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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
