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PLANET EARTH: OUR LOVING HOME:
Our Oceans and the Global Climate: A Deep Interconnection - P2/2
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Greetings, informed viewers,
to today’s episode
of Planet Earth:
Our Loving Home,
the conclusion of a two-part
series, focusing on
the deep interconnection
between our oceans
and the world’s climate.
Oceans cover 71% of
the Earth’s surface,
contain approximately
97 % of the world’s water,
sustain a diverse array
of sea life and play
a vital role in regulating
our planet’s climate
in a multitude of ways –
including through
thermohaline circulation,
also known as the
Great Ocean Conveyor
which absorbs
large quantities of heat
and carbon dioxide.
Last week in part one,
we saw the different ways
in which the oceans
stabilize the climate,
but the relationship
is not one way.
Today we’ll examine
how climate change
increases sea levels
and some of
the possible consequences
that our world faces
from this process.
The experts featured today
Dr. Claude
Hillaire-Marcel,
a Canadian geoscientist
from the University
of Quebec at Montreal,
Professor
Anders Levermann,
a senior researcher at
the Potsdam Institute of
Climate Impact Research
in Germany and
the lead author of
the Sea Level Change
chapter for the coming
5th Assessment Report
of the United Nations
Intergovernmental Panel
on Climate Change (IPCC)
and Dr. Ted Scambos,
senior research scientist
at The National Snow and
Ice Data Center (NSIDC)
at the University
of Colorado, USA.
The major drivers
of advancing sea levels
are the thermal expansion
of seawater and the melting
of ice caps and glaciers
due to global warming.
We’re disturbing
the climate system with
a temperature increase,
and the higher
the temperature increases,
the more disturbance
we introduce and therefore
the risk increases,
I would say.
Sea level can rise by
the expansion of water
when it gets warmer.
That’s the simple part.
We know the physics
and the big question is
only how deep
it’s mixed down in the sea,
so how many layers
are expanding, really.
So we have several
feedbacks which we are
unraveling now,
both the ice shelf
melting feedback,
and melting in
the Arctic sea ice, which
leads to a warmer ocean
and a change in climate
in the Arctic.
The acceleration
of glaciers
seems to be accelerated
by the presence
of a little bit of melting,
which leads
to further sea level rise.
We know we’re going
to be pushed in
this direction of a climate
that we have not seen
in several million years.
Many scientists point out
that the future
sea level rise estimates
made in the 2007
4th Assessment Report
of the Intergovernmental
Panel on Climate Change
were far too low,
with the revised forecasts
pointing to danger ahead
for low-lying areas.
In its last assessment,
this group used
several climate models,
but all these models failed
or were too conservative
to really predict
the evolution
of the recent few years
in terms of sea level rise.
The sea level is rising
faster than these models
predicted in terms of
the shrinking of
summer ice in the Arctic.
There is less ice
in the Arctic in summer
than these models predicted
for the last few years.
I’m one of the lead authors
of the next report
of the Intergovernmental
Panel on Climate Change
on this specific
sea level chapter.
There we will
have to try to make
a very thorough analysis
of the sea level.
The last IPCC report
was good
but the sea level was
a clear underestimation
of what we have to expect
in the future.
The reason I say this is
that the last IPCC report
said, in the next century
we’re going to get
20 centimeters
to 60 centimeters
in sea level rise globally.
Now, in the last century,
we had 15 to 20
centimeters already.
The 20 to 60
for the next century
came from
the different scenarios
that we could have,
the different
global warming paths
that we might be on.
In the period from
where the projection
started in 2000, until
the report was published
in 2007, we had already
underestimated
the observed sea level
by 40%.
If you do already
the first seven years
by 40% wrong,
it’s almost half wrong.
So, the reason was simply
that we didn’t have
enough proper models
for the great ice sheets in
Greenland and Antarctica.
These are the unknowns.
We will now pause
for a moment and
when we come back,
we’ll have more about how
the heating of our Earth
is causing
sea level changes.
Please stay tuned
to Supreme Master
Television.
Welcome back to today’s
Planet Earth:
Our Loving Home
on Supreme Master
Television
where we are examining
the important relationship
between the oceans
and our world’s climate.
During the past century,
the global
average sea level
rose at a rate of about
1.7 millimeters per year.
The current average is
3.1 millimeters per year.
With the warming
of the planet
and the melting glaciers
and ice sheets,
one forecast by a UK and
Finnish scientific team
pegs the average
global sea level
to advance by 0.8 meters
to 1.5 meters
by the end of the century.
Many major cities
around the world, such as
New York City, USA,
are at one meter or less
above sea level.
In the last ice age
we had 120 to 130 meters
less sea level compared
to the present day.
So, when you hear
that we had
15 to 20 centimeters
in the last century
of sea level change,
you get the feeling that
we are only talking about
centimeters all the time
and that sounds like
not so much. It is a lot.
The ice melt in Greenland
is important.
The Greenland ice sheet
is 3,000 meters thick.
To the sea level rising,
the most critical one
today is Greenland.
The last episode
with a warmer globe
than present was
about 125,000 years ago,
an interval which
geologists refer to
as the last interglacial.
