WEBVTT FILE 1 00:00:01.070 --> 00:00:05.070 [rhythmic music] 2 00:00:05.070 --> 00:00:09.000 Kriebel: High tide flooding is the leading edge of the sea level rise problem. 3 00:00:09.000 --> 00:00:13.070 Grieco: We've been following the data for decades. 4 00:00:13.070 --> 00:00:17.070 Going back 50 years, we experienced a flooding like that 5 00:00:17.070 --> 00:00:21.070 maybe four times a year where a roadway would be totally flooded 6 00:00:21.070 --> 00:00:25.070 and impassable. Most recently in 2018, 7 00:00:25.070 --> 00:00:29.070 we had 52 days of flooding. And so the frequency 8 00:00:29.070 --> 00:00:33.000 is increasing and the severity, the depth of the water is increasing as well. 9 00:00:33.000 --> 00:00:37.070 Hamlington: Over the past decade or so, we've seen very high rates 10 00:00:37.070 --> 00:00:41.070 of sea level rise along all the coasts of the US, so the US West coast, 11 00:00:41.070 --> 00:00:45.070 the Gulf coast, and also the East coast. 12 00:00:45.070 --> 00:00:49.070 And if you look at a global map of the ocean and the satellite altimeter measured sea level trends, 13 00:00:49.070 --> 00:00:53.070 the US really stands out as this hot spot 14 00:00:53.070 --> 00:00:57.000 with all coastlines going up very rapidly. 15 00:00:57.000 --> 00:01:01.070 Sweet: You know, it’s causing disruption in people's lives. Patience is starting to be lost in some of these communities 16 00:01:01.070 --> 00:01:05.070 and it's, it's a struggle, but it's not just a local problem. 17 00:01:05.070 --> 00:01:09.070 It's really a national problem as we want to deal with the increased 18 00:01:09.070 --> 00:01:13.070 risk of coastal flooding due to sea level rise now, 19 00:01:13.070 --> 00:01:17.000 and as we move into the future. 20 00:01:17.000 --> 00:01:21.000 [music builds and fades] 21 00:01:21.000 --> 00:01:25.070 Hamlington: As sea level continues to increase, 22 00:01:25.070 --> 00:01:29.000 as ice melts, the ocean expands due to global warming, 23 00:01:29.000 --> 00:01:33.070 we're going to continue to see these effects increase. 24 00:01:33.070 --> 00:01:37.070 You're going to get more frequent and worse high tide flooding in a lot of locations. And locations that aren't experiencing 25 00:01:37.070 --> 00:01:41.070 high tide flooding now, 10, 20, 30 years from now, 26 00:01:41.070 --> 00:01:45.000 they will be experiencing high tide flooding on a pretty regular basis. 27 00:01:45.000 --> 00:01:49.070 And on top of that, minor meteorological events. So a slightly lowered And on top of that, minor meteorological events. So a slightly 28 00:01:49.070 --> 00:01:53.070 lowered atmospheric pressure, on-shore winds that might in our case, 29 00:01:53.070 --> 00:01:57.070 push up the Chesapeake Bay or push in the Severn River. Any of those factors 30 00:01:57.070 --> 00:02:01.070 can cause a little bit of an additional rise in water level 31 00:02:01.070 --> 00:02:05.000 on top of the astronomical tides. 32 00:02:05.000 --> 00:02:09.070 Sweet: And we're not talking about extreme winds. We're talking about the kind of winds that we like when we go sailing. 33 00:02:09.070 --> 00:02:13.070 15. 20 knot winds. But it's that kind of variability 34 00:02:13.070 --> 00:02:17.000 that is causing flooding to happen at record breaking instances. 35 00:02:17.000 --> 00:02:21.070 Hamlington: So we have seasonal cycles that occur. 36 00:02:21.070 --> 00:02:25.070 So over the course of a year, you're going to have a time of the year where sea level is higher than others. 37 00:02:25.070 --> 00:02:29.070 You have a, what we call inter-annual to decadal variability. 38 00:02:29.070 --> 00:02:33.070 So El Niño would be example of this. So when you have an El Niño that occurs, 39 00:02:33.070 --> 00:02:37.070 you have a higher sea level than normal on the US West coast. 40 00:02:37.070 --> 00:02:41.070 Then on even longer time scales than that we have melting of ice, we have thermal expansion 41 00:02:41.070 --> 00:02:45.000 due to global warming that's causing long-term sea level rise. 42 00:02:45.000 --> 00:02:49.000 Sweet: The other part is, what’s land doing? 43 00:02:49.000 --> 00:02:53.070 On the East coast and Gulf coast, we have a land subsidence issue. 44 00:02:53.070 --> 00:02:57.000 Some of that’s natural. Compaction of sediments 45 00:02:57.000 --> 00:03:01.070 in the Mississippi Delta, you know, glacial isostatic adjustment that’s occurring. 46 00:03:01.070 --> 00:03:05.070 But there's a part that's unnatural. It's extraction of fresh water for drinking 47 00:03:05.070 --> 00:03:09.070 and fossil fuels for consumption. That component 48 00:03:09.070 --> 00:03:13.070 can exacerbate relative sea level rise, almost on the same order of magnitude 49 00:03:13.070 --> 00:03:17.000 that the ocean is rising itself. 