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One of the world's largest airships is taking a team of scientists | 0:00:11 | 0:00:16 | |
and explorers on a unique expedition. | 0:00:16 | 0:00:19 | |
A voyage deep into one of the most mysterious and precious | 0:00:22 | 0:00:28 | |
environments on earth. | 0:00:28 | 0:00:30 | |
The atmosphere. | 0:00:35 | 0:00:37 | |
It's in every breath you take. | 0:00:39 | 0:00:41 | |
It is a home to life... | 0:00:43 | 0:00:45 | |
..and it makes the weather. | 0:00:49 | 0:00:51 | |
So, we have this dynamic bubble of air, constantly moving, constantly | 0:00:52 | 0:00:58 | |
changing and that's what we're here with Cloud Lab to explore. | 0:00:58 | 0:01:02 | |
This quest is taking the team coast to coast across America. | 0:01:04 | 0:01:11 | |
So far, they have experienced the powerful weather systems of | 0:01:11 | 0:01:15 | |
the Southern coast. | 0:01:15 | 0:01:16 | |
You can feel the energy in the air around you. | 0:01:17 | 0:01:20 | |
It's absolutely fantastic. | 0:01:20 | 0:01:22 | |
Now, they are heading across a different kind of landscape - | 0:01:24 | 0:01:29 | |
the deserts of the west to the Pacific Ocean, | 0:01:29 | 0:01:33 | |
to explore three key themes. | 0:01:34 | 0:01:37 | |
Oh, wow! | 0:01:37 | 0:01:39 | |
Life - they will investigate the relationship between life and the | 0:01:39 | 0:01:43 | |
layers of the atmosphere right up to the death-zone of high altitude. | 0:01:43 | 0:01:48 | |
We've got every reason to think that there is life up there. | 0:01:49 | 0:01:52 | |
And the more interesting question, I guess, is how much is there | 0:01:52 | 0:01:56 | |
and what's it up to? | 0:01:56 | 0:01:57 | |
Climate - they will experience the surprising way in which the | 0:01:59 | 0:02:03 | |
atmosphere can transform the ocean... | 0:02:03 | 0:02:05 | |
Another giant-sized animal. This whole place is like super-sized. | 0:02:08 | 0:02:13 | |
..and human impact - | 0:02:16 | 0:02:18 | |
the ways in which we, ourselves, are changing the atmosphere. | 0:02:18 | 0:02:24 | |
We've hard evidence that human beings are creating | 0:02:24 | 0:02:27 | |
their own weather. | 0:02:27 | 0:02:29 | |
Checks for take-off then, please. | 0:02:40 | 0:02:42 | |
INAUDIBLE RADIO CHAT | 0:02:42 | 0:02:45 | |
The Cloud Lab Team are setting out on the second half | 0:02:55 | 0:02:58 | |
of their epic voyage, heading west across the United States. | 0:02:58 | 0:03:03 | |
From Texas, they will journey from airfield to airfield through | 0:03:07 | 0:03:10 | |
the arid west before concluding the expedition on the Pacific coast. | 0:03:10 | 0:03:17 | |
But as they meet the desert, there's a dramatic change in the airship's behaviour. | 0:03:24 | 0:03:30 | |
Expedition leader, Felicity Aston, wants to know what's causing it. | 0:03:30 | 0:03:34 | |
What's happening with the movement? | 0:03:38 | 0:03:40 | |
We've suddenly started making really steep climbs and sharp descents. | 0:03:40 | 0:03:44 | |
We've just started getting some thermals now. | 0:03:44 | 0:03:46 | |
So we are getting these rising bubbles of air from the surface. | 0:03:46 | 0:03:49 | |
When we fly into it, it lifts the nose up then as we continue | 0:03:49 | 0:03:52 | |
it lifts the whole body up, and then as we move further it lifts the tail up | 0:03:52 | 0:03:56 | |
so we've got a correcting motion that pushes us back down again. | 0:03:56 | 0:03:59 | |
It's really quite steep. We're pointing to the sky one minute, | 0:03:59 | 0:04:02 | |
and then down at the floor the next. | 0:04:02 | 0:04:04 | |
It can get quite extreme at times, yes. | 0:04:04 | 0:04:06 | |
-You get used to it. -Really? Like sea-sickness? -Yes. | 0:04:06 | 0:04:10 | |
-You all right? -Yeah. | 0:04:13 | 0:04:17 | |
Despite the discomfort, it's the airship's ability to fly with the | 0:04:20 | 0:04:24 | |
currents of air that allows the team to pursue one of their key themes - | 0:04:24 | 0:04:28 | |
the relationship between life and the atmosphere. | 0:04:30 | 0:04:33 | |
They want to know how conditions change through the different layers | 0:04:37 | 0:04:41 | |
of the atmosphere and how that impacts upon the life found there. | 0:04:41 | 0:04:44 | |
So, Felicity and atmospheric chemist, Dr Jim McQuade, | 0:04:46 | 0:04:50 | |
are fishing for life in the layer of air that is the most dynamic | 0:04:50 | 0:04:53 | |
and closest to the earth. It's called the boundary layer. | 0:04:53 | 0:04:57 | |
We've got two - we've got two different ones. | 0:04:57 | 0:05:00 | |
By flying through this layer, they hope to shed light on one particular family of creatures... | 0:05:03 | 0:05:09 | |
He's pretty gorgeous. | 0:05:09 | 0:05:11 | |
..insects. | 0:05:12 | 0:05:13 | |
Whilst we're familiar with the lives of insects close to the | 0:05:16 | 0:05:19 | |
earth's surface, some have another, little known existence higher up | 0:05:19 | 0:05:24 | |
in the atmosphere. | 0:05:24 | 0:05:26 | |
The team are going to try and discover whether they get | 0:05:28 | 0:05:31 | |
blown here accidentally or are they exploiting atmospheric | 0:05:31 | 0:05:35 | |
conditions found in its different layers? | 0:05:35 | 0:05:38 | |
Elsewhere, another Cloud Lab team member | 0:05:50 | 0:05:52 | |
is targeting a different layer of the atmosphere | 0:05:52 | 0:05:55 | |
and another kind of life. | 0:05:55 | 0:05:56 | |
Microbiologist Dr Chris Van Tulleken is setting out | 0:05:58 | 0:06:02 | |
to find living bacteria in the high altitude death zone. | 0:06:02 | 0:06:07 | |
And the microscope I want to do last, just because it is so dusty. | 0:06:07 | 0:06:12 | |
He's brought in a specialist researcher, Noelle Bryan, to help him. | 0:06:12 | 0:06:16 | |
I need to get a sample of sky that's ten times higher than the samples | 0:06:18 | 0:06:25 | |
we've got before. So we're going up to almost 30,000 feet from... | 0:06:25 | 0:06:30 | |
you know, the cloud samples were from about 1,000 and 3,000 feet | 0:06:30 | 0:06:34 | |
so we want to find out if there are bacteria up there | 0:06:34 | 0:06:36 | |
and that's what Noelle is very, very expert at. | 0:06:36 | 0:06:39 | |
With this experiment, Chris is hoping to build upon some remarkable findings of his. | 0:06:44 | 0:06:49 | |
Earlier in the expedition, he discovered that the skies are alive. | 0:06:53 | 0:06:57 | |
We've got evidence here that we've got bacteria in clouds | 0:06:57 | 0:07:02 | |
and that's right at the cutting edge of science. | 0:07:02 | 0:07:05 | |
