WEBVTT FILE 1 00:00:00.020 --> 00:00:04.140 I actually started off in fundamental particle physics, so working at 2 00:00:04.140 --> 00:00:08.270 CERN in Geneva, and 3 00:00:08.270 --> 00:00:12.480 that was really exciting, I loved the research environment, I loved the work, but 4 00:00:12.480 --> 00:00:16.690 most people who work there are really kind of motivated by these very abstract 5 00:00:16.690 --> 00:00:20.890 fundamental problems or the beauty of a mathematical equation, and I'm so happy 6 00:00:20.890 --> 00:00:25.090 people like that exist, but it's not me. I'm more excited by 7 00:00:25.090 --> 00:00:29.320 tangible problems, things that we can relate to society, to human needs and problems 8 00:00:29.320 --> 00:00:33.520 problems and so moving towards the atmosphere, looking at air 9 00:00:33.520 --> 00:00:37.730 quality and climate just made more sense for what I'm personally 10 00:00:37.730 --> 00:00:41.990 motivated by. I'm measuring the number and size of aerosol particles. 11 00:00:41.990 --> 00:00:46.180 Aerosols are any small solid or liquid drop that's suspended in the air 12 00:00:46.180 --> 00:00:50.420 so in the atmosphere that we fly through. 13 00:00:50.420 --> 00:00:54.520 They can come from multiple different sources, so they could be 14 00:00:54.520 --> 00:00:56.520 desert dust that's blown up into the atmosphere 15 00:00:56.520 --> 00:00:58.770 and the little bits of sand stay there 16 00:00:58.770 --> 00:01:03.140 or it could be sea spray blown up, but you can also get 17 00:01:03.140 --> 00:01:07.330 things like particles forming out of the gas phase to make solid or liquid drops 18 00:01:07.330 --> 00:01:11.420 in situ in the atmosphere. And those are the really small ones, we're quite interested in measuring those. 19 00:01:11.420 --> 00:01:15.630 The reason we care about aerosols in the atmosphere is 20 00:01:15.630 --> 00:01:19.820 they're affecting climate, they're affecting the radiative budget, and even though they're quite 21 00:01:19.820 --> 00:01:24.030 a small effect in there when you compare it to things like greenhouse gases, they're one of the less 22 00:01:24.030 --> 00:01:28.390 well-understood ones, and so the better we can start understanding these aerosols, 23 00:01:28.390 --> 00:01:32.600 where they are, how they move around the atmosphere, how they're transformed 24 00:01:32.600 --> 00:01:36.780 the smaller the uncertainties we have on our climate predictions. 25 00:01:36.780 --> 00:01:40.810 Also aerosols are really important for human health and so we want to be able to 26 00:01:40.810 --> 00:01:44.890 predict where we've got high concentrations of them, what they're made of 27 00:01:44.890 --> 00:01:49.000 and all of the things that might be impacting health, and so it's really interesting for us 28 00:01:49.000 --> 00:01:53.230 to measure them, especially this whole sort of global pattern that we can capture on ATom. 29 00:01:53.230 --> 00:01:57.410 And really see where that's happening and potentially why it's happening. Where the 30 00:01:57.410 --> 00:02:01.600 window would normally be on a plane we have like a metal window plate, and on that, we have a custom inlet 31 00:02:01.600 --> 00:02:05.670 that brings in air without losing or changing the particles that are present in it. 32 00:02:05.670 --> 00:02:09.870 And then this goes through a system of different tubes to bring it to all of the different instruments 33 00:02:09.870 --> 00:02:14.000 in our suite. And we need multiple instruments because aerosols can range 34 00:02:14.000 --> 00:02:18.200 hugely in size from just a huge nanometers in size 35 00:02:18.200 --> 00:02:22.390 right up to many microns, and so you have use different techniques to meaure them 36 00:02:22.390 --> 00:02:38.000 in different sizes.