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.