1 00:00:00,000 --> 00:00:14,800 Hey, Bill Nye the Science Guy here. 2 00:00:14,800 --> 00:00:17,920 When you dream about going places, where does your mind take you? 3 00:00:17,920 --> 00:00:18,920 Somewhere on Earth? 4 00:00:18,920 --> 00:00:20,480 Or to the stars? 5 00:00:20,480 --> 00:00:24,520 If you spend time looking at the stars, you'll notice one that's a bit red. 6 00:00:24,520 --> 00:00:26,960 It's actually not a star at all, it's the planet Mars. 7 00:00:26,960 --> 00:00:29,480 It's the next place humans are going to explore. 8 00:00:29,480 --> 00:00:33,600 Of course, none of this exploration could be done without science and mathematics. 9 00:00:33,600 --> 00:00:38,320 On this episode of NASA Connect, NASA researchers will show you how the principles of geometry 10 00:00:38,320 --> 00:00:42,440 are used to survey and map our planet Earth and the planet Mars. 11 00:00:42,440 --> 00:00:47,320 So hang tight as Vance, Jennifer and the NASA Science Guys survey Earth and Mars on this 12 00:00:47,320 --> 00:00:49,400 episode of NASA Connect. 13 00:01:18,320 --> 00:01:24,840 Hey guys, welcome to NASA Connect, the show that connects you to the world of math, science, 14 00:01:24,840 --> 00:01:26,280 technology and NASA. 15 00:01:26,280 --> 00:01:27,360 I'm Jennifer Pulley. 16 00:01:27,360 --> 00:01:28,360 And I'm Van Hughes. 17 00:01:28,360 --> 00:01:32,120 Today, we're here at the Virginia Living Museum in Newport News, Virginia. 18 00:01:32,120 --> 00:01:36,160 And right now, we're standing on a sundial, which is basically a plate marked with hour 19 00:01:36,160 --> 00:01:37,680 lines and a gnomon. 20 00:01:37,680 --> 00:01:41,280 A gnomon is a raised projection that casts a shadow from the sun. 21 00:01:41,280 --> 00:01:44,360 Jennifer, why don't you come be the gnomon? 22 00:01:44,400 --> 00:01:47,960 According to your shadow, it's time to start the show. 23 00:01:47,960 --> 00:01:53,320 Well Van, this isn't a bad way to tell time, but you know, I think I'd rather use my watch. 24 00:01:53,320 --> 00:01:58,200 You know, throughout history, the sun and stars governed people's days, years and even 25 00:01:58,200 --> 00:01:59,560 their lives. 26 00:01:59,560 --> 00:02:04,320 Using sundials and observing shadows was one way ancient people told time. 27 00:02:04,320 --> 00:02:09,520 Get this, you can even measure height and distance with shadows cast from the sun. 28 00:02:09,520 --> 00:02:14,880 In fact, you can even measure the circumference of an entire planet, like Earth or Mars, with 29 00:02:14,880 --> 00:02:16,920 something as simple as a shadow. 30 00:02:16,920 --> 00:02:18,400 And geometry. 31 00:02:18,400 --> 00:02:23,760 On today's NASA Connect, we will examine how NASA researchers use the principles of geometry 32 00:02:23,760 --> 00:02:28,800 to survey the world around us and the worlds beyond us. 33 00:02:28,800 --> 00:02:34,800 We'll focus our telescope to see how geometry and satellites are used to measure, map and 34 00:02:34,800 --> 00:02:37,200 survey other planets like Mars. 35 00:02:37,480 --> 00:02:41,520 Which, by the way, can be seen quite well in this planetarium. 36 00:02:41,520 --> 00:02:47,360 Anyway, we'll visit some students from George Washington University who are studying and 37 00:02:47,360 --> 00:02:52,440 surveying the Martian landscape at NASA Langley Research Center in Hampton, Virginia. 38 00:02:52,440 --> 00:02:57,320 And we'll visit a researcher from NASA's Jet Propulsion Laboratory in Pasadena, California, 39 00:02:57,320 --> 00:03:02,160 who will show us how geometry is used by NASA's Mars Global Surveyor. 40 00:03:02,160 --> 00:03:06,520 Later on in the show, students from Central Middle School in Charlotte Courthouse, Virginia 41 00:03:06,520 --> 00:03:07,520 will join us. 42 00:03:07,520 --> 00:03:10,160 They've got an awesome experiment you'll want to try. 43 00:03:10,160 --> 00:03:15,040 Plus, NASA's Educational Technology Program Manager, Dr. Shelley Canright, will introduce 44 00:03:15,040 --> 00:03:19,240 us to some students from Davis Middle School in Hampton, Virginia. 45 00:03:19,240 --> 00:03:22,720 These students are using the internet to create their own Mars Surveyor. 46 00:03:22,720 --> 00:03:26,400 We'll learn more about this web-based activity later in the show. 47 00:03:26,400 --> 00:03:30,720 Hey, as we go through the show, our friend Norbert will visit you too. 48 00:03:30,720 --> 00:03:34,640 Every time he appears with a cue card, that's your cue to think about the answers to the 49 00:03:34,640 --> 00:03:36,160 questions he gives you. 50 00:03:37,080 --> 00:03:40,960 Plus, we'll go to NASA Ames Research Center in Moffett Field, California. 51 00:03:40,960 --> 00:03:46,240 There, we'll get all the latest information on the search for life on Mars and learn all 52 00:03:46,240 --> 00:03:49,200 about green slime. 