KATHLEEN WENDT: Extreme climate events
are happening all over the world.
They are becoming more common and more severe.
To help us deal with these challenges,
we need to understand the causes.
CRYSTAL KOLDEN: In just the last decade, 2010 to 2020,
we saw the hottest decade ever.
RALPH KEELING: You look at the data
and you can't deny that humans are having a profound impact
on the whole planet.
KATHLEEN WENDT: It's only by understanding the science
will we find the solutions.
ASMERET ASEFAW BERHE: It's a lot of work,
but it also comes with a number of opportunities.
KATHLEEN WENDT: If the past teaches us anything,
it's that now is a better time than ever
to start making major changes.
CRYSTAL KOLDEN: In 2020, we had the largest number
of mega-fires across the Western US that we've ever seen.
When we have multiyear droughts that
then leave behind an enormous amount of dead downed wood,
when an ignition does occur, there's
an enormous amount of fuel.
It allows for incredibly explosive growth.
That spreads the fire quickly across the landscape.
We just didn't see these mega-fires 20, 30 years ago.
And now we're seeing them annually.
KATHLEEN WENDT: The drought's driving
these mega-fires are occurring at a time
that the Earth is warming.
ASMERET ASEFAW BERHE: We've been monitoring
atmospheric temperatures around the world since the 1880s,
and the global average temperature
has changed by about 1 degree centigrade since then.
KATHLEEN WENDT: What is driving this rise?
To answer that, we need to understand the factors that
control Earth's temperature.
ASMERET ASEFAW BERHE: There are three factors.
The intensity of solar radiation,
the composition of the Earth's atmosphere,
and the reflectivity of the ground surface or albedo.
Scientists have continuously been
monitoring solar radiation and the surface
reflectivity for decades now.
And we know that those haven't changed significantly enough
to contribute to warming our planet.
KATHLEEN WENDT: So that leaves the atmosphere.
How does it affect temperature?
ASMERET ASEFAW BERHE: So the sun is the dominant source
of energy on Earth.
When solar energy comes down to the Earth, some of it
is reflected back from reflective surfaces.
Some of it is absorbed by the ground surface
and is re-radiated back to the atmosphere as infrared energy.
Gases, such as carbon dioxide, methane,
or water vapor that accumulate in the Earth's atmosphere,
they're absorbing that irradiated heat
and are able to trap that heat and cause
warming of our planet.
And that's what we call the greenhouse effect.
KATHLEEN WENDT: Has the atmosphere
been changing in a way that could explain
the increase in temperatures?
To find out, scientists need to measure the greenhouse gases,
especially carbon dioxide, which is one of the most
abundant in our atmosphere.
RALPH KEELING: Charles David Keeling
pioneered the measurement of carbon dioxide
with higher accuracy than it had ever been done before.
And he was my father.
He went by Dave.
KATHLEEN WENDT: Dave started taking air samples
in the mid-1950s with glass flasks.
RALPH KEELING: This flask that's been evacuated, so there's
no air in it nothing.
So what you do to take an air sample is holding our breath,
and then we just turn this stopcock,
and the air just rushes in.
So this flask, it'll be placed on this rack and then analyzed,
and that allows you to very accurately measure
how much carbon dioxide is in the air.
Among the places he started making measurements
was Mauna Loa, which is on the Big Island of Hawaii.
It allows you to sample air that's
representative of a large part of the atmosphere.
KATHLEEN WENDT: Keeling's first monthly reading
was 315 parts per million.
That means for every million molecules of air, 315 of them
were carbon dioxide.
From March 1958 to March 1959, daily air measurements
were taken.
RALPH KEELING: So the carbon dioxide went up to a peak
and then came down and then came up again.
KATHLEEN WENDT: What could cause this pattern to occur?
RALPH KEELING: In the spring and summer, plants leaf out,
and they take up CO2 from the atmosphere,
and that produces a drawdown.
And then in the fall and the winter,
CO2 is being released back, because there's
decomposition going on.
And that brings CO2 back up again.
He was seeing the breathing of carbon dioxide
in and out of the atmosphere caused by vegetation
in the northern hemisphere.
KATHLEEN WENDT: Within the first few years, the same carbon
dioxide seasonal cycle appeared, but another pattern
began to emerge.
RALPH KEELING: He could see that the CO2 overall was rising.
Mauna Loa was only one piece of it.
There was also measurements being
made on ships and airplanes and particularly at the South Pole
all documenting, very clearly, this rise.
The program my father started, which I continue
involves keeping the measurements
going at Mauna Loa.
But we also take air samples from around the world,
so we get a large scale view of how CO2 is varying.
In the late '50s when my father started,
the concentrations in the atmosphere
were around 315 parts per million.
And they're now over 100 parts per million above that.
Today, we're recording concentrations around 415 parts
per million.
We are still marching upwards.
KATHLEEN WENDT: Carbon dioxide levels in the atmosphere
are increasing dramatically.
But is this a new phenomenon?