Chris not only detected bacteria in clouds, he revealed that | 0:07:05 | 0:07:10 | |
they played a significant role in making rain. Now, he's looking | 0:07:10 | 0:07:14 | |
for life beyond the clouds, upwards of 10,000 feet | 0:07:14 | 0:07:18 | |
to a layer of the atmosphere called the free troposphere. | 0:07:18 | 0:07:22 | |
Far away from the influence of the earth's surface, | 0:07:24 | 0:07:26 | |
the free troposphere is cold, desolate and bone dry. | 0:07:26 | 0:07:30 | |
Even for bacteria, this is an extreme environment. | 0:07:34 | 0:07:37 | |
Every time you look for a place where nothing should be able | 0:07:42 | 0:07:46 | |
to survive, there's always a microbe that can take it, | 0:07:46 | 0:07:50 | |
so that's what we are looking for. | 0:07:50 | 0:07:53 | |
Who is the hardiest, who is the toughest? | 0:07:53 | 0:07:55 | |
Who can take the desiccation, the low pressure, | 0:07:55 | 0:07:59 | |
the increased UV radiation? | 0:07:59 | 0:08:01 | |
Humans are wimps. We have a small temperature range. | 0:08:01 | 0:08:06 | |
We have a very defined set of environmental conditions | 0:08:06 | 0:08:10 | |
that we can survive. | 0:08:10 | 0:08:11 | |
Perhaps not all humans are wimps. | 0:08:15 | 0:08:18 | |
The free troposphere is far beyond the flight ceiling of the airship, | 0:08:18 | 0:08:24 | |
so Chris and Noelle have enlisted | 0:08:24 | 0:08:26 | |
the services of former paratrooper, Andy Torbet. | 0:08:26 | 0:08:28 | |
The idea is that I'm going to jump | 0:08:35 | 0:08:37 | |
out of a plane at about 26,000 feet and parachute | 0:08:37 | 0:08:42 | |
all the way back down to earth, collecting samples as I go. | 0:08:42 | 0:08:45 | |
The experiment will involve Andy attempting a highly technical jump | 0:08:49 | 0:08:53 | |
called a High Altitude High Opening, or HAHO. | 0:08:53 | 0:08:56 | |
It's usually the preserve of elite, special forces. | 0:08:56 | 0:09:00 | |
There's a lot of problems with sky diving from | 0:09:01 | 0:09:04 | |
26,000 feet so people don't do it. | 0:09:04 | 0:09:06 | |
One. The air is so thin, it's very, very hard to get stable. | 0:09:06 | 0:09:09 | |
You need to get stable within 3-5 seconds in order to open your chute. | 0:09:12 | 0:09:16 | |
If you open your parachute any longer than sort of 5 seconds, | 0:09:16 | 0:09:18 | |
you pick up so much speed again because the air is | 0:09:18 | 0:09:20 | |
so thin that when you open you get what's called a hard opening | 0:09:20 | 0:09:24 | |
and that actually has enough force to break your spine. | 0:09:24 | 0:09:29 | |
Bearing in mind that when I open my parachute at | 0:09:29 | 0:09:31 | |
26,000 feet it's going to be minus 28, minus 30 | 0:09:31 | 0:09:35 | |
so it's going to be bloody cold as well. | 0:09:35 | 0:09:38 | |
And the air is so thin, there's so little oxygen, | 0:09:38 | 0:09:41 | |
if you don't have an oxygen supply, like a mask on, | 0:09:41 | 0:09:43 | |
you're going to suffocate and die within about a minute. | 0:09:43 | 0:09:46 | |
So it's a fairly hostile environment. | 0:09:46 | 0:09:48 | |
Very little is known about life at the altitudes Andy is | 0:09:53 | 0:09:56 | |
reaching for but as we look for life beyond our planet, finding what | 0:09:56 | 0:10:03 | |
can survive earth's extreme habitats is taking on new significance. | 0:10:03 | 0:10:09 | |
It also requires a novel, scientific approach. | 0:10:09 | 0:10:12 | |
The principle is presumably going to be, Andy flies up. | 0:10:17 | 0:10:20 | |
He's got a petri dish or a growth medium dish. | 0:10:20 | 0:10:23 | |
He opens the lid. | 0:10:23 | 0:10:25 | |
Then closes the lid before he hits the ground and there's our sample. | 0:10:25 | 0:10:29 | |
But presumably it's a bit more complicated than that. | 0:10:29 | 0:10:32 | |
The idea is the same. | 0:10:32 | 0:10:34 | |
We're going to have a device that goes up. | 0:10:34 | 0:10:36 | |
It's going to open. | 0:10:36 | 0:10:38 | |
We're going to catch a sample, close the doors and bring it back down. | 0:10:38 | 0:10:41 | |
Only, instead of one surface of a Petri dish, | 0:10:41 | 0:10:44 | |
with these plastic rods we're able to have 40 different surfaces. | 0:10:44 | 0:10:47 | |
So, it's sealed. He goes up, opens it, | 0:10:47 | 0:10:52 | |
the air goes over and then before he hits 10,000 feet, closes. | 0:10:52 | 0:10:57 | |
Seal it back up. | 0:10:57 | 0:10:59 | |
And that's our sample. | 0:10:59 | 0:11:00 | |
Then we bring it back here and we can work out what it is. | 0:11:00 | 0:11:02 | |
And then we can do all sorts of different things. | 0:11:02 | 0:11:05 | |
A lot now depends on what Andy can achieve. | 0:11:08 | 0:11:10 | |
Over the coming days, he'll put the finishing touches | 0:11:11 | 0:11:14 | |
to weeks of preparation, | 0:11:14 | 0:11:17 | |
working with ex-special forces skydive master, Dane Kenny. | 0:11:17 | 0:11:21 | |
Two minutes. | 0:11:22 | 0:11:24 | |
Dane will supervise Andy as he jumps from increasingly high altitudes. | 0:11:25 | 0:11:30 | |
Acclimatising to the changing nature of the atmosphere. | 0:11:30 | 0:11:33 | |
Cloud Lab biologist, Dr Sarah Beynon, has joined the expedition | 0:11:57 | 0:12:01 | |
to further the survey of insect life. | 0:12:01 | 0:12:05 | |
-What time is it now? -Seven... | 0:12:05 | 0:12:07 | |
For Sarah, it's yielding some surprising insights into | 0:12:07 | 0:12:10 | |
exactly which insects are found in the boundary layer, | 0:12:10 | 0:12:14 | |
and at what altitude. | 0:12:14 | 0:12:15 | |
Bear with me. So, that's a flea beetle. | 0:12:18 | 0:12:21 | |
And I haven't seen any data of these being found at altitude before. | 0:12:21 | 0:12:26 | |
We had no idea that these insects were up there. | 0:12:26 | 0:12:30 | |
A lot of what we do know relies on radar which tells us | 0:12:30 | 0:12:34 | |
what's up there in terms of the abundance but we have no idea | 0:12:34 | 0:12:38 | |
what makes that up so tiny insects like this, | 0:12:38 | 0:12:41 | |
we can't tell what species of insect are up there. | 0:12:41 | 0:12:44 | |
So it's only through deploying something like this | 0:12:44 | 0:12:46 | |
that we have any idea of what is flying at those altitudes. | 0:12:46 | 0:12:51 | |
Now, Sarah wants to seek out evidence for one particular relationship | 0:12:55 | 0:13:00 | |
between insect and atmospheric condition. | 0:13:00 | 0:13:03 | |
So I have a spare net, so I'll put that one in. | 0:13:06 | 0:13:09 | |
OK, thank you. | 0:13:09 | 0:13:12 | |
Can you record the altitude, as well please Jim, and the time? | 0:13:12 | 0:13:15 | |