50 00:03:17.000 --> 00:03:21.000 [gentle wave sounds] 51 00:03:21.000 --> 00:03:25.000 Hamlington: Yeah, so a lot of times we talk about coastal flooding 52 00:03:25.000 --> 00:03:29.070 and sea level rise as a future problem. So you see projections out to the end of the century, 53 00:03:29.070 --> 00:03:33.070 but in reality, sea level rise and coastal flooding is a problem that we're experiencing now. 54 00:03:33.070 --> 00:03:37.000 55 00:03:37.000 --> 00:03:41.070 Kriebel: Right where we’re at right now is a road that flooded 41 times 56 00:03:41.070 --> 00:03:45.070 times last year. And you can see 57 00:03:45.070 --> 00:03:49.070 how the road is so much lower than the top of the sea wall. 58 00:03:49.070 --> 00:03:53.070 The storm drains are really the problem that the water can come up freely from 59 00:03:53.070 --> 00:03:57.000 from the Severn River and just backflow right through the storm drains. 60 00:03:57.000 --> 00:04:01.070 Grieco: And when the tides rise to a certain elevation, 61 00:04:01.070 --> 00:04:05.070 the water backs up through the storm drain system and comes out through 62 00:04:05.070 --> 00:04:09.070 the storm drains in parking lots, for example. 63 00:04:09.070 --> 00:04:13.070 One particular intersection that floods is a main arterial to the downtown area. 64 00:04:13.070 --> 00:04:17.070 And so it gets completely closed. And so, first responders are impacted. 65 00:04:17.070 --> 00:04:21.070 When the parking lot's flooded, then their clients can’t park there, 66 00:04:21.070 --> 00:04:25.070 or they tend not to even come downtown 67 00:04:25.070 --> 00:04:29.070 when these days are reported. It's been documented there’s impacts to their revenues 68 00:04:29.070 --> 00:04:33.000 upwards of $200,000 a year just due to tidal flooding. 69 00:04:33.000 --> 00:04:37.070 Kriebel: I guess you could say it’s sort of a battle between land elevation and water elevation. 70 00:04:37.070 --> 00:04:41.070 It's what I've been calling the game of inches. 71 00:04:41.070 --> 00:04:45.000 Of all the hundreds of high tides a year, some are just a few inches higher than others. 72 00:04:45.000 --> 00:04:49.070 And those are the ones of course that are causing flooding now. 73 00:04:49.070 --> 00:04:53.070 The real problem though, is all the high tide events that are just a few inches below, 74 00:04:53.070 --> 00:04:57.000 it's only gonna take a few inches of additional sea level rise 75 00:04:57.000 --> 00:05:01.070 to nudge them upward. So what will happen over time 76 00:05:01.070 --> 00:05:05.000 is with sea level rise … we're going to end up not with 20 or 40 flood events, 77 00:05:05.000 --> 00:05:09.000 but we'll then be into hundreds of flood events per year. 78 00:05:09.000 --> 00:05:13.000 [music fades and rebuilds] 79 00:05:13.000 --> 00:05:17.070 Sweet: One of the things that communities are doing 80 00:05:17.070 --> 00:05:21.070 is they’re preventing water from coming back through the stormwater systems. 81 00:05:21.070 --> 00:05:25.000 They’re called backflow preventers. You want to let rain out, 82 00:05:25.000 --> 00:05:29.000 but you don’t want to let the ocean in. 83 00:05:29.000 --> 00:05:33.070 Kriebel: Some places like Charleston are putting large underground 84 00:05:33.070 --> 00:05:37.070 water storage facilities, deep underground, where they can direct rainwater and get it off the city streets 85 00:05:37.070 --> 00:05:41.070 and try to hold it there until after you know the rainstorm goes. 86 00:05:41.070 --> 00:05:45.070 If you have low lying areas, you may need pump stations 87 00:05:45.070 --> 00:05:49.000 to collect rain water and pump it. 88 00:05:49.000 --> 00:05:53.000 Hamlington: But then there's these other strategies where coastal communities are trying to reduce 89 00:05:53.000 --> 00:05:57.000 the amount of pavement they have for instance, increase the amount of green space they have 90 00:05:57.000 --> 00:06:01.070 in these different locations, restoring beach front. A lot of these 91 00:06:01.070 --> 00:06:05.000 different things can reduce the impact of coastal flooding going forward. 92 00:06:05.000 --> 00:06:09.070 So NASA has the observations 93 00:06:09.070 --> 00:06:13.070 that are really needed to improve our understanding of 94 00:06:13.070 --> 00:06:17.070 sea level science. So across the board, 95 00:06:17.070 --> 00:06:21.070 we have processes that are contributing to sea level change on a range of timescales 96 00:06:21.070 --> 00:06:25.070 and the variety of satellite observations that we have available to us now 97 00:06:25.070 --> 00:06:29.000 really allow us to improve our understanding of these different processes. 98 00:06:29.000 --> 00:06:33.070 Sweet: What we're doing at NOAA is really trying to give the 99 00:06:33.070 --> 00:06:37.000 data to decision makers so that they can make informed decisions 100 00:06:37.000 --> 00:06:41.070 that's best for their community. But one thing's for certain, 101 00:06:41.070 --> 00:06:45.070 is under current flood defenses, these projections suggest that a floodier future 102 00:06:45.070 --> 00:06:49.070 is going to be here in the next few decades 103 00:06:49.070 --> 00:06:53.070 and the way of life is going to have to adapt to this. 104 00:06:53.070 --> 00:06:57.301 [music fades]