WEBVTT
Kind: captions
Language: en

1
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I'm about to step onto brand new land.

2
00:00:14.400 --> 00:00:17.480
And admittedly, yes, it is a
little bit underwater right now

3
00:00:17.490 --> 00:00:20.480
because, well, that
river there is in flood.

4
00:00:20.480 --> 00:00:24.080
But 50 years ago, this
would've been open water

5
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and I would've been jumping
off this boat up to my neck.

6
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And yes, I was extremely nervous

7
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about that little jump [laughs]

8
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'cause that's the first
time I came off here.

9
00:00:35.630 --> 00:00:37.940
But yeah, this is the Wax Lake Delta.

10
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50 years ago: no trees, no plants,
nowhere to put your feet,

11
00:00:41.820 --> 00:00:45.250
I would've been swimming,
on a coastline that's famous

12
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not for building up but for eroding.

13
00:00:47.170 --> 00:00:50.763
And to explain why, we have to
go just a little bit inland.

14
00:00:52.960 --> 00:00:55.920
The Mississippi River
is so murky and brown

15
00:00:55.920 --> 00:00:58.040
because it's filled
with silt and sediment.

16
00:00:58.040 --> 00:01:00.640
Throughout history, roughly
every thousand years or so,

17
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deposits of that sediment build up enough

18
00:01:02.850 --> 00:01:05.310
that the river basically blocks itself

19
00:01:05.310 --> 00:01:08.230
and then takes a different and
steeper route to the ocean,

20
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at least until silt builds up
on that new route

21
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and the river moves again.

22
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That massive and relatively sudden change

23
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is called an avulsion.

24
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And avulsions were fine
until modern times,

25
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when the industry that you can hear

26
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and the livelihoods of
untold numbers of people

27
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rely on the river being
exactly where it is.

28
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But in the past, every time that humans

29
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have tried to fix the rivers around here,

30
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there have been unintended consequences.

31
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We built levees like this one

32
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to protect towns like Baton Rouge here,

33
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but they make the river
flow faster and higher

34
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because all the water is now
concentrated into one channel.

35
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And because they restrict water flow,
they move the flooding upstream,

36
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which means the next neighbourhood over

37
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has to build their levee
higher to deal with it.

38
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There are regulations
to prevent 'levee wars',

39
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when communities have to keep
building their levees higher

40
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because their neighbours
are doing the same.

41
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Those regulations aren't always followed.

42
00:01:58.240 --> 00:02:02.060
And downstream, levees mean that
instead of a wider river during floods,

43
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you get a faster river, eroding away those
silt and sediment deposits,

44
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literally washing away the
land that it once created.

45
00:02:09.790 --> 00:02:11.480
And now, the river doesn't flood as much,

46
00:02:11.480 --> 00:02:15.720
so the ground next to it
dries out and settles and sinks.

47
00:02:15.720 --> 00:02:18.190
Louisiana's coastline is disappearing.

48
00:02:18.190 --> 00:02:22.030
In 2011, government cartographers
retired 35 placenames,

49
00:02:22.030 --> 00:02:23.640
taking them off the maps

50
00:02:23.640 --> 00:02:26.190
because those islands and bays
just don't exist anymore.

51
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They're just open water.

52
00:02:27.230 --> 00:02:31.660
But there is one place on the coastline,
a couple of hours south of Baton Rouge,

53
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where land is appearing again,

54
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and that is also an
unintended consequence,

55
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which brings us back
to where I was standing

56
00:02:38.470 --> 00:02:40.377
at the Wax Lake Delta.

57
00:02:40.377 --> 00:02:44.860
- The Wax Lake Outlet is a
channel off the Atchafalaya River.

58
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The Atchafalaya River is a
channel off the Mississippi.

59
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So, a channel off a channel off
the Mississippi River. [thunder booms]

60
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Excuse me, I heard a little thunder.

61
00:02:52.250 --> 00:02:53.300
- Okay, no, we--
- Let's get out of here.