What time is it now? | 0:13:15 | 0:13:16 | |
-Uh, 7:03. -OK. | 0:13:16 | 0:13:19 | |
The aim is to roam the vastness of the sky to intercept | 0:13:26 | 0:13:29 | |
a noctuid moth, one of a family of different species. | 0:13:29 | 0:13:32 | |
To do so, they must first wait for nightfall and a radical | 0:13:36 | 0:13:40 | |
transformation of the atmosphere called the nocturnal inversion. | 0:13:40 | 0:13:44 | |
-How high are we now? -Er, Nine hundred feet. | 0:13:45 | 0:13:49 | |
-Nine hundred feet? -Yeah. | 0:13:49 | 0:13:50 | |
As the sun goes down, the air that sits above the earth cools | 0:13:56 | 0:14:00 | |
more rapidly than the air at high altitude and that can create | 0:14:00 | 0:14:04 | |
fast-moving streams of air. | 0:14:04 | 0:14:05 | |
Noctuid moths are believed to use this nocturnal inversion to migrate | 0:14:10 | 0:14:15 | |
as far as 600 miles in a single night | 0:14:15 | 0:14:18 | |
by selecting the most favourable air streams... | 0:14:18 | 0:14:21 | |
..but rarely have they been caught in the process. | 0:14:23 | 0:14:27 | |
Sarah aims to change all that. | 0:14:27 | 0:14:29 | |
The moths at this time of night should be making their way | 0:14:33 | 0:14:36 | |
up into the higher airspace to migrate. | 0:14:36 | 0:14:40 | |
-So we should catch them on their journey upwards. -Yeah. | 0:14:40 | 0:14:43 | |
The airship's sensitivity to atmospheric conditions | 0:14:46 | 0:14:50 | |
pays dividends as it drifts with the air currents. | 0:14:50 | 0:14:53 | |
All they can do now is sit, wait and hope | 0:14:57 | 0:15:00 | |
that the moths are on their way. | 0:15:00 | 0:15:04 | |
Ooh a moth! | 0:15:14 | 0:15:17 | |
-No kidding! -No there really is a moth, where did it go? | 0:15:17 | 0:15:21 | |
Hang on. OK, lights? I haven't got my net with me. | 0:15:21 | 0:15:24 | |
Shine a light somewhere and keep it there, to keep the moth to it. | 0:15:24 | 0:15:27 | |
A moth has flown in through the window. | 0:15:27 | 0:15:29 | |
I need to get a net, OK, thank you. | 0:15:29 | 0:15:31 | |
Oh, it's here, it's here! | 0:15:35 | 0:15:37 | |
-Whoa, whoa - gosh, where's it gone? -There. | 0:15:37 | 0:15:41 | |
OK, could you grab the killing cloth please? | 0:15:44 | 0:15:47 | |
We've found a moth! | 0:15:47 | 0:15:50 | |
The net isn't collecting them, but it's just | 0:15:50 | 0:15:52 | |
flown in at 500 feet above the ground, which means they're here! | 0:15:52 | 0:15:57 | |
OK, we need to be careful as I need to know what species it is. | 0:15:57 | 0:16:00 | |
I think what we'll do is just shove the whole net in | 0:16:00 | 0:16:02 | |
to be on the safe side. Awesome! | 0:16:02 | 0:16:05 | |
Teamwork! Excellent! | 0:16:07 | 0:16:11 | |
PILOT: Ready for landing, OK? | 0:16:13 | 0:16:15 | |
Sarah will need to get the moth under better light to identify it. | 0:16:18 | 0:16:23 | |
Only then can she be sure if it's one of the migrating noctuid species | 0:16:23 | 0:16:28 | |
taking advantage of the night-time air. | 0:16:28 | 0:16:30 | |
For the airship's 15-strong ground support team, | 0:16:36 | 0:16:39 | |
the night has just begun. | 0:16:39 | 0:16:41 | |
After several weeks of flying, the airship has been venting helium | 0:16:41 | 0:16:45 | |
in order to adjust to different altitudes. Now it needs topping up. | 0:16:45 | 0:16:49 | |
Well, this is the second rack here we've probably got at least two more. | 0:16:49 | 0:16:53 | |
We've been here about an hour so far so maybe another couple of hours. | 0:16:53 | 0:16:57 | |
Taking care of the airship all the time - it needs constant attention. | 0:16:57 | 0:17:02 | |
It's a very demanding mistress. | 0:17:02 | 0:17:04 | |
Sarah is drawing together the haul of insects from the survey. | 0:17:13 | 0:17:17 | |
Already, she's discerning a difference between the insects that | 0:17:17 | 0:17:20 | |
travel by day and those that travel by night, | 0:17:20 | 0:17:23 | |
including the one that flew into the airship. | 0:17:23 | 0:17:25 | |
In the daytime, most of the insects we caught were small, | 0:17:27 | 0:17:31 | |
like this leaf beetle | 0:17:31 | 0:17:32 | |
and these insects would have been carried up by the | 0:17:33 | 0:17:36 | |
turbulent daytime air and would have been at the mercy of the winds. | 0:17:36 | 0:17:41 | |
Whereas at night-time, everything started to get a bit more | 0:17:41 | 0:17:45 | |
interesting and every single time we flew at night, | 0:17:45 | 0:17:49 | |
we caught migratory, noctuid moths. | 0:17:49 | 0:17:52 | |
We've got a fall armyworm moth here | 0:17:52 | 0:17:57 | |
and these moths, they migrate northwards in the spring | 0:17:57 | 0:18:01 | |
and summer to make the most of the agricultural crops that are | 0:18:01 | 0:18:04 | |
growing and they decimate crops such as corn and cotton and then they | 0:18:04 | 0:18:09 | |
migrate...well, we think they migrate southwards again in the fall. | 0:18:09 | 0:18:14 | |
But we know very, very little about this fall migration | 0:18:17 | 0:18:21 | |
so any individuals we find in the fall is really, really useful. | 0:18:21 | 0:18:26 | |
The study demonstrates how insects exploit the varying conditions | 0:18:29 | 0:18:34 | |
of the sky at different altitudes and times of day. | 0:18:34 | 0:18:37 | |
Other research suggests that insects exploit the dynamic nature | 0:18:40 | 0:18:44 | |
of the boundary layer on a vast scale. | 0:18:44 | 0:18:48 | |
So, in a 1km square patch of countryside surveyed over the course | 0:18:48 | 0:18:51 | |
of a summer month, as many as 3 billion insects pass overhead. | 0:18:51 | 0:18:57 | |
The question remains, how much life exists | 0:19:03 | 0:19:06 | |
beyond here in the higher atmosphere? | 0:19:06 | 0:19:09 | |
-Is that tight? -Yeah, that's tight. | 0:19:11 | 0:19:14 | |
It's a question Andy hopes to soon help answer by undertaking | 0:19:14 | 0:19:18 | |
the HAHO jump. At more than 26,000 feet, | 0:19:18 | 0:19:24 | |
it will be the highest he's attempted yet. | 0:19:24 | 0:19:26 | |
Remember, the priority is safe parachuting. | 0:19:27 | 0:19:32 | |
So I know this is very important, | 0:19:32 | 0:19:34 | |
but we can't do that if you've got an issue with the parachute. | 0:19:34 | 0:19:37 | |
-Happy? -Happy. -Good. | 0:19:37 | 0:19:40 | |
-Right, let's get out there. -Look at that. | 0:19:40 | 0:19:45 | |
Steady as a rock but I shoot with this hand. | 0:19:45 | 0:19:48 | |
You'll be fine, mate. | 0:19:51 | 0:19:53 | |
Andy will have just one attempt to get the precious air sample, | 0:19:55 | 0:19:59 | |
