Cornell Trieste CLEWS modelling October 2013
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Transcript of Cornell Trieste CLEWS modelling October 2013
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Sarah Cornell Stockholm Resilience Centre
Joint ICTP-IAEA Advancing Modelling of Climate, Land-use, Energy & Water (CLEW) Interactions
9 October, 2013
Characterizing a “safe operating space”
for humanity
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The Gaia Hypothesis –
our planet functions as a single “organism” that maintains the conditions
necessary for its survival.
James Lovelock
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The Earth system science perspective …
• The Co-evolution of Climate and Life, Schneider and Londer (1984)
• NASA Earth system science overview (1988) – the Bretherton diagram
• International Geosphere-Biosphere Programme (IGBP) founded 1986
• The Amsterdam Declaration on Global Change (2001) and the Earth System Science Partnership
• Future Earth (2013– )
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Excerpts from the Amsterdam Declaration on Global Change (2001):
• The Earth System behaves as a self-regulating system comprised of physical, chemical, biological and human components…
• Human activities are significantly influencing Earth's environment in many ways in addition to greenhouse gas emissions and climate change…
• Earth System dynamics are characterised by critical thresholds and abrupt changes…
• The Earth is currently operating in a no-analogue state.
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The “Bretherton Diagram” (NASA 1988) set out the observational, conceptual and computational modelling framework for 1-2 decades of global change research.
Spot the human...
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IPCC AR5 WG I SPM, 2013
Carbon cycle Dynamic vegetationCloud & aerosol chemistry“Green ocean”
AtmosphereLand surfaceOceansSea-iceSulfur cycle (sulfate aerosol)
Incr
easi
ng c
ompl
exit
y
1960s
Present day
Climate modeling
Earth system modeling
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Towards a new geological era:
The Anthropocene
0
-4
-8
Time, thousands of years ago
Cha
nge
in t
empe
ratu
re
from
pre
sent
day
, °C
Plot shows GRIP ice core O18 isotope data – a measure of past air temperature
Holocene
Homo sapiens living in Asia… … in Australia and Europe
Neolithic revolution – first villages and farming
Roman empire
Steffen, Crutzen and McNeill (2007) The Anthropocene: are humans now overwhelming the great forces of Nature? Ambio
100 80 60 40 20 0
many glacial periods through history
The 2°C global warming policy target Humanity’s trajectory?
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From Steffen et al. 2004
TheAnthropocene
The changing humanenterprise,
from 1750 to 2000
The period from 1950 to 2000 is often called
The Great Acceleration
Population GDPForeign
investment
River dams Water use Fertilizer use
McDonaldsPaper useUrban pop.
Motor vehicles Telephones Intl. tourism
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TheAnthropocene
The human imprinton the
global environment, from 1750 to 2000
From Steffen et al. 2004
Atmos CO2 Atmos N2O Atmos CH4
Ozone depletion
NH mean temperature
Severe floods
Fisheries exploitation
Coastal infrastructure
Coastal biogeochem
Tropical forest loss
Cultivated land Extinctions
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The Planetary Boundaries
Method?Assumptions?Evidence base?Issues for debate?
J. Rockström and 28 co-authors (2009), Feature published in Nature
Article published in Ecology & Society
Concept taken up by UN High-Level Panel on Global Sustainability
(Rio + 20), UNEP, EEA, WEF, World Bank, NGOs such as Oxfam, and
many other policy arenas.
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The Planetary Boundaries
Method? Expert deliberation
Assumptions?A well-characterized HoloceneDynamic system can be represented with static measures
Evidence base?Earth observation, models/theory, palaeo records – but “in silos”
Issues for debate?Cross-scale interactions, thresholdsArbitrariness of boundaries risk/impactRole of scientific expertise in governance
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The proposed boundaries and their ‘control variables’:
Rockström et al. (2009)
Climate change CO2 concentration and radiative forcing
Ocean acidification Surface ocean CO32- saturation state
Stratospheric ozone depletion Ozone concentration
Perturbed biogeochemical flows (nitrogen and phosphorus)
Human-induced phosphorus inflow to ocean; Human fixation of atmospheric N2 to bioavailable forms
Global freshwater use Annual volume of water used in human activities
Land system change % land converted to cropland
Biodiversity loss Global species extinction rate
Chemical pollution Not quantified (concentrations and effects considered)
Atmospheric aerosol loading Not quantified
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Figures from IPCC AR5 WG I SPM (2013)
Trend (°C over period)
proposed planetary boundary = 350 ppm
Climate and CO2
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Ocean acidification (the other half of the CO2/climate problem)
Upper figure from IPCC AR5, lower figure from Ricke (2013)
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Biodiversity loss (using Mean Species Abundance)
Figure from Alkemade et al. 2009
Proposed boundary
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Ecological changes • are seen to be widespread • influence biophysical feedbacks (“Gaia”)• are under-monitored and weakly managed
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Chemical Pollution
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Chemical PollutionImage/links: http://news.bbc.co.uk/2/hi/science/nature/4083331.stm
Global problem? Yes (but surprisingly hard to find global data…)
Earth System impacts? Yes (as seen in CFCs/ozone and in “PBT” chemicals)
Holocene baseline? Zero… Chemical pollution is a full complexity problem,
in a system with purpose and intentionality.
