New Scientist - 14.09.2019

(John Hannent) #1

40 | New Scientist | 14 September 2019


of the life-support systems that have sustained
the Holocene.
The changes could be abrupt and
irreversible. We don’t know where things
may end up. If the Holocene is our desired
reference point – the stable planet we know
and depend on – we need to find out where
those thresholds are, thus identifying our safe
operating space. That is what our research on
planetary boundaries tries to do.

So what are these boundaries?
We identify nine. There are three that
operate at a planetary scale: the oceans,
the atmospheric climate system and the
stratospheric ozone layer. Each has thresholds
beyond which danger lies. There are four more
that we call biosphere boundaries. They help
regulate the planetary systems. They are
biological diversity, the hydrological cycle, land
cover such as forests, and the flows of nutrients
vital to life, such as nitrogen and phosphorus.
Finally, we identify two categories of alien
things that don’t exist naturally: novel entities
including nuclear waste and gender-bending
chemicals, and aerosol air pollution, which
alters Earth’s energy balance and impacts
regional climate systems such as the
south Asian monsoon.

How do we know when we have crossed a
planetary boundary?
Our scientific understanding of Earth systems
has advanced tremendously over the past
30 years, but still we don’t know exactly where
the critical boundaries are for these systems.
So we apply a precautionary approach. We
identify safe zones and high-risk zones.
Between them, uncertainty ranges, within
which we don’t know what might happen.
We place the planetary boundary at the
lower levels of the uncertainty ranges.

What is the boundary for climate change,
for example?
For climate change, we chose the atmospheric
concentration of the most important
greenhouse gas, carbon dioxide. We
assessed the uncertainty range as being
between 350 and 450 parts per million,
so the planetary boundary is 350 ppm.
The world is now well above that, at 410 ppm,
and we are starting to see dangerous impacts.
In the oceans, there is heating, a slowing down
of the Gulf Stream and accelerated Arctic sea-
ice melting. In the atmosphere, we see a
serious impact on the jet stream and many
more extreme weather events. All these effects
may foreshadow the breakdown of other

systems, such as the hydrological cycle and
biodiversity. We are already into the high-risk
zones for biodiversity and nutrients.

Your critics say you don’t properly distinguish
between global and local systems.
Of course, before you reach any of our
planetary boundaries, you can have massive
problems locally. Lakes dry up, rivers fill with
pollution, ecosystems collapse and so on.
But when we talk about keeping within a safe
operating space, we mean safe for the planet
as a whole, not for every human or every
ecosystem. Even so, apparently local problems
can go global, especially if they occur widely.

Which problems have gone global in this way?
Water seems very local, for instance, but
there is a global hydrological cycle that is the
bloodstream of the biosphere. Take away the
rain and forests die, triggering massive releases
of carbon into the atmosphere and loss of
biodiversity. Or take away a major forest like

CLIMATE
CHANGE

Nitrogen
cycle

Phosphorus
cycle

BIOGEOCHEMICAL
FLOWS

NOVEL ENTITIES
Chemical pollution and
substances that don’t
exist naturally
(boundary to be
determined)
?
?

?


STRATOSPHERIC
OZONE

OCEAN
ACIDIFICATION

FRESHWATER
USE

CHANGE IN
LAND USE

ATMOSPHERIC
AEROSOL LOADING
(boundary to be
determined)

BIODIVERSITY

Extinction
rate

Below boundary (safe)

Biodiversity
intactness
(boundary to be
determined)

Overstepping the mark
We have already gone beyond four of the nine proposed safe operating levels for
humans on Earth, know as planetary boundaries

In zone of uncertainty (increasing risk)
Beyond zone of uncertainty (high risk) Outer boundary of safe zone
Start of high-risk zone

Johan Rockström is a global
sustainability expert whose research
focuses on water in tropical regions.
He is a former director of the Stockholm
Resilience Centre and is now co-director
of the Potsdam Institute for Climate
Impact Research in Germany

MIKAEL AXELSSON
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