305 00:15:22,106 --> 00:15:24,705 the seismic activity of the planet. 306 00:15:24,706 --> 00:15:27,385 - So we're gonna be doing that using a seismometer, 307 00:15:27,386 --> 00:15:29,505 a very high precision seismometer. 308 00:15:29,506 --> 00:15:32,066 Using techniques that have been well-developed on Earth 309 00:15:32,067 --> 00:15:35,746 to get the understanding of the crust, mantle, and core, 310 00:15:35,747 --> 00:15:38,025 and sort of the relationship between those. 311 00:15:38,026 --> 00:15:39,705 - Gonna take its temperature by measuring 312 00:15:39,706 --> 00:15:41,105 the thermal gradient of the surface, 313 00:15:41,106 --> 00:15:42,585 which tells how much heat is coming out. 314 00:15:42,586 --> 00:15:46,305 And we also have a heat flow probe called HP Cubed 315 00:15:46,306 --> 00:15:48,185 and what that does is it's gonna basically take 316 00:15:48,186 --> 00:15:50,786 the temperature of Mars and from that it'll be able 317 00:15:50,787 --> 00:15:52,747 to understand what the thermal flex is 318 00:15:52,748 --> 00:15:54,826 over the course of a full Martian year. 319 00:15:54,827 --> 00:15:57,586 - And it's gonna sort of measure its reflexes 320 00:15:57,587 --> 00:16:00,146 by looking at how the rotation wobbles 321 00:16:00,147 --> 00:16:03,627 with the tiled effects of the sun. 322 00:16:03,628 --> 00:16:06,306 - Our final experiment is called RISE 323 00:16:06,307 --> 00:16:08,627 and that's going to be looking at the, 324 00:16:08,628 --> 00:16:11,427 basically the wobble of Mars to help understand 325 00:16:11,428 --> 00:16:14,668 what the core size may be in composition. 326 00:16:16,907 --> 00:16:19,427 - The European Space Agency is also well along 327 00:16:19,428 --> 00:16:23,106 with ExoMars, a rover with advanced drilling capability 328 00:16:23,107 --> 00:16:25,506 due to be launched by 2018. 329 00:16:25,507 --> 00:16:28,186 Its principle goal, to drill down deep 330 00:16:28,187 --> 00:16:30,588 in search of microorganisms. 331 00:16:37,388 --> 00:16:41,307 - What is new with ExoMars, with the rover in particular, 332 00:16:41,308 --> 00:16:43,027 is what we call the mobility. 333 00:16:43,028 --> 00:16:46,147 Mobility, not only horizontal, but also vertical. 334 00:16:46,148 --> 00:16:48,307 This is a particular thing that we have 335 00:16:48,308 --> 00:16:52,587 on board ExoMars mission, so we will be able to sample 336 00:16:52,588 --> 00:16:54,947 material from below the surface 337 00:16:54,948 --> 00:16:56,868 that is quite important to understand 338 00:16:56,869 --> 00:17:01,147 if there is any sign of a past life activity on Mars. 339 00:17:01,148 --> 00:17:03,348 - We will be looking, for the first time, 340 00:17:03,349 --> 00:17:04,828 in the third dimension, 341 00:17:04,829 --> 00:17:07,269 the third dimension being depth. 342 00:17:07,270 --> 00:17:10,669 And we think that is where we have the highest chance 343 00:17:10,670 --> 00:17:13,148 of making an interesting discovery 344 00:17:13,149 --> 00:17:17,870 regarding the presence of organic molecules in Mars. 345 00:17:26,350 --> 00:17:28,469 - It's a whole planet out there 346 00:17:28,470 --> 00:17:30,508 with a complicated history. 347 00:17:30,509 --> 00:17:34,629 It's that history is a story that's stored in the rocks 348 00:17:34,630 --> 00:17:37,028 and our job is to figure out that story 349 00:17:37,029 --> 00:17:38,989 and what that story of that planet 350 00:17:38,990 --> 00:17:41,509 tells us about this planet that we live on. 351 00:17:41,510 --> 00:17:44,709 - So where Curiosity takes rocks and grinds them up 352 00:17:44,710 --> 00:17:46,949 into powder and looks at their bulk constituents, 353 00:17:46,950 --> 00:17:50,309 what this mission would need to do is be able to look 354 00:17:50,310 --> 00:17:53,430 in a microscopic level and examine the rocks 355 00:17:53,431 --> 00:17:55,670 for these very tiny and detailed messages 356 00:17:55,671 --> 00:17:57,109 that they would be sending to us 357 00:17:57,110 --> 00:17:59,350 about the past life that could've lived there. 