WEBVTT FILE 1 00:00:00.200 --> 00:00:03.103 NASA funded researchers have linked unexplained pockets of 2 00:00:03.103 --> 00:00:06.807 ozone over the Western Pacific Ocean to fires thousands of 3 00:00:06.807 --> 00:00:11.378 miles away. The findings are from a 2014 field campaign over 4 00:00:11.378 --> 00:00:15.449 the remote island of Guam. Scientists took to the air 5 00:00:15.449 --> 00:00:18.552 aboard flying laboratories filled with instruments to study 6 00:00:18.552 --> 00:00:22.089 the chemistry of the atmosphere. Measurements taken along flight 7 00:00:22.089 --> 00:00:26.593 paths up to 30,000 feet revealed areas with levels of ozone that 8 00:00:26.593 --> 00:00:29.796 were three times higher than normal. So while 9 00:00:29.796 --> 00:00:33.500 ozone is an important shield against ultraviolet radiation in 10 00:00:33.500 --> 00:00:36.103 the upper atmosphere, in the lower atmosphere it is a very 11 00:00:36.103 --> 00:00:39.606 strong greenhouse gas. So what we were trying to explore, is 12 00:00:39.606 --> 00:00:43.277 what was causing these very high levels of ozone in the Pacific. 13 00:00:43.277 --> 00:00:46.146 The answer came from two chemicals found with the ozone 14 00:00:46.146 --> 00:00:49.349 linked to forest fires and the burning of vegetation. As these 15 00:00:49.349 --> 00:00:53.153 fires burn, a mix of organic compounds and gases that react 16 00:00:53.153 --> 00:00:56.924 to form ozone are released into the atmosphere.  They’re then 17 00:00:56.924 --> 00:01:00.127 transported by winds, sometimes thousands of miles from their 18 00:01:00.127 --> 00:01:03.096 source. Using a computer model, we traced the 19 00:01:03.096 --> 00:01:05.899 winds back in time to their origins so we could figure out 20 00:01:05.899 --> 00:01:09.303 the source of these chemicals. What the model and satellite 21 00:01:09.303 --> 00:01:12.472 data showed, is that these chemicals were coming from fires 22 00:01:12.472 --> 00:01:16.076 in Africa and Southeast Asia. The red and orange lines in this 23 00:01:16.076 --> 00:01:19.479 visualization trace the path of high concentrations of 24 00:01:19.479 --> 00:01:22.816 ozone-filled air detected in the Western Pacific to their source. 25 00:01:22.816 --> 00:01:26.853 The air could be traced back ten to fifteen days to fires in 26 00:01:26.853 --> 00:01:30.657 Southeast Asia and tropical Africa. In one of the remotest 27 00:01:30.657 --> 00:01:34.227 parts of the Northern Hemisphere, we’re seeing impacts 28 00:01:34.227 --> 00:01:37.698 from fires that are happening half a world away. So what I 29 00:01:37.698 --> 00:01:40.200 think is important about this study, is that it helps us 30 00:01:40.200 --> 00:01:44.738 connect these fires in Africa and Southeast Asia to processes 31 00:01:44.738 --> 00:01:46.540 that are happening across the globe.