and with it, a chance of finding microbial life. | 0:19:59 | 0:20:02 | |
The weather is closing in and safe conditions | 0:20:08 | 0:20:11 | |
are unlikely to return for days. | 0:20:11 | 0:20:13 | |
Before going to altitude, | 0:20:16 | 0:20:18 | |
the entire team must flood their lungs with pure oxygen. | 0:20:18 | 0:20:21 | |
If not, there's a risk that the nitrogen in their blood | 0:20:23 | 0:20:26 | |
could form bubbles, leading to the bends. | 0:20:26 | 0:20:28 | |
Without this and other precautions against | 0:20:33 | 0:20:35 | |
the sub-freezing temperatures and desperately dry air, | 0:20:35 | 0:20:39 | |
Andy would be dead within seconds. | 0:20:39 | 0:20:41 | |
It raises the question of how ANY life, even bacteria, | 0:20:47 | 0:20:51 | |
can survive extreme altitudes. | 0:20:51 | 0:20:53 | |
The answer could lie in another form of microscopic life, | 0:21:01 | 0:21:04 | |
one that has an extraordinary adaptation to aridity. | 0:21:06 | 0:21:09 | |
These are things called tardigrades or water bears | 0:21:12 | 0:21:16 | |
and they are unusual because they're extremely small and they can | 0:21:16 | 0:21:20 | |
survive complete desiccation, so complete drying out and this is | 0:21:20 | 0:21:25 | |
a desiccated, a dried out tardigrade here magnified on the microscope. | 0:21:25 | 0:21:30 | |
They are in a state of almost suspended animation. | 0:21:30 | 0:21:33 | |
The chemical processes that drive life are at a virtual standstill. | 0:21:35 | 0:21:39 | |
But it takes just a few drops of water to re-animate it. | 0:21:43 | 0:21:47 | |
When you run water over it, you see the chemical reactions start | 0:21:49 | 0:21:53 | |
happening again, absorbing the water and is now very obviously alive. | 0:21:53 | 0:22:01 | |
And it's gone from chemically dead, chemically totally inert, to now | 0:22:01 | 0:22:07 | |
being, you know, obviously quite an adorable little living thing. | 0:22:07 | 0:22:11 | |
It's got little legs and kind of a little face there. | 0:22:11 | 0:22:14 | |
Whilst the transformation is plain to see, | 0:22:17 | 0:22:20 | |
the secret to the tardigrade's survival is what's happening within. | 0:22:20 | 0:22:25 | |
We think that the way the tardigrades survive those | 0:22:25 | 0:22:28 | |
environments is by being able to tolerate the DNA | 0:22:28 | 0:22:31 | |
and protein damage that comes from being terribly dried out. | 0:22:31 | 0:22:35 | |
What they have is very, very good DNA repair mechanisms. | 0:22:35 | 0:22:39 | |
Chris believes that bacteria at high altitude | 0:22:44 | 0:22:47 | |
may use these same repair mechanisms to withstand the aridity. | 0:22:47 | 0:22:51 | |
Finding live specimens will go a long way to suggesting as much. | 0:22:55 | 0:22:58 | |
That now depends on what happens when Andy meets | 0:23:02 | 0:23:05 | |
the vanishingly thin air. | 0:23:05 | 0:23:07 | |
If Andy can't get stable, he'll have to free-fall to where the air is dense enough to slow his descent. | 0:23:33 | 0:23:39 | |
God, he's got a lot to think about. | 0:23:54 | 0:23:56 | |
It's much, much more skilful than I thought it was. | 0:23:57 | 0:24:00 | |
Andy's botched the exit and is struggling to get stable. | 0:24:39 | 0:24:42 | |
Despite the poor exit, Andy managed to open his parachute within | 0:25:15 | 0:25:18 | |
the vital first few seconds. | 0:25:18 | 0:25:20 | |
Now, he has to gather the sample. | 0:25:22 | 0:25:24 | |
The box must be closed at 10,000 feet. | 0:25:55 | 0:25:58 | |
If not, he will expose the sample to the lower atmosphere | 0:25:59 | 0:26:03 | |
where life can more easily exist. | 0:26:03 | 0:26:05 | |
There he is. | 0:26:30 | 0:26:32 | |
The reason I get Andy to do this is because he's a much better | 0:26:32 | 0:26:35 | |
microbiologist than I am a sky diver. | 0:26:35 | 0:26:38 | |
Andy appears to have pulled off the job. | 0:26:40 | 0:26:43 | |
But there's one thing the team haven't foreseen | 0:26:46 | 0:26:49 | |
that jeopardises the entire experiment. | 0:26:49 | 0:26:52 | |
Oooh! | 0:26:54 | 0:26:55 | |
Now, the sample is at risk of contamination. | 0:26:57 | 0:27:01 | |
You all right, mate? How you doing? | 0:27:01 | 0:27:03 | |
It was a good landing. | 0:27:03 | 0:27:05 | |
What I wasn't expecting is my feet were dead. | 0:27:05 | 0:27:07 | |
-I had no blood in my feet. -They were numb, really? | 0:27:07 | 0:27:11 | |
-Your shoes are freezing cold. -Because I've been | 0:27:12 | 0:27:15 | |
sitting in this harness 20 minutes, | 0:27:15 | 0:27:16 | |
my legs were completely numb and they just gave way on me. | 0:27:16 | 0:27:20 | |
Well, never mind that, let's make this safe. | 0:27:20 | 0:27:23 | |
-Good. Right I'm going to get this to the lab. -OK, mate, no dramas. | 0:27:27 | 0:27:30 | |
The sense of relief is just... It was weird. | 0:27:33 | 0:27:36 | |
You don't notice the kind of the amount of stress or pressure | 0:27:36 | 0:27:39 | |
that's on your shoulders that's built up over the last three months | 0:27:39 | 0:27:42 | |
until it's taken away. | 0:27:42 | 0:27:44 | |
And suddenly you're like... It's gone, we've actually done it. | 0:27:44 | 0:27:47 | |
There's an element of kind of disbelief we've actually | 0:27:47 | 0:27:51 | |
pulled this off. | 0:27:51 | 0:27:52 | |
I got to jump the HAHO | 0:27:52 | 0:27:53 | |
and I managed to pull it off without seriously | 0:27:53 | 0:27:56 | |
injuring myself or killing myself, so, er... It was really good. | 0:27:56 | 0:28:02 | |
No-one's ever done it like this before. | 0:28:02 | 0:28:04 | |
But you know, if you work out how much of the air up there we've | 0:28:06 | 0:28:09 | |
passed over the rods, we should get something sticking and all we want | 0:28:09 | 0:28:14 | |
to see is that there's something up there, you know it's... One | 0:28:14 | 0:28:17 | |
or two bugs and we can amplify them, grow them, work out what they are. | 0:28:17 | 0:28:21 | |
It's a lovely thought isn't it, this, | 0:28:21 | 0:28:24 | |
got a little bit of troposphere in here. | 0:28:24 | 0:28:27 | |
It's really nice. | 0:28:27 | 0:28:29 | |
-Noelle! -Is this it? | 0:28:30 | 0:28:33 | |
That is it. | 0:28:33 | 0:28:35 | |
Did you think we were going to get this, honestly? | 0:28:35 | 0:28:37 | |
No. | 0:28:37 | 0:28:39 | |
Andy's slow descent through more than 16,000 feet | 0:28:41 | 0:28:44 | |
of high-altitude air has given Chris and Noelle the best chance | 0:28:44 | 0:28:47 | |
of finding microbial life. | 0:28:47 | 0:28:51 | |