53 00:03:49,200 --> 00:03:54,880 So hang tight, as NASA Connect takes you on a global surveyor mission to our planet Earth 54 00:03:54,880 --> 00:03:56,880 and to planet Mars. 55 00:03:56,880 --> 00:04:07,520 What is surveying? 56 00:04:07,520 --> 00:04:11,120 How do surveyors use geometry? 57 00:04:11,120 --> 00:04:15,200 Surveying is the measurement of angles and distances, elevation and direction. 58 00:04:15,200 --> 00:04:20,200 It's especially useful for locating property boundaries, construction layout and map making. 59 00:04:20,200 --> 00:04:24,960 Okay, Terry, can you tell me how surveyors use this equipment and geometry to survey 60 00:04:24,960 --> 00:04:25,960 land? 61 00:04:26,040 --> 00:04:27,560 First, let's look at this transit. 62 00:04:27,560 --> 00:04:33,040 It contains a telescope, a compass, and a protractor, and it's used to measure horizontal 63 00:04:33,040 --> 00:04:34,960 and vertical angles. 64 00:04:34,960 --> 00:04:38,720 You can measure angles in the field with this and measure those same angles back at your 65 00:04:38,720 --> 00:04:41,100 desk with a protractor. 66 00:04:41,100 --> 00:04:45,880 This instrument is used to lay out objects like football fields, baseball fields, soccer 67 00:04:45,880 --> 00:04:46,880 fields. 68 00:04:46,880 --> 00:04:51,000 Today, let's demonstrate how we use this by laying out this football field. 69 00:04:51,000 --> 00:04:52,000 Alright. 70 00:04:52,000 --> 00:04:55,640 First, we pick a starting point and set the transit over the point. 71 00:04:55,640 --> 00:04:58,360 We call this point corner number one. 72 00:04:58,360 --> 00:05:03,000 Then we measure 300 feet to the next corner and call it corner number four. 73 00:05:03,000 --> 00:05:05,480 We mark this corner with a corner marker. 74 00:05:05,480 --> 00:05:10,720 With zero on the scale, we look through the telescope and line up corner number four. 75 00:05:10,720 --> 00:05:15,400 We know that the angle between the sides of a rectangle is 90 degrees, so we turn the 76 00:05:15,400 --> 00:05:21,160 telescope towards corner number two until we can read 90 degrees on the transit circle 77 00:05:21,160 --> 00:05:22,160 or scale. 78 00:05:22,680 --> 00:05:28,040 Now we measure the width of the football field, 150 feet, and mark corner number two. 79 00:05:28,040 --> 00:05:32,240 Next, we move the transit over corner number two. 80 00:05:32,240 --> 00:05:37,400 With zero on the scale, we look through the telescope at corner number one marker. 81 00:05:37,400 --> 00:05:42,160 We turn the telescope towards corner number three until we can read 90 degrees on the 82 00:05:42,160 --> 00:05:43,160 scale. 83 00:05:43,160 --> 00:05:46,840 We measure 300 feet and mark corner number three. 84 00:05:46,840 --> 00:05:49,920 We now have all of the corners marked. 85 00:05:49,920 --> 00:05:54,840 Applying one of the basic rules of geometry, we know that the sum of the interior angles 86 00:05:54,840 --> 00:06:01,840 of a four-sided polygon is 360 degrees, so our last angle must measure 90 degrees for 87 00:06:01,840 --> 00:06:03,560 a correct layout. 88 00:06:03,560 --> 00:06:08,360 The rule for checking the angles of any object is that the sum of the interior angles of 89 00:06:08,360 --> 00:06:13,720 a closed polygon is equal to the number of sides minus two times 180 degrees. 90 00:06:13,720 --> 00:06:19,320 You know, Jennifer, the art and science of surveying had been used for over 3,400 years 91 00:06:19,320 --> 00:06:21,480 to map and measure our world. 92 00:06:21,480 --> 00:06:26,880 Today, scientists at NASA are preparing to measure and map the planets of our solar system. 93 00:06:26,880 --> 00:06:28,960 Hmm, who knows? 94 00:06:28,960 --> 00:06:31,920 Maybe one day one of you will help survey Mars. 95 00:06:31,920 --> 00:06:36,760 Did you know that George Washington was a surveyor before he became president? 96 00:06:36,760 --> 00:06:41,160 Did you know Lewis and Clark used transits on the Exploration Mission? 97 00:06:41,160 --> 00:06:48,320 To understand angles and circumference, let's look at something we can all relate to, pizza. 98 00:06:48,320 --> 00:06:49,320 Take a slice of pizza. 99 00:06:49,320 --> 00:06:53,920 Can you tell just by looking at it how many slices were in the original pizza and how 100 00:06:53,920 --> 00:06:55,760 big a round it was? 101 00:06:55,760 --> 00:06:56,760 Sure you can. 102 00:06:56,760 --> 00:06:58,440 All it takes is a little geometry. 103 00:06:58,440 --> 00:07:02,760 A pizza usually has eight identical slices, but not all of them. 104 00:07:02,760 --> 00:07:06,280 So let's measure the angle width of this slice. 105 00:07:06,280 --> 00:07:08,720 That's the part you put in your mouth first. 