WEBVTT FILE 1 00:00:00.010 --> 00:00:04.200 The Montreal Protocol has been a great success at banning 2 00:00:04.200 --> 00:00:08.270 the production of ozone-depleting substances. 3 00:00:08.270 --> 00:00:12.380 And we know this because we've been measuring those substances at the Earth's surface since 4 00:00:12.380 --> 00:00:16.520 the 1980s or even before. in some cases. So before the Montreal Protocol. 5 00:00:16.520 --> 00:00:20.700 ozone-depleting substances at the surface were going up rapidly. 6 00:00:20.700 --> 00:00:24.910 Once the Protocol was signed and the regulations went into effect. 7 00:00:24.910 --> 00:00:29.090 we saw at the surface. levels of ozone-depleting substances going down. 8 00:00:29.090 --> 00:00:33.460 And so that's great. But those substances have to 9 00:00:33.460 --> 00:00:37.630 get high up into the stratosphere before they can destroy ozone. and they have to break down 10 00:00:37.630 --> 00:00:41.810 high up in the stratosphere. and the chlorine that gets released from the chlorofluorocarbons 11 00:00:41.810 --> 00:00:45.990 that's what actually destroys ozone. What we haven't had up until 12 00:00:45.990 --> 00:00:50.170 now is any measurement inside the Antarctic ozone hole 13 00:00:50.170 --> 00:00:54.220 that the chlorine levels there is actually going down. What I've shown 14 00:00:54.220 --> 00:00:58.300 is that if you're very careful about when you measure 15 00:00:58.300 --> 00:01:02.340 hydrogen chloride. that's HCl. in the atmosphere. and you measure it over time. 16 00:01:02.340 --> 00:01:06.390 you can see that HCl. so that reactive chlorine that destroys 17 00:01:06.390 --> 00:01:10.460 ozone. those levels are actually going down inside the Antarctic 18 00:01:10.460 --> 00:01:14.580 ozone hole. So that's great. so that's part of saying. 19 00:01:14.580 --> 00:01:18.760 "Hey. the ozone hole's recovering. it's getting smaller and it's because of declining chlorine." 20 00:01:18.760 --> 00:01:22.930 But the other part is to also look at how much ozone depletion 21 00:01:22.930 --> 00:01:27.110 is going on at the same time. because ozone levels can vary 22 00:01:27.110 --> 00:01:31.290 for a lot of different reasons. mostly because of temperature. If one year it's warm. 23 00:01:31.290 --> 00:01:35.330 you don't have as much ozone depletion. One year's really cold. you have more ozone depletion. 24 00:01:35.330 --> 00:01:39.430 So it makes it really hard to see the signal that the atmosphere's showing 25 00:01:39.430 --> 00:01:43.610 us. is the ozone hole really recovering? So what we did 26 00:01:43.610 --> 00:01:47.640 in this study. we were able to look at ozone changes during 27 00:01:47.640 --> 00:01:51.830 a period of time. in the winter. when most of that ozone change 28 00:01:51.830 --> 00:01:56.010 is coming just from chemical changes. so that temperatures aren't really affecting it very much. 29 00:01:56.010 --> 00:02:00.050 And we're able to do this because of measurements from the NASA Aura 30 00:02:00.050 --> 00:02:04.170 instrument called the Microwave Limb Sounder. so what we've seen by using the MLS 31 00:02:04.170 --> 00:02:08.330 data is that ozone depletion has declined. 32 00:02:08.330 --> 00:02:12.510 It does vary a lot still. but it declines and it's declining 33 00:02:12.510 --> 00:02:16.690 sort of in step with the chlorine changes. and so that's what we're 34 00:02:16.690 --> 00:02:20.880 excited about. is that we see. for the first time. chlorine levels are definitely 35 00:02:20.880 --> 00:02:24.930 going down. and ozone levels are responding to it. 36 00:02:24.930 --> 00:02:28.367