It will require forensic precision to ensure it wasn't in vain. | 0:28:51 | 0:28:55 | |
It's worth explaining that while we do this, sterile air is | 0:28:55 | 0:28:59 | |
flowing from this all over this surface so that no bugs can get in. | 0:28:59 | 0:29:06 | |
So even if a piece of hair falls off Noelle's head, | 0:29:06 | 0:29:09 | |
it won't land on the sample. | 0:29:09 | 0:29:11 | |
This is what I do all day virtually every day in London. | 0:29:21 | 0:29:26 | |
And I think it puts a lot of people off doing science | 0:29:26 | 0:29:29 | |
because it seems super mundane but it isn't. | 0:29:29 | 0:29:32 | |
This is where we... This is where we get the answers. | 0:29:32 | 0:29:37 | |
The best bit is not the skydiving. | 0:29:37 | 0:29:39 | |
The best bit is the answers. | 0:29:39 | 0:29:42 | |
Now we want to have a look at it on the microscope. | 0:29:42 | 0:29:46 | |
And in order to look at it, we're going to stain it with another dye. | 0:29:46 | 0:29:51 | |
We're going to stain it with this stuff which stains nucleic acid | 0:29:51 | 0:29:55 | |
so, things like DNA. Again, only life has nucleic acid, so it'll | 0:29:55 | 0:30:00 | |
stain that and then we'll be able to see the objects more clearly. | 0:30:00 | 0:30:04 | |
Once the sample is stained, | 0:30:06 | 0:30:08 | |
any cells will reflect back the light emitted from the microscope, | 0:30:08 | 0:30:13 | |
showing up as tiny glimmers of green. | 0:30:13 | 0:30:15 | |
There you go. You see... | 0:30:17 | 0:30:18 | |
You think there's going to be nothing there don't you, | 0:30:18 | 0:30:21 | |
you're just looking in to blackness and then - | 0:30:21 | 0:30:24 | |
what I was hoping to see and what I can see - is every | 0:30:24 | 0:30:28 | |
once in a while you move the microscope and that's what you see. | 0:30:28 | 0:30:31 | |
You just get that little beacon of a green dot. | 0:30:31 | 0:30:34 | |
Just a little green glow. | 0:30:34 | 0:30:36 | |
And each of those little green dots - those are cells. | 0:30:36 | 0:30:39 | |
The amazing thing is it's one thing | 0:30:39 | 0:30:41 | |
seeing the DNA glowing in the right size and shape of a bacteria | 0:30:41 | 0:30:45 | |
but the fact that it's alive, that is a really peculiar thing. | 0:30:45 | 0:30:49 | |
To find dead bacteria up there yeah, maybe. | 0:30:49 | 0:30:52 | |
To find living stuff up there is such a harsh environment. | 0:30:52 | 0:30:55 | |
No oxygen, its freezing cold, low pressure, | 0:30:55 | 0:30:58 | |
-high winds, you know, no water. -No water. | 0:30:58 | 0:31:02 | |
Amazing. | 0:31:02 | 0:31:04 | |
The experiment joins a growing band of scientific research into life high in the atmosphere. | 0:31:07 | 0:31:13 | |
The picture that is emerging is that life is far more robust than ever imagined. | 0:31:17 | 0:31:22 | |
And that opens up all sorts of possibilities | 0:31:27 | 0:31:29 | |
for the prospects for life | 0:31:29 | 0:31:31 | |
in other extreme environments beyond our planet. | 0:31:31 | 0:31:34 | |
PILOT SPEAKS OVER RADIO | 0:31:47 | 0:31:52 | |
The airship is heading to the desert city of Phoenix, Arizona. | 0:32:11 | 0:32:15 | |
What's drawing the team here is another of their key themes, | 0:32:21 | 0:32:25 | |
the way in which we, ourselves, | 0:32:27 | 0:32:29 | |
can change the way the atmosphere behaves. | 0:32:29 | 0:32:32 | |
Earlier in the expedition, Felicity and atmospheric chemist, | 0:32:37 | 0:32:41 | |
Dr Jim McQuade, uncovered the surprising link | 0:32:41 | 0:32:44 | |
between pollution, clouds and extreme weather. | 0:32:44 | 0:32:49 | |
So what we're saying is that by cleaning | 0:32:51 | 0:32:54 | |
up our atmosphere, we've allowed there to be more hurricanes. | 0:32:54 | 0:32:59 | |
They're now hoping that Cloud Lab will enable them | 0:33:05 | 0:33:07 | |
to get to the bottom of another question | 0:33:07 | 0:33:10 | |
about our impact on the atmosphere - | 0:33:10 | 0:33:12 | |
can cities make their own weather? | 0:33:12 | 0:33:15 | |
So, I've been looking at historical data | 0:33:17 | 0:33:20 | |
and you can see that Phoenix, in the last 100 years, has gone | 0:33:20 | 0:33:24 | |
from being a really small, agricultural settlement into a large, urban city. | 0:33:24 | 0:33:30 | |
In the same period of time, there has been a distinct | 0:33:30 | 0:33:33 | |
change in the amount of rainfall in the city. | 0:33:33 | 0:33:36 | |
There are areas of Phoenix that have had up to | 0:33:37 | 0:33:40 | |
a 12% increase in the amount of rainfall which is really significant | 0:33:40 | 0:33:46 | |
and it looks like there might be a correlation between the two. | 0:33:46 | 0:33:49 | |
So, we want to see | 0:33:49 | 0:33:50 | |
if we can unravel how the city might be creating its own weather. | 0:33:50 | 0:33:54 | |
It's difficult to imagine that a single city could interfere | 0:33:59 | 0:34:03 | |
with a process that unfolds on such a grand scale as the weather. | 0:34:03 | 0:34:07 | |
The rain that falls here has followed the same cycle for millennia. | 0:34:10 | 0:34:14 | |
Every summer, warm, moist air is swept up from the oceans | 0:34:16 | 0:34:20 | |
to the South. As this air meets the hot desert, | 0:34:20 | 0:34:26 | |
variations in the landscape drive pockets of air upwards as thermals | 0:34:26 | 0:34:32 | |
where the moisture cools, condenses and ultimately falls | 0:34:32 | 0:34:39 | |
in sudden downpours of rain. | 0:34:39 | 0:34:41 | |
Where this rain occurs should be fairly random... | 0:34:47 | 0:34:51 | |
..but something appears to be concentrating it upon the city. | 0:34:57 | 0:35:01 | |
To see why, Felicity is going to start by surveying temperatures in Phoenix and the surrounding desert. | 0:35:07 | 0:35:13 | |
I took several readings of the surface temperature and I was | 0:35:19 | 0:35:22 | |
getting between 37 and 38 degrees centigrade. | 0:35:22 | 0:35:28 | |
So, it's pretty hot down there, | 0:35:28 | 0:35:29 | |
it's soaking up all the heat from the sun. | 0:35:29 | 0:35:32 | |
For the city to be concentrating rainfall, it needs to be | 0:35:36 | 0:35:40 | |
hotter than the desert, driving extra thermal activity. | 0:35:40 | 0:35:43 | |
Meanwhile, Jim is surveying another factor that could be increasing rain - humidity. | 0:35:52 | 0:35:58 | |
A hygrometer gives an on-the-spot reading of how much water vapour | 0:35:59 | 0:36:04 | |
is being carried in the air. | 0:36:04 | 0:36:07 | |
The dry bulb was 24.5, giving | 0:36:07 | 0:36:10 | |
a relative humidity of 26%. | 0:36:10 | 0:36:13 | |