106 00:07:08,720 --> 00:07:13,840 Excuse me, sir, what does this protractor read? 107 00:07:13,840 --> 00:07:16,960 The protractor reads an angle width of 45 degrees. 108 00:07:16,960 --> 00:07:17,960 Right. 109 00:07:18,600 --> 00:07:21,680 Now, what is the measurement of all the other angles touching the center? 110 00:07:21,680 --> 00:07:25,680 They have to be equal or the same measurement, 45 degrees. 111 00:07:25,680 --> 00:07:26,680 Right. 112 00:07:26,680 --> 00:07:31,600 Now, most pizzas are circular and circles measure 360 degrees. 113 00:07:31,600 --> 00:07:39,200 If you divide 360 degrees by 45 degrees, the original pizza had eight slices. 114 00:07:39,200 --> 00:07:42,880 Now, let's figure the circumference of this pizza. 115 00:07:42,880 --> 00:07:44,720 Most pizzas are measured in inches. 116 00:07:44,720 --> 00:07:49,640 So, using the pizza with eight slices, if the length of the crust arc is five and a 117 00:07:49,640 --> 00:07:51,880 half inches, how round is your pizza? 118 00:07:51,880 --> 00:08:00,720 If there are eight slices and the crust arc measures 5.5 inches long, then eight times 119 00:08:00,720 --> 00:08:04,440 5.5 inches equals 44 inches. 120 00:08:04,440 --> 00:08:08,280 The pizza has a circumference of 44 inches. 121 00:08:08,280 --> 00:08:09,280 Great. 122 00:08:09,280 --> 00:08:10,280 Try this one. 123 00:08:10,840 --> 00:08:16,000 The angle width of your pizza slice measures 30 degrees and the crust arc is two and a 124 00:08:16,000 --> 00:08:17,400 half inches. 125 00:08:17,400 --> 00:08:22,200 How many slices would there be in the original pizza and what is the circumference? 126 00:08:22,200 --> 00:08:23,480 I've got it. 127 00:08:23,480 --> 00:08:28,160 360 degrees divided by 30 degrees equals 12 slices. 128 00:08:28,160 --> 00:08:33,920 12 slices times 2.5 inches equals a circumference of 30 inches. 129 00:08:33,920 --> 00:08:39,320 So, sir, would you rather eat a 12-slice pizza or an 8-slice pizza? 130 00:08:39,360 --> 00:08:41,360 Hmm, I'll choose the 8-slices. 131 00:08:41,360 --> 00:08:43,360 I couldn't possibly eat 12. 132 00:08:46,760 --> 00:08:51,760 Did you know that over 2,000 years ago, a Greek librarian used geometry to determine 133 00:08:51,760 --> 00:08:53,360 the circumference of the Earth? 134 00:08:58,360 --> 00:08:59,360 Hi, there. 135 00:08:59,360 --> 00:09:00,360 It's Tom. 136 00:09:00,360 --> 00:09:01,360 Can you explain the circumference of the Earth? 137 00:09:01,360 --> 00:09:07,240 What are the angle relationships between parallel lines and a transversal? 138 00:09:07,280 --> 00:09:12,320 The concept of the Earth being a large sphere was not unknown to the ancient Greeks. 139 00:09:12,320 --> 00:09:17,040 An everyday observation, such as the disappearance of ships below the horizon, indicated that 140 00:09:17,040 --> 00:09:19,760 the Earth might be spherical or round. 141 00:09:19,760 --> 00:09:21,480 But how large was it? 142 00:09:21,480 --> 00:09:26,400 The person who figured it out was a librarian named Aristophanes, who lived in Alexandria, 143 00:09:26,400 --> 00:09:29,520 Egypt about 300 BC. 144 00:09:29,520 --> 00:09:33,400 While looking through a scroll one day, he read that at noon on the longest day of the 145 00:09:33,400 --> 00:09:39,120 year, a vertical column cast no shadow in Syene, a city south of Alexandria. 146 00:09:39,120 --> 00:09:42,840 Aristophanes knew that this did not happen in Alexandria. 147 00:09:42,840 --> 00:09:47,720 He thought to himself, how was it possible to have shadows in Alexandria and not in Syene 148 00:09:47,720 --> 00:09:49,920 at the same time of day? 149 00:09:49,920 --> 00:09:56,320 Aristophanes figured out that the sun must be directly overhead in Syene but not in Alexandria. 150 00:09:56,320 --> 00:09:57,320 Aha! 151 00:09:57,320 --> 00:10:01,200 Here was proof that the Earth's surface is curved. 152 00:10:01,400 --> 00:10:05,160 Using a little geometry, Aristophanes set out to determine the circumference of the 153 00:10:05,160 --> 00:10:09,000 Earth and find out just how big it is. 154 00:10:09,000 --> 00:10:14,880 Just like our pizza example, if our friend Aristophanes could determine the central angle 155 00:10:14,880 --> 00:10:20,920 at the center of the Earth and the length of the edge or arc, then he could figure out 156 00:10:20,920 --> 00:10:22,600 the circumference of the Earth. 157 00:10:22,600 --> 00:10:27,840 Now, finding the length of the edge or arc was fairly simple math. 158 00:10:27,840 --> 00:10:33,200 Aristophanes asked a friend to walk from Alexandria to Syene to measure the distance 159 00:10:33,200 --> 00:10:35,040 between the two cities. 160 00:10:35,040 --> 00:10:41,160 His friend estimated the distance to be around 800 kilometers or about 500 miles. 161 00:10:41,160 --> 00:10:45,600 Finding the central angle, however, would take some geometry. 