1 00:00:00,050 --> 00:00:04,210 (off screen) “So joining us now from NASA’s Goddard Space Flight Center is Dr. Michelle Thaller. 2 00:00:04,230 --> 00:00:08,390 Thanks for joining us.” (Thaller) “Thank you, great to be here.’ (off screen) “So tell us what exactly is a 3 00:00:08,410 --> 00:00:12,570 supermoon and will it affect Earth?” (Thaller) “Well a supermoon happens when you 4 00:00:12,590 --> 00:00:16,680 get a full moon near a perigee. And perigees are a word for the closest 5 00:00:16,700 --> 00:00:20,800 approach the moon makes to the Earth every month. Apogee is the farthest away. 6 00:00:20,820 --> 00:00:24,910 You see the moon’s orbit is not a perfect circle. It’s actually a little elliptical. Sometimes 7 00:00:24,930 --> 00:00:29,030 it’s a little farther away. Sometimes it’s a little closer. And that means that the size of the moon 8 00:00:29,050 --> 00:00:33,160 seems to change in the sky. And when you get a full moon that happens when 9 00:00:33,180 --> 00:00:37,280 the moon is very close, that’s called a supermoon. Now as far as the affects 10 00:00:37,300 --> 00:00:41,380 on the Earth…nothing very direct. The actual size of the moon in the sky doesn’t change 11 00:00:41,400 --> 00:00:45,460 very much. It’s only about 12 percent larger than an average full moon. 12 00:00:45,480 --> 00:00:49,510 And as you may know, the highest tides of the month happen at 13 00:00:49,530 --> 00:00:53,540 full moon and new moon. These are called the spring tides of each month. 14 00:00:53,560 --> 00:00:57,720 And because the moon is a little closer than normal, that means the tides will be a little bit higher 15 00:00:57,740 --> 00:01:01,890 than normal as well. But we’re talking about a change of less than an inch. 16 00:01:01,910 --> 00:01:06,070 So one of the challenges about measuring what they call the perigean tide, 17 00:01:06,090 --> 00:01:10,250 the high tides associated with a supermoon, is even measuring it at 18 00:01:10,270 --> 00:01:14,430 all. It’s a fun thing to actually detect. It’s not something that you can easily see. 19 00:01:14,450 --> 00:01:18,600 (off screen) “So what is the best time to view the supermoon and will it look different 20 00:01:18,620 --> 00:01:22,780 from other full moons?” (Thaller) “Well to me the best time to view 21 00:01:22,800 --> 00:01:26,940 any full moon is right at sunset because that’s when it rises. And when you see the 22 00:01:26,960 --> 00:01:31,080 moon with respect to the horizon with buildings and trees or whatever 23 00:01:31,100 --> 00:01:35,220 it just seems to look so much more spectacular. It looks larger. In reality 24 00:01:35,240 --> 00:01:39,320 the size changes not that much. The moon at perigee or closest is just 25 00:01:39,340 --> 00:01:43,370 a little bit larger than the moon when its farther away. Um there really 26 00:01:43,390 --> 00:01:47,470 isn’t a best time at night to view this. Kind of a trivia that the actual moment 27 00:01:47,490 --> 00:01:51,540 of supermoon when it’s both closest and the most full is going 28 00:01:51,560 --> 00:01:55,590 to be at 7:30 a.m. this Sunday. But that’s actually after the moon has set. 29 00:01:55,610 --> 00:01:59,640 So I would say anytime on Saturday night, go out and look at this beautiful big, 30 00:01:59,660 --> 00:02:03,830 bright, full moon. My personal favorite time is right after sunset. 31 00:02:03,850 --> 00:02:08,010 (off screen) “NASA has a major observatory in orbit around the moon right 32 00:02:08,030 --> 00:02:12,190 now call the Lunar Reconnaissance Orbiter. What are some of the cool things you’re seeing.” 33 00:02:12,210 --> 00:02:16,370 (Thaller) “Well yeah so we actually have an observatory orbiting the moon right now. 34 00:02:16,390 --> 00:02:20,550 And we are returning spectacular high-resolution images of the entire 35 00:02:20,570 --> 00:02:24,690 lunar surface. We can see all the Apollo landing sites, the footprints of the 36 00:02:24,710 --> 00:02:28,860 astronauts. The poles of the moon are fascinating places. 