358 00:17:59,351 --> 00:18:01,509 - This that I'm holding up here 359 00:18:01,510 --> 00:18:03,790 is a classic biosignature from the Earth, 360 00:18:03,791 --> 00:18:04,870 it's a fossil. 361 00:18:04,871 --> 00:18:07,109 We're not actually expecting to see a fossil 362 00:18:07,110 --> 00:18:09,589 of shells or other components, 363 00:18:09,590 --> 00:18:12,870 but what we want to be able to see are, 364 00:18:12,871 --> 00:18:14,309 with this instrumentation, 365 00:18:14,310 --> 00:18:17,510 are the fine-scale layering that one might see in a rock, 366 00:18:17,511 --> 00:18:20,471 in which we can see dark and light-toned layers. 367 00:18:20,472 --> 00:18:23,272 And those dark and light tone layers are telling a story. 368 00:18:30,311 --> 00:18:33,550 - When will NASA send astronauts to Mars? 369 00:18:33,551 --> 00:18:35,471 - Five, four, three, 370 00:18:35,472 --> 00:18:37,191 two, one. 371 00:18:38,792 --> 00:18:41,550 And lift off at dawn. 372 00:18:41,551 --> 00:18:43,071 The dawn of Orion 373 00:18:43,072 --> 00:18:46,311 and a new era of American space exploration. 374 00:18:47,831 --> 00:18:49,030 - The first test flight 375 00:18:49,031 --> 00:18:51,351 of the Orion crew capsule is complete, 376 00:18:51,352 --> 00:18:54,831 the hardware and systems are ready for mass production. 377 00:18:54,832 --> 00:18:57,432 The components, the engineering, the manufacturing, 378 00:18:57,433 --> 00:18:59,792 are all underway with NASA looking back 379 00:18:59,793 --> 00:19:01,272 to what worked in the past 380 00:19:01,273 --> 00:19:03,353 and utilizing it for the future. 381 00:19:10,633 --> 00:19:11,911 - Fire. 382 00:19:11,912 --> 00:19:14,031 - The solid rocket booster technology 383 00:19:14,032 --> 00:19:15,432 straight from the space shuttle 384 00:19:15,433 --> 00:19:17,552 has been extended and tested. 385 00:19:19,952 --> 00:19:22,872 NASA's new Space Launch System, or SLS, 386 00:19:22,873 --> 00:19:24,591 is coming closer to fruition, 387 00:19:24,592 --> 00:19:26,992 reusing the space shuttle's main engines 388 00:19:26,993 --> 00:19:28,832 as the new system's work horses, 389 00:19:28,833 --> 00:19:30,673 saving billions of dollars 390 00:19:30,674 --> 00:19:33,113 and years in research and development. 391 00:20:00,393 --> 00:20:02,473 The Europeans are teaming up with NASA 392 00:20:02,474 --> 00:20:04,754 to provide the service model for Orion, 393 00:20:04,755 --> 00:20:08,314 allowing for long duration, deep space flights. 394 00:20:15,314 --> 00:20:18,233 Autonomous Martian landing systems are well advanced 395 00:20:18,234 --> 00:20:19,393 and being tested. 396 00:20:19,394 --> 00:20:21,833 Software and hardware are fully integrated 397 00:20:21,834 --> 00:20:25,193 for both manned and unmanned Martian landings 398 00:20:25,194 --> 00:20:27,355 and when they get there. 399 00:20:28,154 --> 00:20:29,393 - Desert RAT stands for 400 00:20:29,394 --> 00:20:31,713 Desert Research and Technology studies. 401 00:20:31,714 --> 00:20:34,634 This is a group of engineers and scientists. 402 00:20:34,635 --> 00:20:37,233 - We're looking to test out new concepts, 403 00:20:37,234 --> 00:20:40,514 procedures, equipment, like rover concepts, 404 00:20:40,515 --> 00:20:42,114 to see how they work in the field environment. 405 00:20:42,115 --> 00:20:44,394 - So the team tests these technologies 406 00:20:44,395 --> 00:20:47,075 to make sure that in future human space flight missions 407 00:20:47,076 --> 00:20:49,514 we'll be able to do science as best as we can. 408 00:20:49,515 --> 00:20:51,475 That's something that NASA's never done, 409 00:20:51,476 --> 00:20:54,075 two human rovers at the same time. 410 00:20:54,076 --> 00:20:55,795 So we're really trying to develop 411 00:20:55,796 --> 00:20:58,275 how do you use these assets at the same time? 412 00:20:58,276 --> 00:21:00,554 And interesting things that you might not think about 413 00:21:00,555 --> 00:21:02,394 are your communications. 