So, the air's very dry here, which is actually the definition of a desert. | 0:36:13 | 0:36:18 | |
It's nothing to do with temperature. | 0:36:18 | 0:36:20 | |
It's how dry it is, | 0:36:20 | 0:36:21 | |
so that's why Antarctica can be classified as a desert. | 0:36:21 | 0:36:24 | |
Unsurprisingly, in the desert, there's plenty of heat but no water. | 0:36:27 | 0:36:32 | |
But what really matters is how this picture compares with the city. | 0:36:35 | 0:36:40 | |
OK, another measurement next to an orange tree | 0:36:50 | 0:36:53 | |
and a lemon tree in someone's front garden. | 0:36:53 | 0:36:56 | |
It's not like back in Leeds - got an apple tree. | 0:36:57 | 0:37:00 | |
45% relative humidity. | 0:37:06 | 0:37:09 | |
It's very obvious that there's a lot more water available to be | 0:37:10 | 0:37:14 | |
evaporating into the atmosphere just from manicured lawns. | 0:37:14 | 0:37:18 | |
There are lots of sprinklers down here. | 0:37:18 | 0:37:20 | |
Increased humidity is a consequence of the millions of gallons of water | 0:37:32 | 0:37:36 | |
diverted to the city from the surrounding rivers. | 0:37:36 | 0:37:39 | |
I'm getting a real variety in surface temperatures. | 0:37:42 | 0:37:45 | |
So, if I take a reading from the road or a car park, it's pretty much the | 0:37:45 | 0:37:51 | |
same surface temperature as in the desert, but if I point the camera | 0:37:51 | 0:37:56 | |
at a garden or a swimming pool or a roof top, then it's a lot less. | 0:37:56 | 0:38:02 | |
So, on average, the surface temperature here will overall | 0:38:02 | 0:38:07 | |
be a lot less than the desert. | 0:38:07 | 0:38:09 | |
The city is more humid and a little cooler than the surrounding desert. | 0:38:14 | 0:38:19 | |
Despite these differences, there's no evidence | 0:38:19 | 0:38:22 | |
for the increased thermal activity that can explain the rainfall. | 0:38:22 | 0:38:25 | |
As the day wears on, that picture soon changes. | 0:38:38 | 0:38:41 | |
See, look, look, look, look! See the city... | 0:38:48 | 0:38:52 | |
-Yeah. -.it's hotter than the desert. | 0:38:52 | 0:38:54 | |
OK, yeah, you can see definitely the boundary. | 0:38:54 | 0:38:58 | |
So that's the desert cooling down | 0:38:58 | 0:39:00 | |
and that's the hot city. | 0:39:00 | 0:39:02 | |
That's a really nice example of it. | 0:39:02 | 0:39:04 | |
Whilst the natural landscape has quickly cooled, | 0:39:09 | 0:39:11 | |
the camera reveals the city to have remained warm. | 0:39:11 | 0:39:14 | |
They've identified an effect called the urban heat island. | 0:39:18 | 0:39:21 | |
Earlier today we measured the ground temperature of the suburbs to | 0:39:26 | 0:39:29 | |
be 24, 25 degrees, and see I'm measuring 23, 22. | 0:39:29 | 0:39:35 | |
I mean, it's still as hot as | 0:39:35 | 0:39:36 | |
when we measured it in the middle of the day. | 0:39:36 | 0:39:39 | |
The city's surfaces are continuing to radiate the energy of the sun | 0:39:41 | 0:39:44 | |
they absorbed earlier in the day. | 0:39:44 | 0:39:46 | |
The question is whether the urban heat island is generating thermals. | 0:39:49 | 0:39:53 | |
If it is, they should be able to detect | 0:39:55 | 0:39:58 | |
an increase in temperature at altitude from the airship. | 0:39:58 | 0:40:01 | |
So, I've just had a look the temperature | 0:40:03 | 0:40:06 | |
and this is the temperature going down and that's going down simply | 0:40:06 | 0:40:09 | |
because the sun's going down, you know, we're turning the heater off. | 0:40:09 | 0:40:12 | |
So, this is the temperature over the desert | 0:40:12 | 0:40:15 | |
and this is the temperature over the city. | 0:40:15 | 0:40:18 | |
-Oh, wow, so this is where we hit the city? -Yeah. -OK, this is us... | 0:40:18 | 0:40:22 | |
this is the temperature over the desert and then | 0:40:22 | 0:40:24 | |
we hit the city limits and the temperature quite clearly goes up. | 0:40:24 | 0:40:28 | |
It's not a huge increase, you know, no more than half a degree, | 0:40:28 | 0:40:33 | |
but you can't argue with that. That's a definite. | 0:40:33 | 0:40:35 | |
Despite the difference in temperature being small, it's critical. | 0:40:38 | 0:40:42 | |
It's enough for us to know that the | 0:40:44 | 0:40:46 | |
air above the city is warmer. | 0:40:46 | 0:40:48 | |
So we've got this big parcel of warm air sitting over the city. | 0:40:48 | 0:40:53 | |
It makes a lot of logical sense that that air is going to start rising and | 0:40:55 | 0:40:58 | |
that's going to start convection and the consequence of that is weather. | 0:40:58 | 0:41:03 | |
So the increased rainfall in Phoenix could be caused | 0:41:07 | 0:41:10 | |
by the urban heat island effect. | 0:41:10 | 0:41:12 | |
It generates thermals over the city that force air upward where it | 0:41:14 | 0:41:18 | |
begins to cool. | 0:41:18 | 0:41:20 | |
That, in turn, can cause the vapour to condense | 0:41:20 | 0:41:23 | |
and form rain concentrated here upon Phoenix. | 0:41:23 | 0:41:27 | |
So, we've found | 0:41:30 | 0:41:31 | |
the connection we were looking for, between cities, and the increased | 0:41:31 | 0:41:35 | |
rainfall that Phoenix has been experiencing in the last 100 years. | 0:41:35 | 0:41:40 | |
And the really exciting thing about that is that we've hard | 0:41:40 | 0:41:43 | |
evidence that human beings are creating their own weather. | 0:41:43 | 0:41:47 | |
It's a finding that threatens to have far-reaching consequences. | 0:41:52 | 0:41:56 | |
Our world is increasingly urban and much of that urban expansion | 0:41:57 | 0:42:02 | |
is taking place in sparsely populated arid regions... | 0:42:02 | 0:42:06 | |
..with unknown consequences. | 0:42:06 | 0:42:08 | |
If you take an area of desert and build a city on it, | 0:42:20 | 0:42:23 | |
then that city is going to be much warmer than the desert it's replaced. | 0:42:23 | 0:42:27 | |
And it's going to have an overall warming effect. | 0:42:27 | 0:42:30 | |
So if you multiply that by all the cities being built in desert | 0:42:31 | 0:42:36 | |
areas, all this turning from desert land into green agricultural, | 0:42:36 | 0:42:42 | |
irrigated land, then it leaves another little hanging question, | 0:42:42 | 0:42:46 | |
whether this is having a much larger global effect on our climate. | 0:42:46 | 0:42:50 | |
The airship has reached the western edge of the desert. | 0:43:03 | 0:43:07 | |
Beyond here lies their destination... | 0:43:07 | 0:43:09 | |
..the mighty Pacific, where the team want to conduct their final | 0:43:15 | 0:43:20 | |