162 00:10:45,600 --> 00:10:52,040 First, Aristophanes assumed correctly, I might add, that the sun's rays are parallel since 163 00:10:52,040 --> 00:10:53,600 the sun is so far away. 164 00:10:53,600 --> 00:10:54,600 Check this out. 165 00:10:54,720 --> 00:10:59,480 In this diagram, we can see that there is no shadow at Syene, while there is a shadow 166 00:10:59,480 --> 00:11:01,320 in Alexandria. 167 00:11:01,320 --> 00:11:06,400 The line that is formed by the gnomon, or vertical column at Alexandria and the center 168 00:11:06,400 --> 00:11:13,160 of the Earth, cuts or intersects the two parallel lines formed from the sun's rays. 169 00:11:13,160 --> 00:11:17,560 A line that intersects two parallel lines is called a transversal. 170 00:11:17,560 --> 00:11:23,040 The two angles formed from the transversal line and the parallel lines are called alternate 171 00:11:23,040 --> 00:11:25,200 interior angles. 172 00:11:25,200 --> 00:11:28,160 And according to geometric rule, they are equal. 173 00:11:28,160 --> 00:11:29,680 Let's prove it. 174 00:11:29,680 --> 00:11:34,520 Take a piece of paper of any width and draw a diagonal line on it. 175 00:11:34,520 --> 00:11:37,240 Label the angles A and B just like this. 176 00:11:37,240 --> 00:11:42,240 Now, cut the paper along the diagonal so you have two triangles. 177 00:11:42,240 --> 00:11:45,960 Compare angles A and B by placing one angle on top of the other. 178 00:11:45,960 --> 00:11:47,880 Hey, what do you notice? 179 00:11:47,880 --> 00:11:51,640 The angles are equal no matter what size paper you started with. 180 00:11:51,640 --> 00:11:52,640 Right. 181 00:11:52,640 --> 00:11:58,600 When two parallel lines are intersected by a transversal, the alternate interior angles 182 00:11:58,600 --> 00:11:59,600 are equal. 183 00:11:59,600 --> 00:12:00,600 Huh. 184 00:12:00,600 --> 00:12:03,320 Aristophanes was quite a geometer. 185 00:12:03,320 --> 00:12:08,760 From his measurements, Aristophanes calculated the sun's rays made an angle of 7.5 degrees 186 00:12:08,760 --> 00:12:09,920 at Alexandria. 187 00:12:09,920 --> 00:12:15,800 Now, since this angle was formed by two parallel lines and a transversal, the central angle 188 00:12:15,800 --> 00:12:19,600 of the Earth must also be 7.5 degrees. 189 00:12:19,600 --> 00:12:24,680 By knowing these two things, the central angle and the distance from Alexandria to 190 00:12:24,680 --> 00:12:29,200 Syene, Aristophanes calculated the circumference of the Earth. 191 00:12:29,200 --> 00:12:38,000 360 degrees divided by 7.5 degrees equals 48 slices of the Earth. 192 00:12:38,000 --> 00:12:39,000 Are you still with me? 193 00:12:39,000 --> 00:12:40,000 Okay. 194 00:12:40,000 --> 00:12:41,000 Hang tight. 195 00:12:41,000 --> 00:12:42,000 We're almost there. 196 00:12:42,000 --> 00:12:47,080 Now, if you remember that the estimated distance between Alexandria and Syene is 800 kilometers 197 00:12:47,080 --> 00:12:53,920 and you multiply that distance by the number of slices in the Earth, 48, what is the circumference 198 00:12:53,920 --> 00:12:55,720 of the Earth? 199 00:12:55,720 --> 00:13:04,680 Well, if you estimated that distance to be 38,000 kilometers, you're absolutely right. 200 00:13:04,680 --> 00:13:09,720 Aristophanes' estimate was really close to the Earth's circumference, which is 40,074 201 00:13:09,720 --> 00:13:10,720 kilometers. 202 00:13:10,720 --> 00:13:17,480 His percentage error was about 5% and was probably due to an error in the distance between 203 00:13:17,480 --> 00:13:18,480 the two cities. 204 00:13:18,480 --> 00:13:19,480 5%? 205 00:13:19,480 --> 00:13:20,480 Huh. 206 00:13:20,480 --> 00:13:25,920 That's pretty good, considering Aristophanes used only his feet, his eyes, his imagination, 207 00:13:25,920 --> 00:13:28,920 and of course, his knowledge of geometry. 208 00:13:28,920 --> 00:13:32,600 There are other ways that we survey the Earth, which Aristophanes never dreamed of. 209 00:13:32,600 --> 00:13:35,400 NASA scientists use airplanes and satellites. 210 00:13:35,400 --> 00:13:40,280 But what if we wanted to survey other planets like Mars? 211 00:13:40,840 --> 00:13:42,840 NASA scientists are doing that right now. 212 00:13:42,840 --> 00:13:46,840 But first, let's head to Central Middle School in Charlotte Courthouse, Virginia. 213 00:13:46,840 --> 00:13:49,840 There, students are following in the footsteps of Aristophanes. 214 00:13:50,840 --> 00:13:51,840 Hi! 215 00:13:51,840 --> 00:13:57,840 We're from Central Middle School in Charlotte Courthouse, Virginia. 216 00:13:57,840 --> 00:14:02,840 NASA Connect asked us to show you how to do the student activity for this show. 217 00:14:02,840 --> 00:14:09,320 In this lesson, you will work in small groups to take accurate measurements of shadows using 218 00:14:09,360 --> 00:14:12,360 geometry to determine the size of an angle. 