WEBVTT FILE 1 00:00:04.380 --> 00:00:09.180 A mangrove forest is a forest made out of trees that grow in 2 00:00:09.180 --> 00:00:11.820 areas where land meets sea. 3 00:00:12.120 --> 00:00:18.240 So these are essentially wetland forests that are only present in 4 00:00:18.270 --> 00:00:23.880 tropical or subtropical regions worldwide. My name is Dr. Lola 5 00:00:23.880 --> 00:00:27.450 Fatoyinbo, and I'm a Research Scientist in the Biospheric 6 00:00:27.450 --> 00:00:28.440 Sciences Lab. 7 00:00:30.390 --> 00:00:33.120 Mangroves are important for a whole number of reasons. They 8 00:00:33.120 --> 00:00:37.350 provide what we call ecosystem services to humans. And some of 9 00:00:37.350 --> 00:00:41.910 those services that they provide are storm surge protections, the 10 00:00:41.910 --> 00:00:46.830 protection from waves and erosion of the coast. They're 11 00:00:46.830 --> 00:00:52.110 also really important for water filtration and for protection of 12 00:00:52.110 --> 00:00:52.830 the coastline. 13 00:00:54.850 --> 00:01:01.180 So in 2017, when Hurricane Irma hit southern Florida, we were 14 00:01:01.180 --> 00:01:05.830 really interested in getting a better idea of how resilient 15 00:01:05.860 --> 00:01:10.390 mangrove forests would be to increasing storm impacts that we 16 00:01:10.390 --> 00:01:14.890 were expecting with changes in climate. We worked with an 17 00:01:14.890 --> 00:01:18.520 airborne instrument suite called G-LiHT. This is the Goddard 18 00:01:18.520 --> 00:01:23.260 LIDAR hyperspectral Thermal instrument, which is a small pod 19 00:01:23.260 --> 00:01:27.550 that has multiple instruments set up together that you can 20 00:01:27.940 --> 00:01:32.590 essentially attached to an airplane. What we found was that 21 00:01:32.590 --> 00:01:35.560 actually, the main cause of permanent die off in mangrove 22 00:01:35.560 --> 00:01:39.850 forests is when you have these really high storm surge that 23 00:01:39.850 --> 00:01:45.340 come in to areas and result in ponding of water in these basin 24 00:01:45.340 --> 00:01:49.990 mangrove areas. So essentially, areas where salt water becomes 25 00:01:49.990 --> 00:01:53.290 stagnant. And when that water becomes stagnant, it gets a 26 00:01:53.290 --> 00:01:57.280 really high concentration of nutrients and the salt, leading 27 00:01:57.280 --> 00:02:01.780 to a permanent die off of these mangrove areas, which is in some 28 00:02:01.780 --> 00:02:05.230 ways becoming a vicious cycle. Because in those areas, because 29 00:02:05.230 --> 00:02:08.710 they're basins, you're not able to grow new mangroves that are 30 00:02:08.710 --> 00:02:12.550 then accumulating more soil. And so you end up with mangroves 31 00:02:12.550 --> 00:02:16.480 dying, the peat collapsing and that peak collapse, not allowing 32 00:02:16.480 --> 00:02:21.940 for new mangroves to come in and resulting in permanent dieoff. 33 00:02:21.940 --> 00:02:25.120 o I think the greatest takeaw y from this study is that ev 34 00:02:25.120 --> 00:02:27.190 n though mangroves are oft n thought of as being real 35 00:02:27.190 --> 00:02:31.330 y resilient and resistant to har h conditions, they are sti 36 00:02:31.330 --> 00:02:34.510 l really vulnerable. And we ne d to make sure that we're able 37 00:02:34.690 --> 00:02:38.350 o maintain the natural conditio s and hydrology that they grow a 38 00:02:38.590 --> 00:02:42.220 d for them to continue to prote t us from these extre 39 00:02:42.220 --> 00:02:42.940 e condition