Latest / DEEP INSIGHT / Two lakes threaten Nepal after deadly flood in 'hazard-prone' region
Transcript
- 0:00Speaker 1: What is already a dangerous race to locate survivors has
- 0:03Speaker 1: been further complicated by the risk of additional possible flash
- 0:07Speaker 1: flooding and landslides. Operations were briefly paused this morning when
- 0:10Speaker 1: a newly formed barrier lake began to overflow, and now
- 0:14Speaker 1: a second lake has been observed in aerial footage of
- 0:17Speaker 1: the flood zone. I want to go to CNN's Tom
- 0:20Speaker 1: Foreman at the Magic Wall to help explain what we're
- 0:22Speaker 1: seeing here. Tom, talk to us about the formation of
- 0:25Speaker 1: these lakes so high up in the mountains.
- 0:27Speaker 2: Yeah, it is a real challenge here. Let's put ourselves
- 0:29Speaker 2: into the map first. India down here, Nepal right through here,
- 0:32Speaker 2: China up here, Mount Everest over this way, just in
- 0:35Speaker 2: case you're wondering. This is where this is all happening.
- 0:37Speaker 2: If we move in to take a look at the
- 0:39Speaker 2: area where that glacier collapsed yesterday, happened that you were
- 0:42Speaker 2: talking about a short while ago. That's right over here.
- 0:45Speaker 2: That gave way, sending all sorts of debris and mud
- 0:49Speaker 2: and water rocketing down into this river valley here, more
- 0:53Speaker 2: than 100 miles an hour and creating all that havoc.
- 0:56Speaker 2: You want to see how much is involved there? All
- 0:58Speaker 2: you have to do is go over here and look
- 1:00Speaker 2: at this. We'll slide it over and you can see
- 1:03Speaker 2: the damage. The before, this is the after. And in
- 1:06Speaker 2: this after, John, that is where you can see the
- 1:09Speaker 2: very thing we're talking about now. A lake that has
- 1:12Speaker 2: formed right there and a lake that has formed right here.
- 1:17Speaker 2: Because as more water flows down and the debris is
- 1:21Speaker 2: blocking its progress, those lakes have been building up there.
- 1:25Speaker 2: And that is really the worry. The worry is that
- 1:28Speaker 2: if all of the material blocking those lakes right now
- 1:32Speaker 2: gives way, if that somehow breaks through in a catastrophic way,
- 1:37Speaker 2: you could send another sort of pulse of, A liquid
- 1:41Speaker 2: shockwave right through the area that the rescue and recovery
- 1:45Speaker 2: is being operated right now, John.
- 1:47Speaker 1: So what, if anything, can be done to alleviate the
- 1:50Speaker 1: risk of those lakes just bursting?
- 1:52Speaker 2: Well, one of the ideas would be, first of all,
- 1:54Speaker 2: you monitor them to see if maybe they're draining at
- 1:56Speaker 2: a slower rate. Maybe that helps off. Maybe they're a
- 1:59Speaker 2: natural thing. Maybe not as much rain things that would
- 2:01Speaker 2: help out a little bit. I suppose in severe cases,
- 2:04Speaker 2: they might see if there were some way to drain
- 2:06Speaker 2: it off. But right now, what they're mainly doing is
- 2:09Speaker 2: talking about trying to get some cameras and more sensors
- 2:11Speaker 2: in place to see what's going to happen and telling
- 2:14Speaker 2: the workers down below what they're telling them right now.
- 2:17Speaker 2: You have to be ready, even amid all this dismal
- 2:21Speaker 2: and dangerous work, you have to be ready to run
- 2:24Speaker 2: for higher ground at a moment's notice if one of
- 2:27Speaker 2: these lakes burst free.
- 2:29Speaker 3: What happened, we think, is that some of the bedrock
- 2:33Speaker 3: high in the mountain just below the summit of Langtang,
- 2:38Speaker 3: Lirung Peak, failed. It was fractured and it collapsed. And
- 2:46Speaker 3: there was a small glacier resting on top. There still
- 2:50Speaker 3: is part of the glacier remaining there. And that piece
- 2:54Speaker 3: of the glacier collapsed with the bedrock. And then on
- 2:57Speaker 3: the way down, Just the frictional energy, we call it
- 3:03Speaker 3: gravitational potential energy, turning into heat, which melted the ice.
- 3:08Speaker 3: And so it was almost entirely melted by the time
- 3:12Speaker 3: it reached the first really damaging point at the China-Nepal border.
- 3:21Speaker 3: And so just horrific. I've never seen anything like this.
- 3:27Speaker 3: in my career to date in terms of Himalayan hazards
- 3:33Speaker 3: and disasters.
- 3:35Speaker 1: And Dan, picking up on that point, you point out
- 3:37Speaker 1: this is one of the most hazard prone landscapes on
- 3:41Speaker 1: the planet. I mean, how much ice are these glaciers
- 3:44Speaker 1: losing every year?
- 3:47Speaker 4: Absolutely. This is a major plate boundary. We have two
- 3:51Speaker 4: continental plates crashing into each other over the last 50
- 3:54Speaker 4: million years, building the highest mountains on Earth. This has
- 3:57Speaker 4: produced incredibly steep slopes and a tremendous amount of elevational
- 4:02Speaker 4: relief from the valley bottoms to the tops.
- 4:04Speaker 3: Of these mountains.