62
00:03:00.680 --> 00:03:04.860
- The Wax Lake Outlet was
built in the early  1940s

63
00:03:04.870 --> 00:03:08.270
and it was designed to pull water
off the Atchafalaya River

64
00:03:08.270 --> 00:03:10.840
and reduce flood stress on Morgan City.

65
00:03:10.840 --> 00:03:12.860
One of the unintended consequences

66
00:03:12.860 --> 00:03:17.770
was the development of a delta
at the mouth of the Wax Lake Outlet.

67
00:03:17.770 --> 00:03:20.380
And so, the Wax Lake Outlet
and the Atchafalaya River

68
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carries a lot of sediment,

69
00:03:22.060 --> 00:03:25.890
and then when it gets to the coast,
the river flow slows down

70
00:03:25.890 --> 00:03:29.330
and all of the sediment
in the river settles out.

71
00:03:29.330 --> 00:03:33.460
We're talking tens of millions
of metric tonnes of sediment every year.

72
00:03:33.460 --> 00:03:36.120
This is solid enough land
that you can walk on it

73
00:03:36.120 --> 00:03:37.170
and you can stand on it.

74
00:03:37.170 --> 00:03:42.950
Louisiana has lost nearly 2,000 square miles'
worth of land over the last century,

75
00:03:42.950 --> 00:03:45.970
and there's a large effort
to rebuild the coast.

76
00:03:45.970 --> 00:03:49.510
A big part of that effort is
to try to partially divert

77
00:03:49.510 --> 00:03:51.290
the flow of the Mississippi River

78
00:03:51.290 --> 00:03:54.680
to create new deltas that
are like the Wax Lake Delta.

79
00:03:54.680 --> 00:03:57.960
And so, people like myself want
to study the Wax Lake Delta

80
00:03:57.960 --> 00:04:00.040
so we understand how deltas build

81
00:04:00.040 --> 00:04:03.560
so we can better design
coastal restoration projects.

82
00:04:03.560 --> 00:04:05.420
It's important to restore the coast,

83
00:04:05.420 --> 00:04:10.680
one, to push back the sea to
enhance flood protection in Louisiana,

84
00:04:10.680 --> 00:04:13.410
and it's also a place where you could
potentially bury carbon.

85
00:04:13.410 --> 00:04:15.950
We have too much CO2 in the atmosphere,

86
00:04:15.950 --> 00:04:18.550
and highly productive
deltas like the Wax Lake

87
00:04:18.550 --> 00:04:21.470
may be one of those places
where we can do that.

88
00:04:21.470 --> 00:04:24.340
I often feel like the numerical models

89
00:04:24.340 --> 00:04:28.540
that we have to understand the
coast are pretty darn good.

90
00:04:28.540 --> 00:04:32.940
The much more difficult thing to model
is to understand people

91
00:04:32.940 --> 00:04:35.950
and how people are going to behave
with this changing coast.

92
00:04:35.950 --> 00:04:40.720
And I feel like, that, we barely
even know the equations.

93
00:04:40.720 --> 00:04:44.060
We don't necessarily know
even what the rules are

94
00:04:44.060 --> 00:04:49.690
to govern how do people deal with
a stressful changing environment.

95
00:04:49.690 --> 00:04:51.980
- So, yes, it's still wet
underfoot here right now

96
00:04:51.980 --> 00:04:54.320
because this whole area's still in flood.

97
00:04:54.320 --> 00:04:57.930
But that just means there's more mud,
more sediment being deposited.

98
00:04:57.930 --> 00:05:00.250
This land is going to be a
couple of centimetres higher

99
00:05:00.250 --> 00:05:03.163
and this coastline is going
to be just a little bit safer.

100
00:05:05.220 --> 00:05:06.800
I've sunk about an inch into the mud

101
00:05:06.800 --> 00:05:09.860
and it's gone in my shoes.
It's in my shoes.

102
00:05:09.860 --> 00:05:11.687
Right, I should totally
have gone with the sandals.

103
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[laughing]

104
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[grunts] All right.