219 00:14:12,360 --> 00:14:15,360 Here are the materials you'll need for each group. 220 00:14:15,360 --> 00:14:19,360 A straight stick approximately 91 centimeters long. 221 00:14:19,360 --> 00:14:22,360 A meter stick or tape measure. 222 00:14:22,360 --> 00:14:27,360 A piece of string approximately 91 centimeters and a rocker weight. 223 00:14:27,360 --> 00:14:30,360 A scientific calculator. 224 00:14:30,360 --> 00:14:32,360 Index card. 225 00:14:32,360 --> 00:14:34,360 Compass. 226 00:14:34,360 --> 00:14:37,360 Copies of the student data chart for each student. 227 00:14:37,360 --> 00:14:38,360 Let's begin. 228 00:14:38,400 --> 00:14:42,400 Divide the class in research groups of three to five members. 229 00:14:43,400 --> 00:14:49,400 Set your measurement station by first placing the gnomon perpendicular to the ground. 230 00:14:49,400 --> 00:14:54,400 For your measurement to be accurate, it is critical that the gnomon is vertical. 231 00:14:54,400 --> 00:15:03,400 To check the vertical position, tie the rock or weight to the string and dangle it above the ground in front of the gnomon. 232 00:15:03,400 --> 00:15:06,400 Next, measure the height of the gnomon. 233 00:15:06,440 --> 00:15:11,440 Place an index card under the station to mark where the shadow ends. 234 00:15:11,440 --> 00:15:16,440 Take measurements every two minutes beginning at least ten minutes before local noon, 235 00:15:16,440 --> 00:15:20,440 which is the time that the sun is highest in the sky. 236 00:15:20,440 --> 00:15:26,440 This will most likely not be noon as indicated on your time measuring device. 237 00:15:26,440 --> 00:15:32,440 Students should note that when the sun is highest in the sky, the shadow length is the shortest. 238 00:15:32,480 --> 00:15:39,480 Since the edge of the shadow is fuzzy and the shadow is moving from east to west in the northern hemisphere, 239 00:15:39,480 --> 00:15:42,480 be careful in deciding where to place your mark. 240 00:15:42,480 --> 00:15:45,480 Record your data on data chart one. 241 00:15:45,480 --> 00:15:54,480 Now, back in your classroom, locate the latitude and longitude of your school location and record it on data chart number one. 242 00:15:54,480 --> 00:15:57,480 Identify your best shadow length. 243 00:15:57,480 --> 00:16:01,480 This is the best shadow length at local noon time. 244 00:16:01,520 --> 00:16:09,520 Next, calculate the tangent by dividing the length of the shadow by the height of the gnomon. 245 00:16:09,520 --> 00:16:15,520 Locate this number, or the nearest rounded number, on the tangent table. 246 00:16:15,520 --> 00:16:25,520 The measure of the tangent can also be found by dividing the length of a shadow by the height of an object on the scientific calculator. 247 00:16:25,520 --> 00:16:29,520 Record tangent on student data chart. 248 00:16:29,560 --> 00:16:33,560 Make a scale drawing of your gnomon and shadow. 249 00:16:33,560 --> 00:16:38,560 Complete the triangle and measure the tangent with a protractor to verify your calculations. 250 00:16:38,560 --> 00:16:40,560 What's next, Jennifer? 251 00:16:40,560 --> 00:16:47,560 Let's analyze the data by reviewing the results of this activity and by responding to the following questions. 252 00:16:47,560 --> 00:16:52,560 Did the weather conditions affect the results of this activity? 253 00:16:52,560 --> 00:16:55,560 If so, how? 254 00:16:55,600 --> 00:17:03,600 As the shadow lengthens over time, how will the angle be affected? 255 00:17:03,600 --> 00:17:12,600 If each group uses a gnomon with a different length, how will that affect the results of this activity? 256 00:17:12,600 --> 00:17:23,600 For more activities like this, check out our website at edu.larc.nasa.gov forward slash connect. 257 00:17:23,640 --> 00:17:31,640 NASA Connect would like to give a special thanks to the mentors from the AIAA chapter at Howard University in Washington, D.C. 258 00:17:31,640 --> 00:17:34,640 We appreciate all your help with the student activity. 259 00:17:34,640 --> 00:17:36,640 Okay, let's review. 260 00:17:36,640 --> 00:17:42,640 We've seen how the sun's position, satellites, and geometry help us survey the Earth. 261 00:17:42,640 --> 00:17:45,640 But what if we wanted to survey Mars? 262 00:17:45,640 --> 00:17:51,640 Well, we don't live on Mars, so how do scientists and NASA survey the red planet? 263 00:17:51,680 --> 00:17:52,680 I thought you'd never ask. 264 00:17:52,680 --> 00:17:57,680 Let's visit NASA's Jet Propulsion Laboratory in Pasadena, California and find out. 265 00:18:01,680 --> 00:18:04,680 What is the Mars Global Surveyor and where is it? 266 00:18:04,680 --> 00:18:10,680 How does the Mars Global Surveyor use geometry to survey the Martian landscape? 