414 00:21:02,395 --> 00:21:04,914 So you potentially have four astronauts talking 415 00:21:04,915 --> 00:21:06,834 all at the same time to Mission Control 416 00:21:06,835 --> 00:21:08,675 or science communication backroom. 417 00:21:08,676 --> 00:21:10,594 - It's just like planning a real mission, say 418 00:21:10,595 --> 00:21:13,114 like you kind of think about Apollo missions. 419 00:21:13,115 --> 00:21:14,475 You had the astronauts on the moon 420 00:21:14,476 --> 00:21:16,515 and you had people, Mission Control, 421 00:21:16,516 --> 00:21:18,515 but there was a science backroom you didn't hear about 422 00:21:18,516 --> 00:21:22,476 but the astronauts were getting information from them. 423 00:21:22,477 --> 00:21:25,315 - Arizona has a very good climate 424 00:21:25,316 --> 00:21:27,356 for these types of analog studies. 425 00:21:27,357 --> 00:21:29,915 You have pretty much open plains and you have a lot 426 00:21:29,916 --> 00:21:31,796 of geological features that are analogous 427 00:21:31,797 --> 00:21:34,357 to places on the moon and on Mars. 428 00:21:42,437 --> 00:21:45,715 - Long-term space voyages are being replicated on the ground 429 00:21:45,716 --> 00:21:48,436 and in orbit with the ISS. 430 00:21:48,437 --> 00:21:50,756 Surface habitats, power systems, 431 00:21:50,757 --> 00:21:53,036 food and oxygen supply manufacturing, 432 00:21:53,037 --> 00:21:55,397 are also on the drawing board. 433 00:21:59,078 --> 00:22:00,997 - The human flight component would like to see 434 00:22:00,998 --> 00:22:04,116 an experiment where resources on the surfaces of Mars 435 00:22:04,117 --> 00:22:06,357 from the rocks or the atmosphere could be used 436 00:22:06,358 --> 00:22:08,916 to generate fuel or other parts 437 00:22:08,917 --> 00:22:12,677 that would enable future exploration 438 00:22:12,678 --> 00:22:15,677 in cutting the tie, so to speak, to Earth. 439 00:22:15,678 --> 00:22:17,236 So you wouldn't necessarily have to bring 440 00:22:17,237 --> 00:22:17,998 everything with you. 441 00:22:17,999 --> 00:22:19,997 You can actually manufacture it on the planet 442 00:22:19,998 --> 00:22:22,477 and that's a really exciting additional component 443 00:22:22,478 --> 00:22:25,316 that we've been exploring and analyzing 444 00:22:25,317 --> 00:22:26,917 in this work. 445 00:22:29,639 --> 00:22:32,837 - NASA isn't the only one with its eye on this prize. 446 00:22:32,838 --> 00:22:36,278 ESA and now the Indian Space Research Organization 447 00:22:36,279 --> 00:22:38,517 have a spacecraft orbiting Mars 448 00:22:38,518 --> 00:22:40,999 and they did it on their first attempt. 449 00:22:42,238 --> 00:22:44,957 Private enterprise is hard at work as well. 450 00:22:44,958 --> 00:22:48,278 Mars 500, Mars One, The Mars Society, 451 00:22:48,279 --> 00:22:51,638 Mars Foundation, and the Mars Initiative, to name a few. 452 00:22:51,639 --> 00:22:54,278 And they have volunteers lining up already 453 00:22:54,279 --> 00:22:56,398 for a one-way trip to Mars. 454 00:22:58,238 --> 00:23:01,037 It is inevitable that we will set foot on Mars 455 00:23:01,038 --> 00:23:02,517 in the very near future. 456 00:23:02,518 --> 00:23:05,440 We will stay and learn her secrets. 457 00:23:08,000 --> 00:23:09,279 Perhaps in the future 458 00:23:09,280 --> 00:23:11,759 we will be able to alter the atmospheric density 459 00:23:11,760 --> 00:23:14,118 through terraforming and return Mars 460 00:23:14,119 --> 00:23:15,958 to the world that it once was, 461 00:23:15,959 --> 00:23:20,679 awash with oceans and rivers, clouds and rain. 462 00:23:20,680 --> 00:23:23,839 Maybe some of us could call it home. 36765

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