set of studies. | 0:43:20 | 0:43:21 | |
An exploration of how the prevailing onshore Pacific wind shapes | 0:43:23 | 0:43:28 | |
the wildlife of the entire Californian coastline. | 0:43:28 | 0:43:31 | |
And that includes the life below the ocean surface. | 0:43:34 | 0:43:37 | |
But first, the airship will have to overcome the Pacific wind. | 0:43:42 | 0:43:46 | |
We're so close to the end of our journey that we can | 0:43:49 | 0:43:52 | |
almost smell the Pacific Ocean. | 0:43:52 | 0:43:54 | |
But there's one last obstacle. These mountains behind me. | 0:43:54 | 0:43:58 | |
There's only one pass through these mountains for miles in either direction. | 0:43:58 | 0:44:02 | |
It's called Banning Pass and it's a bit of a problem for the airship | 0:44:02 | 0:44:06 | |
because it's so narrow. All the winds are funnelled through. | 0:44:06 | 0:44:09 | |
And the winds come from the west towards us so it's going to be flying | 0:44:09 | 0:44:14 | |
into the winds and if there's too much wind, it could take hours, days. | 0:44:14 | 0:44:20 | |
Perhaps we could even be waiting for a week | 0:44:20 | 0:44:22 | |
until conditions are just right. | 0:44:22 | 0:44:24 | |
Even if the wind is blowing a gentle breeze on the far | 0:44:29 | 0:44:31 | |
side of the pass, by the time it reaches the entrance | 0:44:31 | 0:44:35 | |
the funnelling effect can accelerate it to gale force. | 0:44:35 | 0:44:38 | |
We seem to be hitting a lot of turbulence. | 0:44:48 | 0:44:51 | |
The wind is gusting and coming down the valley here. | 0:44:51 | 0:44:53 | |
There's two big mountain ranges coming together to give us | 0:44:53 | 0:44:56 | |
just this one little gap down the middle, so it's much rougher air now. | 0:44:56 | 0:45:00 | |
So you are really having to fight to keep it level? | 0:45:00 | 0:45:02 | |
It's a continuous fight | 0:45:02 | 0:45:03 | |
but at the moment we're making slow progress. | 0:45:03 | 0:45:06 | |
OK, so what's our ground speed at the minute? | 0:45:06 | 0:45:08 | |
-About five knots. -Five knots? 6mph. | 0:45:08 | 0:45:11 | |
It's very bizarre. We are in this unseen jet stream of air. | 0:45:14 | 0:45:19 | |
So these engines are going fast enough to propel us at 30-40 knots, | 0:45:19 | 0:45:24 | |
but unfortunately the wind's coming in the opposite direction | 0:45:24 | 0:45:27 | |
at 30-35 knots, so we're only making only 2 or 3 knots ground speed. | 0:45:27 | 0:45:32 | |
We've barely moved at all. About two miles in the last hour. | 0:45:32 | 0:45:37 | |
-Co-pilot: -It's actually getting worse right at the moment. | 0:45:37 | 0:45:41 | |
We've actually stopped. | 0:45:41 | 0:45:44 | |
I don't think we're going to be going through today. | 0:45:49 | 0:45:52 | |
The vast wind farm here one of the largest in Southern California | 0:45:58 | 0:46:02 | |
is testament to the winds near-constant presence. | 0:46:02 | 0:46:05 | |
We're definitely starting to move forward. | 0:46:11 | 0:46:14 | |
Back there we were not, | 0:46:14 | 0:46:15 | |
now we are definitely moving forward a wee bit. | 0:46:15 | 0:46:17 | |
-CO-PILOT: -Yeah, there we go. We are going it a little bit here. | 0:46:17 | 0:46:20 | |
Despite Felicity's worst fears it seems as though they have | 0:46:22 | 0:46:26 | |
chosen the right day to make their move. | 0:46:26 | 0:46:28 | |
Sarah has gone ahead of the airship to experience the power of the | 0:46:50 | 0:46:54 | |
onshore Pacific wind for herself. | 0:46:54 | 0:46:56 | |
We are going to do a little bit of scratching here, | 0:46:56 | 0:46:59 | |
when we are close to the cliff edge. | 0:46:59 | 0:47:01 | |
And scratching is doing what? | 0:47:01 | 0:47:03 | |
-Well, when we are very close to the edge of the cliff... -Like this? | 0:47:03 | 0:47:07 | |
Yeah. Scratching is our term. | 0:47:07 | 0:47:09 | |
This is where the most lift is, close to the cliff edge. | 0:47:11 | 0:47:16 | |
Sarah and Kirk are being carried on a type of air | 0:47:18 | 0:47:21 | |
movement known as ridge lift. | 0:47:21 | 0:47:23 | |
As the onshore wind hits the cliff, it is diverted | 0:47:25 | 0:47:28 | |
and accelerated upward. | 0:47:28 | 0:47:30 | |
But the real reason Sarah is here is to see how this movement of air | 0:47:31 | 0:47:35 | |
supports life. | 0:47:35 | 0:47:37 | |
Home! Shanty! | 0:47:37 | 0:47:39 | |
Good girl. | 0:47:41 | 0:47:43 | |
-Oh, wow! -Unbelievable, huh? -Oh! | 0:47:46 | 0:47:50 | |
So this is Shanty, who is a trained bird | 0:47:50 | 0:47:53 | |
-and she's using the same updraught that we're using. -Up! | 0:47:53 | 0:47:57 | |
Shanty is a Harris hawk. | 0:48:01 | 0:48:04 | |
A native to this region, they are so highly evolved to | 0:48:06 | 0:48:09 | |
fly on the movement of air from ridge lift to rising thermals | 0:48:09 | 0:48:13 | |
much of their flight time is spent soaring. | 0:48:13 | 0:48:15 | |
Wow! | 0:48:18 | 0:48:20 | |
You can really see her wide, fairly short wings | 0:48:20 | 0:48:25 | |
and that's an adaptation to soaring. | 0:48:25 | 0:48:27 | |
Look at her soaring up there now. | 0:48:27 | 0:48:29 | |
And it's great to see the sort of finger-tips of her wings that | 0:48:29 | 0:48:32 | |
she's using to control her flight. | 0:48:32 | 0:48:36 | |
It's a behaviour found throughout the family of birds called raptors | 0:48:36 | 0:48:41 | |
that also includes eagles and vultures, enabling them | 0:48:41 | 0:48:44 | |
to extend their range to vast distances. | 0:48:44 | 0:48:50 | |
It makes sense for them to use these up-draughts | 0:48:50 | 0:48:52 | |
so that they expend as little energy as possible when they are hunting. | 0:48:52 | 0:48:56 | |
Exactly. And the raptors own motto, like any good predator, | 0:48:56 | 0:49:00 | |
is the maximum amount of reward for the least amount of effort. | 0:49:00 | 0:49:03 | |
So if they can stay up without putting much energy into it, | 0:49:03 | 0:49:08 | |
that's great. | 0:49:08 | 0:49:10 | |
-Here she comes again. -Goodness me. | 0:49:10 | 0:49:14 | |
Good girl! | 0:49:14 | 0:49:15 | |
Hang on, it's the Pacific, it's the sea! | 0:49:43 | 0:49:45 | |
You should have your bikini on, we should be there in swimming trunks! | 0:49:45 | 0:49:48 | |
We've made it. | 0:49:48 | 0:49:51 | |
-This is the ocean, we've made it. -Fantastic! | 0:49:51 | 0:49:54 | |
So, Atlantic to Pacific. | 0:49:54 | 0:49:58 | |
It's not quite journeys' end. | 0:50:00 | 0:50:04 | |
The team have chosen this particular destination to explore | 0:50:04 | 0:50:08 | |
a surprising relationship between life and the Pacific wind. | 0:50:08 | 0:50:12 | |
