Business on the Edge 2024
Page 17 of 77 · WEF_Business_on_the_Edge_2024.pdf
2.1 Our planet’s life-support systems
are severely threatened
2.2 Five Earth systems are at imminent
risk of tipping today While some effects of the nature and climate crisis
are already apparent today, other more serious
consequences are on the horizon. The science
is clear that risks are mounting but the precise
timing and magnitude of the impending changes
are difficult to specify, given the complexity and
interdependencies of Earth systems and their
tipping points.A tipping point is a critical threshold that, when
reached, leads to a significant change in the state
of the system that is typically irreversible.25 Given
their scale, the degradation and tipping of Earth
systems pose grave threats to the future of our
species, affecting liveability and survivability in
many geographies around the world. Crossing an
Earth system tipping point “will severely damage
our planet’s life-support systems and threaten the
stability of our societies”, according to the authors
of the Global Tipping Points Report 2023.26
At present levels of global heating, five Earth
systems are close to crossing tipping points:27
–Greenland ice sheet collapse
–West Antarctic ice sheet collapse
–Warm-water coral reef die-off
–Labrador & Irminger Seas convection collapse
–Boreal permafrost abrupt thaw28
Land ice on the Greenland and West Antarctic
ice sheets – melting rapidly and close to crossing
tipping points – represents 10 metres of sea-level
rise29 with unavoidable rises already locked in.30
Communities around the world are experiencing
the effects of coastal erosion, flooding and storm
surges. Some 630 million people live on land lying
below projected annual flood levels for the end
of the century.31 The displacement of so many
people could lead to a global security crisis, with increased competition for freshwater, land and
other resources.
For more information on risks to land ice, the chain
of geographic reactions unlocked when it melts and
the global consequences of its decline and tipping,
refer to Figure 8.
Sea ice is showing marked signs of deterioration.
Regardless of emissions scenarios, there is likely
to be at least one sea-ice-free summer in the Arctic
before 2050. Decreased sea ice extent creates a
feedback loop that amplifies warming, because
darker water absorbs a greater amount of solar
radiation compared with reflective, white sea ice.
Amplified Arctic warming destabilizes the polar jet
stream which could lead to increased temperature
extremes at lower latitudes.
For more information on risks to sea ice, the chain
of geographic reactions unlocked when it melts and
the global consequences of its decline and tipping,
refer to Figure 9.
The Greenland
and West Antarctic
ice sheets – close
to crossing their
tipping points –
represent 10 metres
of sea-level rise with
unavoidable rises
already locked in.
17 Business on the Edge: Building Industry Resilience to Climate Hazards
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