During this interval
the Greenland ice sheet
was significantly reduced
because
there was drastically
different vegetation
in southern Greenland
than today.
So it means
that the southern part of
the ice sheet had probably
largely disappeared.
And there was still
a robust ice sheet,
but in the northern part
of the island.
And it is an interval when
the average sea level
was about four meters
above present. Okay.
Minimum. Okay.
Possibly more than
four meters but it's a very
conservative estimate.
So it means that we have
started now a process
leading to a fast melting
of part of this ice sheet,
of the Greenland ice sheet
due to global warming
that is potentially leading
to a higher sea level of
few meters above present.
In terms of how fast,
again, it’s very… you know
things accelerate.
So perhaps
a couple of years ago,
a few years ago
I would have said,
"Well, maybe
a few thousand years,"
to be prudent.
Ah, now,
it’s perhaps 2,000 years
to see a very fast rise
in sea level.
And well, it means
that’s, at our time scale,
that’s one generation
or two generations or
three generations, which
is our real concern now.
The rate
of sea level increases
may be fast enough
to lead to really critical
and difficult
to solve problems
in many countries
of the world. Ok.
Bangladesh for example
just to mention one.
The Antarctic is an
extremely sensitive area
with respect
to global warming.
A recent study from
the University of Toronto,
Canada found that if
a complete disintegration
of the Western Antarctic
Ice Sheet were to occur
due to climate change,
the Sheet’s sheer weight
could cause
Earth’s rotational axis
to shift by 500 meters.
The scientists also
concluded that
such an event would
cause an uneven global rise
in sea level with the
coastline of North America
seeing a six meter rise,
and the rest of the world
seeing about
a five meter rise.
In fact, the West Antarctic
Ice Sheet has collapsed
several times over
the last five-million years.
When they occurred
in the past,
that meant the collapse
of the West Antarctic
Ice Sheet and
three and a half meters of
sea level rise from there,
plus another
three and a half from the
East Antarctic Ice Sheet.
So there was
about seven meters
of sea level rise.
Greenland and Antarctica
each probably account
for about 25% of
the total sea level rise
and sea level rise rates
have been going up
since the last
20 or 30 years or so.
Prior to about again 1990,
the sea level rise rate was
something like between
one and two millimeters
per year.
Now the total
sea level rise rate is
between two and three
millimeters per year and
we’re just getting started
on this warming trend.
The problem is that
Greenland and Antarctica
have the ability
to contribute much, much
more ice to the ocean,
which would cause
the sea level rise rate
to increase very rapidly.
Warming of the oceans
will increase
as the pace of warming in
the atmosphere increases
but not at the rate
that Greenland and
Antarctica can increase
their contribution of ice
to the ocean.
So in the future, more
and more of sea level rise
will come from
the ice sheets relative
to the thermal expansion
of the oceans.
Which countries
will be most affected
by increasing sea levels?
Several island nations
such as
the Maldives, Kiribati
and Tuvalu are in danger
of soon disappearing
altogether.
The President
of the Maldives,
His Excellency
Mohamed Nasheed
is looking for places
to move his country’s
entire population
in anticipation
of such an event.
Professor Levermann’s
research has closely
examined this issue
in terms of consequences
for Europe
and North America.
What we found was
an increase mainly
along the American
and the European coasts.
The strongest increase
was around
the Greenland coast.
There are people living
there, so it's important,
the highly populated areas
up to Florida (USA),
or the entire US coast,
the same
for the European coast.
US researchers
recently did something
slightly different;
they projected
global warming
plus a weakening of the
thermohaline circulation.
They found the U.S. coast
was very strongly affected.
So these are
the main regions
that need to worry.
That's the East coast
of the U.S. and Canada
and potentially
the European coasts, too.
We sincerely thank the
respected Earth scientists
featured today for
their insightful research
on the relationship
between the oceans
and our global climate
and for helping us
better understand
increasing sea levels and
the serious consequences
for life on our planet.
For more details
on the scientists featured
on today’s program,
please visit
the following websites:
Dr. Claude Hillaire-Marcel
www.Professeurs.UQAM.ca
Professor
Anders Levermann
www.PIK-Potsdam.de
Dr. Ted Scambos
NSIDC.org
Eco-wise viewers,
thank you for joining us
on today’s Planet Earth:
Our Loving Home.
Coming up next is
Enlightening Entertainment
after Noteworthy News.
May we all live
sustainable lives
to protect the oceans
and curb climate change.
Mr. Laurent Imbault is
a noted Canadian actor
and comedian and
founder of GoodnessTV,
an Internet television station
that broadcasts
only good news.
Through online media,
Mr. Imbault seeks
to improve our world.
The idea is to create
a network of people
sharing ideas, sharing
know-how, knowledge,
experiences,
so that things can move
a lot faster than
they’re moving now.
So GoodnessTV
really wants to become
‘goodness network’
where people can
exchange all these ideas
and grow faster.
Watch the second
and final part of
"Laurent Imbault
and GoodnessTV:
Uplifting the World"
Sunday, August 8,
on Good People,
Good Works.
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