WEBVTT FILE 1 00:00:00.130 --> 00:00:04.200 Narrator: There’s a new class of chemical compounds 2 00:00:04.220 --> 00:00:08.310 impacting the Earth's ozone layer and raising concerns among some scientists, 3 00:00:08.330 --> 00:00:12.520 but a new NASA analysis indicates 4 00:00:12.540 --> 00:00:16.610 stratospheric ozone could actually be impacted more by 5 00:00:16.630 --> 00:00:20.680 climate change and the continued release of already-banned chemicals. 6 00:00:20.700 --> 00:00:24.810 The Earth’s ozone hole is showing signs of recovery, 7 00:00:24.830 --> 00:00:28.970 decades after the landmark agreement called the Montreal Protocol 8 00:00:28.990 --> 00:00:33.150 that banned many chemical compounds harmful to the ozone layer. 9 00:00:33.170 --> 00:00:37.390 Liang: So we know the Montreal Protocol was a huge success. 10 00:00:37.410 --> 00:00:41.600 This was signed in the late 1980s when scientists and policy makers 11 00:00:41.620 --> 00:00:45.810 from around the world gathered together to try to save the ozone layer. 12 00:00:45.830 --> 00:00:49.930 Strahan: The chemicals they regulated persist in the atmosphere 13 00:00:49.950 --> 00:00:54.120 for many decades, they thinned the ozone layer and created a seasonal hole over Antarctica. 14 00:00:54.140 --> 00:00:58.330 They basically take away part of our planet’s natural sunscreen, 15 00:00:58.350 --> 00:01:02.390 and that increases the risk of skin cancer and damage to plants. 16 00:01:02.410 --> 00:01:06.460 Narrator:Scientists have projected the ozone hole could disappear almost completely 17 00:01:06.480 --> 00:01:10.540 by about 2075, but several factors could delay that recovery. 18 00:01:10.560 --> 00:01:14.750 Liang: There are some industrial compounds that were not banned 19 00:01:14.770 --> 00:01:18.880 by the Montreal Protocol, but as they enter the atmosphere, they will also 20 00:01:18.900 --> 00:01:22.970 hurt the ozone layer. 21 00:01:22.990 --> 00:01:27.110 Strahan: But the unregulated compounds have a short lifespan in the atmosphere 22 00:01:27.130 --> 00:01:31.220 than the chlorofluorocarbons that were originally banned, so they have a short-lived impact on ozone, 23 00:01:31.240 --> 00:01:35.310 and we don’t think they’ll delay recovery by more than a few years. 24 00:01:35.330 --> 00:01:39.560 Liang: We projected by 2050 more than 25 00:01:39.580 --> 00:01:43.770 half of ozone-destroying compounds in the atmosphere will come from 26 00:01:43.790 --> 00:01:47.990 long-lived substances banned by the Protocol. 27 00:01:48.010 --> 00:01:52.130 Narrator:Because these compounds stay in the air for such a long time compared to the 28 00:01:52.150 --> 00:01:56.190 unregulated short-lived compounds, they will have a disproportionate and lingering 29 00:01:56.210 --> 00:02:00.390 impact on ozone, so any non-compliance with the Protocol 30 00:02:00.410 --> 00:02:04.570 can have significant consequences. 31 00:02:04.590 --> 00:02:08.660 Strahan: And the really big uncertainty in ozone-layer recovery is climate change. 32 00:02:08.680 --> 00:02:12.900 There are many naturally produced ozone-depleting substances that are emitted by the oceans, 33 00:02:12.920 --> 00:02:17.150 and as the oceans continue to warm due to climate change, 34 00:02:17.170 --> 00:02:21.360 those emissions will increase, and that will further delay ozone recovery. 35 00:02:21.380 --> 00:02:25.560 Narrator:Scientists want to better understand how climate change will affect ozone recovery. 36 00:02:25.580 --> 00:02:29.680 Liang: This is a hard problem. 37 00:02:29.700 --> 00:02:33.840 As a scientific community we need to work on this major issue. 38 00:02:33.860 --> 00:02:38.040 We now have a powerful new tool to simulate atmosphere and its interaction 39 00:02:38.060 --> 00:02:42.220 with land and ocean, to study this issue. And that’s what we’re going to do. 40 00:02:42.240 --> 00:02:49.680 [beep beep, beep beep, beep beep]