267 00:18:10,680 --> 00:18:15,680 The Mars Global Surveyor is a spacecraft that is in orbit around Mars. 268 00:18:15,720 --> 00:18:22,720 Its purpose is to take pictures of Mars, to measure the temperature of the surface and the atmosphere of Mars, 269 00:18:22,720 --> 00:18:29,720 and to bounce laser signals off the surface of Mars to precisely determine the shape of Mars. 270 00:18:29,720 --> 00:18:34,720 You might think of Mars as simply being a sphere by looking at pictures of it. 271 00:18:34,720 --> 00:18:38,720 But to scientists, it has lots of bumps and ridges. 272 00:18:38,760 --> 00:18:48,760 For example, the poles of Mars are so cold that the atmosphere actually condenses out to form dry ice at the poles. 273 00:18:48,760 --> 00:18:54,760 And as much as 25% of the atmosphere condenses out into the dry ice at the poles. 274 00:18:54,760 --> 00:18:58,760 So there's quite a large change in the atmosphere. 275 00:18:58,760 --> 00:19:03,760 Also, Mars is known for having a large bulge on the side of it. 276 00:19:03,800 --> 00:19:08,800 It's the largest volcano in the solar system, known as Olympus Mons. 277 00:19:08,800 --> 00:19:16,800 And so one of the functions of the Mars Global Surveyor was to measure the shape of Mars to carefully determine how big is this bulge. 278 00:19:16,800 --> 00:19:22,800 Because it has a huge effect on the orbits of spacecraft. It's such a large bulge on the side. 279 00:19:22,800 --> 00:19:29,800 The way that we use geometry to convert the laser pulses into the shape of Mars, 280 00:19:29,840 --> 00:19:36,840 what we have to do is carefully time how long it takes for the pulses to reach Mars and bounce back to the spacecraft. 281 00:19:36,840 --> 00:19:46,840 And then we combine that with the shape of the orbit, which we determine by looking at how the radio signal changes as the spacecraft goes around Mars. 282 00:19:49,840 --> 00:19:54,840 What is aerobraking? How does geometry influence aerobraking? 283 00:19:54,880 --> 00:20:02,880 Aerobraking is when we use drag from the atmosphere to gradually shrink the orbit down. 284 00:20:02,880 --> 00:20:12,880 So what we have to do is use the drag from the atmosphere to gradually slow the orbit down so that it would shrink from this highly elliptical 45-hour orbit 285 00:20:12,880 --> 00:20:17,880 down to a very circular two-hour orbit around Mars. 286 00:20:17,880 --> 00:20:19,880 This is geometry in action. 287 00:20:19,920 --> 00:20:27,920 How would you like to try your hand at designing your own Mars Global Surveyor? 288 00:20:27,920 --> 00:20:34,920 Before introducing you to our featured EdTech activity in middle school, I wanted to give you a quick tour of Norbert's lab. 289 00:20:34,920 --> 00:20:40,920 You already know Norbert. He's that funny character that provides us with the cute cards and other learning activities and aids 290 00:20:40,920 --> 00:20:46,920 to help us understand the math, science and technology concepts presented in each of the NASA Connect programs. 291 00:20:46,960 --> 00:20:53,960 His lab is your interactive link to activities and resources on the web, so you'll get the most out of NASA Connect. 292 00:20:53,960 --> 00:21:00,960 Just click on the rooms to enter areas like Career Corner, where you'll meet some of our guests and members of our television team. 293 00:21:00,960 --> 00:21:06,960 There's a study room with terms and definitions related to the show, and a page with links to other cool sites. 294 00:21:06,960 --> 00:21:13,960 And this is where you'll get to the online activity, especially created in partnership with NASA's Learning Technologies team. 295 00:21:14,000 --> 00:21:22,000 To introduce us to the web activity for this show, let's pop in on a teacher and her students at Davis Middle School in Hampton, Virginia. 296 00:21:22,000 --> 00:21:27,000 Thanks, Jelly. My name is Vivian Carr, and I'm a math and science teacher here at Davis Middle School. 297 00:21:27,000 --> 00:21:35,000 My students love coming to the computer lab. They use it for reinforcement and enrichment of many skills in most of the content areas. 298 00:21:35,000 --> 00:21:41,000 Now I'd like to introduce you to Ruby Bruno. Ruby, tell us, how do you use technology? 299 00:21:41,040 --> 00:21:46,040 Technology is a tool that we use in several ways, for communication with others through email, 300 00:21:46,040 --> 00:21:53,040 for conducting research using the internet, for writing papers and preparing electronic presentations of our work, 301 00:21:53,040 --> 00:22:00,040 and for participating in problem-solving online projects such as NASA Connect to reinforce what we are learning in class. 302 00:22:00,040 --> 00:22:08,040 In the online component for this show, we're learning what goes into the design of a spacecraft used for planetary observation. 303 00:22:08,080 --> 00:22:14,080 To do this, we learn about different instruments used for observing planetary surfaces from space. 