-What's that there!? -Ah, yes! | 0:50:14 | 0:50:17 | |
-What is it then go on? -A Blue Whale. | 0:50:17 | 0:50:19 | |
-Is it really? -Really. | 0:50:19 | 0:50:20 | |
-I've never seen a Blue Whale before. Look at that. -Wow! | 0:50:20 | 0:50:25 | |
-Hang on, there's more than one. -There's two of them. | 0:50:25 | 0:50:30 | |
These are just the first indications of what they have come to see | 0:50:30 | 0:50:35 | |
because the wind can make habitats in the ocean too. | 0:50:35 | 0:50:38 | |
This is Monterey Bay, California. | 0:50:45 | 0:50:48 | |
Beneath its gleaming surface is a uniquely fertile eco system... | 0:50:51 | 0:50:55 | |
..that makes this one of the most biodiverse habitats in the earth's oceans. | 0:50:58 | 0:51:02 | |
-There you go, there you go. -There's two more of them right there. | 0:51:22 | 0:51:25 | |
-The charismatic megafauna. -Charismatic megafauna. | 0:51:25 | 0:51:29 | |
Chris and Andy have joined local marine biologist, | 0:51:29 | 0:51:33 | |
Steve Lonhart, to understand how this rich environment is | 0:51:33 | 0:51:37 | |
created by the wind. | 0:51:37 | 0:51:39 | |
If you can imagine the wind which is coming from | 0:51:41 | 0:51:43 | |
the northwest, so kind of over our shoulder, moving in this direction. | 0:51:43 | 0:51:47 | |
As it moves that way, | 0:51:47 | 0:51:50 | |
it actually just pushes the warm waters of the surface off, | 0:51:50 | 0:51:54 | |
and then you get this really cool nutrient rich water that's coming | 0:51:54 | 0:51:57 | |
up from the bottom, right where we are, right here, coming up from | 0:51:57 | 0:51:59 | |
the bottom and that's sort of like...you can think of it like fertiliser. | 0:51:59 | 0:52:03 | |
Meaning dead sea lions, dead kelp, | 0:52:03 | 0:52:06 | |
anything that dies, birds, all falls to the bottom? | 0:52:06 | 0:52:09 | |
Falls to the bottom, | 0:52:09 | 0:52:11 | |
and it is broken down into all its little constituent members, | 0:52:11 | 0:52:15 | |
that eventually just dissolve into the water. | 0:52:15 | 0:52:18 | |
When the water comes up, its clear, which allows things like kelp | 0:52:18 | 0:52:22 | |
and seaweeds, to do what they do which is photosynthesise. | 0:52:22 | 0:52:26 | |
Just like plants on land nitrogen, | 0:52:26 | 0:52:28 | |
carbon, building blocks of life. | 0:52:28 | 0:52:30 | |
And instead of those things being in the air and the soil, | 0:52:30 | 0:52:33 | |
-they're dissolved in the water. -That's right. | 0:52:33 | 0:52:35 | |
Then you have a forest, not on land, | 0:52:35 | 0:52:37 | |
it's actually on the shore. | 0:52:37 | 0:52:39 | |
To see the result of this process in its full majesty you have to | 0:52:43 | 0:52:47 | |
look beneath the surface... | 0:52:47 | 0:52:49 | |
..and to the unique environment that it creates. | 0:52:50 | 0:52:53 | |
The forest of giant kelp. | 0:53:07 | 0:53:09 | |
Not only does the kelp benefit from the nutrients drawn | 0:53:12 | 0:53:15 | |
up from the depths, | 0:53:15 | 0:53:17 | |
it is also bathed in the energy of the sun, allowing it to | 0:53:17 | 0:53:21 | |
reach 175 feet in height. | 0:53:21 | 0:53:24 | |
Ah, so these are the giant kelp. | 0:53:29 | 0:53:33 | |
You see the little bubbles? | 0:53:37 | 0:53:40 | |
Awesome, and that's what holds the giant kelp up. | 0:53:40 | 0:53:43 | |
-Chris, this is Andy. -Go ahead. Over. | 0:53:52 | 0:53:58 | |
Every square inch of this entire system all the rocks, | 0:53:58 | 0:54:05 | |
the nooks, the crannies - are all teeming with life. | 0:54:05 | 0:54:09 | |
There's not a square inch that's left bare and barren. | 0:54:09 | 0:54:14 | |
There's life everywhere. Outstanding again. | 0:54:14 | 0:54:22 | |
How does this compare with other dives you've done? | 0:54:24 | 0:54:29 | |
This whole place is like a normal sort of temperate | 0:54:29 | 0:54:33 | |
reef but just much, much, much bigger. | 0:54:33 | 0:54:38 | |
Everything has been super-sized. | 0:54:38 | 0:54:40 | |
It's huge. | 0:54:44 | 0:54:45 | |
It seems like all the life | 0:54:47 | 0:54:48 | |
down there is scaled-up enormously because of this nutrient-rich water. | 0:54:48 | 0:54:54 | |
I've just seen the biggest anemone I've ever | 0:54:57 | 0:55:01 | |
seen in my life. It's huge. | 0:55:01 | 0:55:06 | |
I've never seen an anemone that I would consider a man-eater, | 0:55:06 | 0:55:11 | |
but if there ever was one, this is it. | 0:55:11 | 0:55:14 | |
This is probably the best sight so far. I'm coming up. | 0:55:17 | 0:55:21 | |
I'm rising up the trunks of these huge, giant kelp. | 0:55:21 | 0:55:26 | |
Whilst this may be a very special environment, it also | 0:55:31 | 0:55:35 | |
vividly demonstrates the power of the atmosphere to reach into every | 0:55:35 | 0:55:40 | |
corner of the planet and make it a place for life. | 0:55:40 | 0:55:44 | |
For me, it really provides an insight into just how complex the atmosphere is. | 0:55:50 | 0:55:56 | |
It's not just something that we breathe and that produces | 0:55:56 | 0:55:59 | |
weather, it has the ability to shape the landscape underneath it. | 0:55:59 | 0:56:04 | |
It plays a huge part in forming the environments in which we all live. | 0:56:04 | 0:56:08 | |
Reaching the Pacific brings to an end what has been an extraordinary | 0:56:14 | 0:56:18 | |
and unique adventure. | 0:56:18 | 0:56:20 | |
This epic journey coast to coast | 0:56:22 | 0:56:25 | |
has enabled the team to experience the atmosphere as never before. | 0:56:25 | 0:56:29 | |
That's the one I want! That one! | 0:56:29 | 0:56:33 | |
They've explored the extraordinary processes that generate weather... | 0:56:33 | 0:56:39 | |
-20 million. -So, that small cloud weighed four tonnes? -Yes. | 0:56:39 | 0:56:43 | |
-That's incredible. -It is. | 0:56:43 | 0:56:46 | |
..they've seen some of the many ways that life - at every scale | 0:56:46 | 0:56:50 | |
from microscopic bacteria... | 0:56:50 | 0:56:53 | |
Now we are sucking in the cloud. | 0:56:54 | 0:56:57 | |
..to more familiar species exploit each level of the atmosphere... | 0:56:58 | 0:57:03 | |
Good luck, little one. | 0:57:05 | 0:57:06 | |
These waterfronts, they are vital for movement, | 0:57:06 | 0:57:09 | |
not just on a small scale, but on a global scale. | 0:57:09 | 0:57:12 | |
..and they've revealed the often complex mechanisms by which | 0:57:22 | 0:57:25 | |
we, ourselves, are shaping this realm. | 0:57:25 | 0:57:29 | |
-Cheers, everyone! -Cheers, guys. | 0:57:54 | 0:57:56 | |
-Cheers! -To the Pacific! | 0:57:56 | 0:58:00 |