And in order to answer that, we have to look into the past.
So we use ice cores.
So when we drill into these Antarctic ice
sheets over a mile deep, these long ice cores
allows us a window into the past.
When it snows every year, little packets
of air that are in between the individual snowflakes
get trapped as bubbles.
These snow layers build up on top of each other.
The further we drill down, the older the ice.
And so far, we've been able to drill down to ice
that is 800,000 years old.
Polar ice kind of is like a constellation of bubbles.
And trapped inside each of these bubbles
is fossil air that's been trapped since that ice formed.
And they allow us to study what greenhouse gas concentrations
were in the past.
So we place a sample of Antarctic ice in a glass flask,
and then we vacuum away all of the modern air.
Then we left the Antarctic ice melt,
and the tiny bubbles that are trapped inside the ice
are released into the vacuum.
We can measure what the greenhouse gas
concentrations were at the time of this bubble formation.
Going back 800,000 years ago, we see fluctuations
in carbon dioxide concentrations over time,
from about 180 parts per million up to 300 parts per million.
And then we reach a period of the Industrial Revolution,
CO2 concentrations begin to gradually rise.
And over the last 30 years, we've
seen a skyrocket of CO2 concentrations
up to the point of 415 parts per million.
Ice cores can also tell scientists
about past temperatures.
So by analyzing the water molecules
in the ice of these ice cores, we
can determine what the past temperature of the poles was.
So when we plot the carbon dioxide
record and the temperature record
going back 800,000 years, whenever
there is a fall or rise in CO2 concentrations,
we see an associated change in temperatures.
And this tells us that throughout Earth's history,
temperature and CO2 concentrations are intimately
linked.
This rise in carbon dioxide is causing a rise
in global average temperatures.
And this rate is completely unprecedented-- it's
something we've never seen over the course of human history.
What is causing it?
The carbon atom can help us find out.
Carbon always has six protons.
Now, most carbon also has six neutrons in its nucleus,
and that gives it a mass of 12.
We refer to it as carbon-12 some.
Carbon however, has seven neutrons.
And so that has a mass of 13, and we call it carbon-13.
The different varieties of carbon and carbon dioxide
allow us to determine whether the CO2 comes from plants,
volcanoes, or the oceans.
Plants prefer to take up carbon-12 for photosynthesis.
And so what happens is that this plant matter
is made up of much, much more carbon-12 than carbon-13.
This carbon-12 preference creates a distinctive ratio,
which is also in the carbon dioxide released
when plants die or are burnt.
The carbon dioxide coming from volcanoes and oceans
has a different ratio.
Over the past century, the carbon-13 to carbon-12 ratio
in the atmosphere has become more and more
like the ratio found in plants.
But how?
Fossil fuels are made of ancient plants.
And so when we dig them up and burn them,
we're emitting more and more carbon-12 into the atmosphere.
And this is changing the carbon-13 to carbon-12 ratio
within the atmosphere.
This tells us definitively that the rise in CO2 concentrations
that we're observing today is due to the burning
of fossil fuels.
The past 250 years of burning fossil fuels
has caused global average temperatures
to rise by 1 degree Celsius, which
is creating massive disruptions across the planet.
CRYSTAL KOLDEN: When we trap more heat in our atmosphere,
that energy is what actually translates into extreme events.
So if we continue to burn fossil fuels,
we will see an increase of 3 to 5 degrees Celsius
over the next century, increasing mega-fires that
are incredibly destructive.
When you couple sea level rise with events like hurricanes
and typhoons, across the globe, you
have millions and millions of people, animals, and plants
that are likely to be displaced.
RALPH KEELING: If we don't bend this curve,
we're not in a good place.
It is something that humans created, this rise.
And we're in a position to do something about it.
KATHLEEN WENDT: To stop carbon dioxide
from increasing further, we need to reduce or eliminate
the burning of fossil fuels.
ASMERET ASEFAW BERHE: And that has
to mean converting our energy sources
in all aspects of our lives--
in industry and agriculture and transportation
into renewable systems as soon as possible.
This transition also brings a number
of opportunities for green jobs and green technology.
And the same time, we also have to draw down
some of the carbon dioxide that's
already in the atmosphere.
Another major solution to draw down the carbon dioxide
lies right under our foot, and it's soil.
Soil is one of the major reservoirs of carbon
in the Earth's system.
If we can actually transform our agricultural practices
to reduce tilling and reduce disruption of the soil,
we can offset a third of the current emissions
of fossil fuels into the atmosphere with soil carbon
sequestration.
We have the solutions for climate change.
What we need now is a large number
of people to have the will to put those solutions in place
and act to address the climate crisis.
[MUSIC PLAYING]
SINGER: (SINGING) We have solutions, oh oh oh.
We have the power, ah ah ah.
This is our future, we're in this together, together.
We can do this, save our planet.
This is our future, now or never.
Clock is ticking.
Time for action.
We'll [INAUDIBLE] we'll find a way together.