37 00:02:28,880 --> 00:02:33,010 There are actually craters both at the north and south pole of the moon where the sun never 38 00:02:33,030 --> 00:02:37,140 shines. You never get any sunlight at all. And of course those are very difficult to image. 39 00:02:37,160 --> 00:02:41,250 . But we’re actually bouncing lasers down to the moon. We’re studying the topography 40 00:02:41,270 --> 00:02:45,370 of these craters. And there’s evidence that there may be ice actually frozen 41 00:02:45,390 --> 00:02:49,450 into the soil in these permanently shadowed craters. So there may be more 42 00:02:49,470 --> 00:02:53,520 water on the moon, frozen water, than we suspected. So LRO is telling 43 00:02:53,540 --> 00:02:57,570 us so much about how the moon came to be, how it changes over time. 44 00:02:57,590 --> 00:03:01,620 We’ve recorded the coldest temperature in the entire solar system with LRO in one of these 45 00:03:01,640 --> 00:03:05,810 permanently shadowed craters. It’s about 23 Celsius above absolute 46 00:03:05,830 --> 00:03:09,990 zero, which is actually much colder than 400 degrees 47 00:03:10,010 --> 00:03:14,180 below zero Fahrenheit. So just a fascinating place and we’re finding out 48 00:03:14,200 --> 00:03:18,360 new things all the time. There’s so much more to learn about this familiar object 49 00:03:18,380 --> 00:03:22,540 in the sky. (off screen) “I understand that LRO has taken some really incredible 50 00:03:22,560 --> 00:03:26,720 images. Can you talk about some of those?” (Thaller) “Well I know that certainly some of my 51 00:03:26,740 --> 00:03:30,900 favorite images are of the Apollo landing sites. In some cases you can actually see the American 52 00:03:30,920 --> 00:03:35,080 flag still up. I’m also a particular fan of 53 00:03:35,100 --> 00:03:39,250 the central mountain peak inside Tycho Crater. You can see this gorgeous mountain 54 00:03:39,270 --> 00:03:43,440 right inside the crater. There are boulders on it that are as big as baseball stadiums. 55 00:03:43,460 --> 00:03:47,610 And I just love the variation of the lunar 56 00:03:47,630 --> 00:03:51,740 terrain. There are dark lava plains that are relatively smooth. 57 00:03:51,760 --> 00:03:55,850 There are high regions where it’s very rocky and bouldery. It tells us 58 00:03:55,870 --> 00:03:59,940 about the evolution of the solar system. You can actually see the scars left by 59 00:03:59,960 --> 00:04:04,010 huge impacts. Here again we have that gorgeous mountain inside Tycho Crater. 60 00:04:04,030 --> 00:04:08,060 That one boulder you see in the middle is the size of an entire 61 00:04:08,080 --> 00:04:12,090 football stadium. It’s incredibly huge. The moon is a 62 00:04:12,110 --> 00:04:16,270 relic of a more exciting and more violent time in our solar system’s 63 00:04:16,290 --> 00:04:20,440 formation when the planets were coming together. Lots of things were colliding. 64 00:04:20,460 --> 00:04:24,620 We think the moon may have been created during a super collision where the 65 00:04:24,640 --> 00:04:28,810 Earth was actually hit by something the size of a planet. So the moon is 66 00:04:28,830 --> 00:04:32,990 so serene and we see it, it’s so familiar to us. It’s also 67 00:04:33,010 --> 00:04:37,180 dramatic and violent and the stories associated with it 68 00:04:37,200 --> 00:04:41,350 just really fire my imagination.” (off screen) “So tell us, where 69 00:04:41,370 --> 00:04:45,520 can we learn more about the moon.” (Thaller) “Well I would say if you want to go through some of the 70 00:04:45,540 --> 00:04:49,690 best images NASA has of the moon, go to the LRO website. That would be 71 00:04:49,710 --> 00:04:53,830 NASA.GOV/LRO for Lunar Reconnaissance Orbiter. 72 00:04:53,850 --> 00:04:57,960 Look at the Apollo landing sites. Look at the giant mountains on the moon. Have fun 73 00:04:57,980 --> 00:05:02,060 fun exploring your closest neighbor in space.