- 4:06Speaker 4: And there's a very large number of glaciers across high
- 4:09Speaker 4: mountain Asia, something on the order of about 95,000. And cumulatively,
- 4:13Speaker 4: that area is about the area of South Korea. And
- 4:17Speaker 4: these glaciers are losing mass very rapidly. If we take
- 4:21Speaker 4: the amount of mass that's being lost every single year
- 4:23Speaker 4: from these glaciers and that meltwater and put it onto
- 4:26Speaker 4: the island of Manhattan, it would inundate the island to
- 4:30Speaker 4: over 1,200 feet. So we're looking at the top of
- 4:33Speaker 4: the Empire State Building submerged in water every single year
- 4:37Speaker 4: from glaciers across this region. Wow.
- 4:40Speaker 2: And we call it water, right?
- 4:42Speaker 1: We turn into liquid there, Jeff, but we've heard one
- 4:45Speaker 1: scientist describe it as, as liquid concrete. This isn't, you know,
- 4:49Speaker 1: like water that comes out of your faucet here. It's
- 4:51Speaker 1: just this incredible destructive mass and impossible to outrun. You
- 4:55Speaker 1: said it was like the equivalent of at least 500,000
- 4:59Speaker 1: large dump truck loads of rock and ice at minimum.
- 5:02Speaker 1: Talk to me about that, Jeff.
- 5:05Speaker 3: Yeah, I think that is a minimum. In fact, um,
- 5:09Speaker 3: the amount of mass that detached from the mountain top
- 5:15Speaker 3: might not be all the mass of the flow that
- 5:19Speaker 3: did all this destruction, because as it flowed down, it
- 5:22Speaker 3: picked up more rock debris, and once it reached the
- 5:26Speaker 3: Boticosi River, there was additional water that it could pick up.
- 5:30Speaker 3: And so the final mass of this was even more
- 5:35Speaker 3: than what detached from the mountain, But there is a question,
- 5:43Speaker 3: have we identified all the entire source of water in
- 5:49Speaker 3: this event?
- 5:52Speaker 1: It really is interesting. There's still so many questions. with
- 5:55Speaker 1: something that in some ways is so photographed. We've seen
- 5:58Speaker 1: so much video of the destruction, but we really still
- 6:01Speaker 1: don't have perfect eyes on what happened at the very beginning.
- 6:05Speaker 1: You know, Dan, what would it have taken, if anything,
- 6:09Speaker 1: to have seen this exact disaster coming?
- 6:14Speaker 4: It's a very difficult thing to predict. In this region,
- 6:18Speaker 4: we've seen a large number of glacial lakes form and
- 6:22Speaker 4: grow through time, and these are actively monitored, and the
- 6:25Speaker 4: most hazardous of these have been identified. But this is
- 6:28Speaker 4: a totally different hazard. This is not something, you know,
- 6:31Speaker 4: when we think about the 95,000 glaciers across the region,
- 6:35Speaker 4: we can't go out and monitor every single one of
- 6:37Speaker 4: those with time-lapse cameras or other radar systems. And so
- 6:40Speaker 4: this is a real challenge. And historical, you know, early
- 6:44Speaker 4: warning systems where we might have a stream gauge on
- 6:47Speaker 4: a bridge to give warning are not capable of providing
- 6:52Speaker 4: sufficient warning. Those bridges were completely washed out during this event.
- 6:57Speaker 1: And Jeff, how dangerous are these ongoing rescue efforts? I mean,
- 7:00Speaker 1: they did pause them for a time this morning, you know,
- 7:04Speaker 1: given the composition of debris and the possibility of the
- 7:08Speaker 1: lakes bursting. How dangerous would you say it is?
- 7:14Speaker 3: John, you just showed some information that I wasn't aware
- 7:20Speaker 3: of until this show. That is the lake forming high
- 7:25Speaker 3: up in the mountain. This is extremely concerning because we
- 7:32Speaker 3: already know that water perched up there would be an
- 7:35Speaker 3: unstable mass. And, you know, there may have been some
- 7:40Speaker 3: additional water that was unseen sort of hiding up there
- 7:47Speaker 3: in the glacier, maybe not on the surface. And now
- 7:52Speaker 3: we see a surface lake. You've got it highlighted in
- 7:56Speaker 3: your box there. And this is very worrisome, even more
- 8:02Speaker 3: so than the landslide dammed. lake because this is perched
- 8:09Speaker 3: high up and it could burst forth and flow into
- 8:14Speaker 3: that landslide dammed lake and together they could burst out
- 8:18Speaker 3: very very rapidly I do not want to be alarmist
- 8:23Speaker 3: here but the alarm bells are ringing and the rescue
- 8:28Speaker 3: crews have to be ready like you said to move
- 8:32Speaker 3: to higher ground at every moment they have to be
- 8:35Speaker 3: thinking like if something happens, where exactly am I going
- 8:41Speaker 3: to ascend the slope? Because running alongside the road ahead
- 8:49Speaker 3: of the flood isn't going to do it. We just
- 8:52Speaker 3: saw a video, you showed a video showing some people
- 8:56Speaker 3: running along the road, and I don't know the details
- 9:00Speaker 3: of that particular location, but In general, that's not the
- 9:04Speaker 3: thing to do. You have to get to higher ground,
- 9:07Speaker 3: not just a higher building.
- 9:10Speaker 1: This does not seem to be the type of disaster
- 9:12Speaker 1: you can outrun. Jeffrey Cargill, Daniel McGrath, thank you so
- 9:14Speaker 1: much for helping us understand some of the science behind this.