304 00:22:14,080 --> 00:22:16,080 One of these is a camera. 305 00:22:16,080 --> 00:22:24,080 We get to pick out what we think are the right batteries to use as well as the size of the solar panels required to run the spacecraft. 306 00:22:24,080 --> 00:22:32,080 We'll also have to consider the cost and weight of the vehicle as we try to put together the best possible planetary observer 307 00:22:32,080 --> 00:22:36,080 we can with all the variables given to us in the activity. 308 00:22:36,120 --> 00:22:40,120 Well, Jennifer, the students here at Davis Middle School leave you and our viewers with the challenge 309 00:22:40,120 --> 00:22:47,120 to assemble and test their very own Mars Surveyor in a cost-effective way that produces the best results. 310 00:22:47,120 --> 00:22:53,120 Viewers can find that challenge in Norbitz Lab on the NASA Connect website. See you on the web. 311 00:22:53,120 --> 00:22:59,120 Let's head to NASA Langley Research Center in Hampton, Virginia and meet up with some George Washington University graduate students. 312 00:22:59,120 --> 00:23:04,120 They are using pictures from the Mars Global Surveyor and geometry to survey Mars. 313 00:23:04,160 --> 00:23:09,160 Music 314 00:23:09,160 --> 00:23:11,160 How are shadows measured on Mars? 315 00:23:11,160 --> 00:23:17,160 How is geometry used to determine the height of land formation on Mars? 316 00:23:17,160 --> 00:23:21,160 Hey guys, I want you to meet Corey Hernandez and Brooke Anderson. 317 00:23:21,160 --> 00:23:24,160 They're graduate students at George Washington University. 318 00:23:24,160 --> 00:23:26,160 Guys, what are you studying over there? 319 00:23:26,160 --> 00:23:32,160 Well, with simple geometry and shadows, we're able to determine the elevation on Mars' surface 320 00:23:32,200 --> 00:23:37,200 such as a mountain, Olympus Mons, that's three times the size of Mount Everest 321 00:23:37,200 --> 00:23:41,200 or a valley, Valles Marineris, which is the size of the United States. 322 00:23:41,200 --> 00:23:43,200 Wow, those are some pretty large land formations. 323 00:23:43,200 --> 00:23:49,200 So, let me get this right, what you're telling me is that geometry is used to determine the elevation of land formations on Mars? 324 00:23:49,200 --> 00:23:53,200 Yes, and we set up an example here for you to demonstrate this. 325 00:23:53,200 --> 00:23:59,200 If this is a mountain on the surface of Mars, this is a protractor to measure the angle of the sun. 326 00:23:59,240 --> 00:24:02,240 This is a metric ruler to measure the length of a shadow. 327 00:24:02,240 --> 00:24:07,240 If this flashlight represents the sun, we know that, like here on Earth, 328 00:24:07,240 --> 00:24:11,240 the sun is directly overhead at 90 degrees at high noon, and as the day goes on, 329 00:24:11,240 --> 00:24:13,240 it goes down to zero degrees at sunset. 330 00:24:13,240 --> 00:24:17,240 So, Corey, what you're telling me is this model here creates a right triangle? 331 00:24:17,240 --> 00:24:21,240 The bottom leg can be represented by the length of the shadow, 332 00:24:21,240 --> 00:24:24,240 which we can get from taking a picture with the Mars Global Surveyor. 333 00:24:24,240 --> 00:24:28,240 Now, the sun makes an angle between the hypotenuse and the bottom leg. 334 00:24:28,280 --> 00:24:31,280 So, let's pretend it's mid-afternoon on Mars. 335 00:24:31,280 --> 00:24:35,280 The sun would be at about an angle of 45 degrees. 336 00:24:35,280 --> 00:24:37,280 Which, Brooke, how long is our shadow? 337 00:24:37,280 --> 00:24:39,280 It gives us about 17 centimeters. 338 00:24:39,280 --> 00:24:41,280 Wow, so you got your angle there. 339 00:24:41,280 --> 00:24:47,280 Yes. So, using our formula, remembering the tangent of 45 degrees is equal to 1, 340 00:24:47,280 --> 00:24:51,280 which we can find from our scientific calculators or our tangent tables, 341 00:24:51,280 --> 00:24:54,280 we can find the height of our mountain to be 17 centimeters. 342 00:24:54,320 --> 00:24:56,320 So, to double-check our answer, 343 00:24:56,320 --> 00:25:01,320 we can see that the height of our mountain is 17 centimeters. 344 00:25:01,320 --> 00:25:04,320 That's about what you calculated. That's pretty cool, Corey. 345 00:25:04,320 --> 00:25:08,320 Well, I looked at Mars through the telescope, and it is definitely red. 346 00:25:08,320 --> 00:25:11,320 But could green slime have once existed on the red planet? 347 00:25:11,320 --> 00:25:14,320 That's one of the many reasons NASA Ames Research Center 348 00:25:14,320 --> 00:25:17,320 in Moffett Field, California, is studying Mars. 349 00:25:17,320 --> 00:25:23,320 So, now let's join researcher Chris McKay with the latest on green slime. 350 00:25:23,360 --> 00:25:27,360 I'm interested in Mars, and in particular, life on Mars. 351 00:25:27,360 --> 00:25:30,360 We know that early in Mars' history, it had water, lots of water. 352 00:25:30,360 --> 00:25:33,360 We can see the rivers and lakes that were formed by that water. 353 00:25:33,360 --> 00:25:36,360 The question is, when it had water, did it have life? 354 00:25:36,360 --> 00:25:40,360 To understand how life might have survived on a cold planet like Mars 355 00:25:40,360 --> 00:25:43,360 and where to look for it, we go to places on Earth 356 00:25:43,360 --> 00:25:46,360 where life is surviving in very cold, dry conditions, 357 00:25:46,360 --> 00:25:47,360 Mars-like conditions. 358 00:25:47,360 --> 00:25:51,360 This is a rock from the Antarctic, the dry valleys of Antarctica, 359 00:25:51,400 --> 00:25:53,400 the most Mars-like place on Earth. 360 00:25:53,400 --> 00:25:56,400 In this rock, there's life, but it's hidden inside the rock. 361 00:25:56,400 --> 00:25:59,400 Just below the surface, there's a layer of green. 362 00:25:59,400 --> 00:26:02,400 These are algae and lichens, and they're growing inside the rock 363 00:26:02,400 --> 00:26:05,400 because the rock provides them a source of moisture, 364 00:26:05,400 --> 00:26:08,400 while at the same time allowing enough light to come through. 365 00:26:08,400 --> 00:26:11,400 By studying life forms in these environments, 366 00:26:11,400 --> 00:26:15,400 we learn about the strategies that life can use in a cold, dry place. 367 00:26:15,400 --> 00:26:18,400 We might apply those strategies to the search for life on Mars. 368 00:26:18,440 --> 00:26:21,440 And maybe we'll find evidence that there was life there 369 00:26:21,440 --> 00:26:25,440 when Mars was not too much colder than the dry valleys of Antarctica. 370 00:26:25,440 --> 00:26:28,440 Well, looks like the sun has shifted, 371 00:26:28,440 --> 00:26:30,440 and that's about all we have time for today. 372 00:26:30,440 --> 00:26:33,440 But before we go, Jennifer and I would love to hear from you 373 00:26:33,440 --> 00:26:34,440 with your comments and ideas, 374 00:26:34,440 --> 00:26:36,440 so why don't you drop us a line at 375 00:26:36,440 --> 00:26:43,440 NASA Connect, NASA LARC MS400, Hampton, Virginia 23681. 376 00:26:43,480 --> 00:26:50,480 And if you're on the web, email us at connect at edu.larc.nasa.gov. 377 00:26:50,480 --> 00:26:52,480 We'd like to thank everyone who helped us today. 378 00:26:52,480 --> 00:26:55,480 The Virginia Living Museum, George Washington University, 379 00:26:55,480 --> 00:26:58,480 our NASA researchers from NASA Langley Research Center, 380 00:26:58,480 --> 00:27:02,480 NASA Ames Research Center, and NASA's Jet Propulsion Laboratory, 381 00:27:02,480 --> 00:27:05,480 Dr. Shelley Canright, and especially the students 382 00:27:05,480 --> 00:27:07,480 and teachers from our middle school. 383 00:27:07,480 --> 00:27:08,480 Thanks, guys. 384 00:27:08,480 --> 00:27:12,480 If you would like a videotaped copy of this NASA Connect show 385 00:27:12,520 --> 00:27:14,520 and the Educator's Guide lesson plans, 386 00:27:14,520 --> 00:27:20,520 contact CORE, the NASA Central Operation of Resources for Educators. 387 00:27:20,520 --> 00:27:25,520 All this information and more is located on the NASA Connect website. 388 00:27:25,520 --> 00:27:27,520 For the NASA Connect series, I'm Jennifer Pulley. 389 00:27:27,520 --> 00:27:28,520 And I'm Van Hughes. 390 00:27:28,520 --> 00:27:31,520 See you next time. 391 00:27:31,520 --> 00:27:33,520 Take a slice of pizza. 392 00:27:33,520 --> 00:27:36,520 Oh, you got it. 393 00:27:36,520 --> 00:27:40,520 What is serving? 394 00:27:40,560 --> 00:27:43,560 One of the functions of the Mars Global Surveyor 395 00:27:43,560 --> 00:27:46,560 was to watch it fall off. 396 00:27:46,560 --> 00:27:51,560 How is geometry used to measure? 397 00:27:51,560 --> 00:27:54,560 Today, we'll use this. 398 00:27:54,560 --> 00:27:58,560 What are the angles? 399 00:27:58,560 --> 00:28:04,560 The sun would be at about an angle of 45 degrees. 400 00:28:04,560 --> 00:28:08,560 How are shatters? 401 00:28:08,600 --> 00:28:12,600 Guys, tell me what you're studying over there. 402 00:28:12,600 --> 00:28:13,600 Welcome to NASA Connect. 403 00:28:13,600 --> 00:28:14,600 Sorry, my fault. 404 00:28:14,600 --> 00:28:15,600 Welcome to NASA Connect. 405 00:28:15,600 --> 00:28:16,600 Sorry. 406 00:28:16,600 --> 00:28:17,600 And I'm Van Hughes. 407 00:28:17,600 --> 00:28:20,600 Today, we're here at the... 408 00:28:20,600 --> 00:28:22,600 I think I see... 409 00:28:22,600 --> 00:28:23,600 Whoa. 410 00:28:23,600 --> 00:28:24,600 Whoa. 411 00:28:24,600 --> 00:28:25,600 Whoa. 412 00:28:25,600 --> 00:28:26,600 Whoa. 413 00:28:26,600 --> 00:28:27,600 Whoa. 414 00:28:27,600 --> 00:28:28,600 Whoa. 415 00:28:28,600 --> 00:28:29,600 Whoa. 416 00:28:29,600 --> 00:28:30,600 Whoa. 417 00:28:30,600 --> 00:28:30,600