Also see Persson et al. 2013, Env Sci Tech
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Land cover change (from forest to other land cover)Figure from Hansen et al. 2010
Observed forest cover in 2000
Observed forest loss 2000-2005
These bands of forest play an important
biophysical role in the Earth system(albedo, hydrology,
carbon cycling)
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January 2000
August 2000
Water Use“Withdrawal Index” – how much is withdrawal tapping into ecological flow resource?
(work in progress, PIK-SRC collaboration – Gerten, Pastor et al.)
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Atmospheric aerosol
Complex behaviour – • Direct and indirect radiative forcing• Direct and indirect ecosystem effects
Figure from NASA GISS
Planetary effects?• Hydrological cycle• Biome shifts• AlbedoChanging weather patterns, e.g., monsoons, convective rains
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Biogeochemical perturbation from nutrient releases
Figure from WRI, using data from Diaz and Rosenberg 2008
Local problem turned global?What about human needs?
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AtmosphereLand surfaceOceansSea-iceSulfur cycle (sulfate aerosol)Carbon cycle Dynamic vegetationCloud & aerosol chemistry“Green ocean”
Incr
easi
ng c
ompl
exit
y1960s
Present day
Climate modeling
Earth system modeling
Incr
easi
ng c
ompl
exit
y So what’s missing from these
high-complexity models?
(and why?)
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“Integration” of different types of knowledge remains a challenge.
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Earth’s mechanisms are
not clockwork
Apollo 11 image, July 1969
Humans are not just observers of the system
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Information and data gaps
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Visualization: J. Friedrich (WRI)
Complex connections
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Jickells et al., 2005
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Modeling: J. Donges et al 2013
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31
Navigating the global community’s
Safe Operating Space…
“The problem is the idea that the planet has a cockpit, and in that cockpit, we can change course.
The planet doesn’t work like that”Maarten Hajer, PBL Netherlands
But what are we doing all this for?
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Human uses social structures global connections
AHDR 2004, 2013ACIA 2005
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Once upon a time two planets met. One seemed very healthy and the other seemed very sick with its face mutilated by a rash…So the healthy one asks the sick one, ”Hey - what happened to you since we last met?" And the sick one answers, "Well, I am really sick… I have a strange disease called homo sapiens."
The healthy planet answers, "Ah, never mind – it's a
minor problem. I had it once and it disappeared by itself".
Alexander Likhotal
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=Re-Invention of
Global Environment
Macro-Engineering=
Macro-Mitigation(including large-scale renewables schemes)
+Macro-Adaptation
(landscape redesign, eco-migration corridors, river diversion, coastal reconstruction, sea level management, etc.)
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DemandCosts & Benefits
Human Well-Being
Natural & Managed
Ecosystems
Brundtland 1987: “harmony among humans
and between humans and nature”
Sustainability is fundamentally simple – humanity’s search for wellbeing in the world
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Costs & Benefits
DemandCosts & Benefits
Industrial Metabolism
Demand
Emissions
Impacts
Impacts
Risk
s
Climate & Earth System
Dynamics
Human Well-Being
Natural & Managed
Ecosystems
Impacts
Radiative Forcing
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Costs & Benefits
DemandCosts & Benefits
Industrial Metabolism
Demand
Impacts
Impacts
Risk
s
Climate & Earth System
Dynamics
Human Well-Being
Natural & Managed
Ecosystems
Impacts
Perc
eptio
ns
Strategic
Decision Making
EmissionsRadiative Forcing
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Costs & Benefits
DemandCosts & Benefits
Industrial Metabolism
Demand
Impacts
Impacts
Risk
s
Climate & Earth System
Dynamics
Human Well-Being
Natural & Managed
Ecosystems
Impacts
Perc
eptio
ns
Strategic
Decision Making
EmissionsRadiative Forcing
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Geoengineering
Costs & Benefits
DemandCosts & Benefits
Industrial Metabolism
Impacts
Impacts
Risk
s
Climate & Earth System
Dynamics
Human Well-Being
Natural & Managed
Ecosystems
Impacts
Perc
eptio
ns
EmissionsRadiative Forcing
Mitigation
Adaptation
Education
Compensation
Disaster Manageme
nt
Conservation
Investment
Adaptation
Strategic
Decision Making
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information that is
• Relevant,
• Robust,
• Rough & ready,
• Reproducible
systems-level wisdomwithout perfect
subsystem-level knowledge
Our models need to provide
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Integration of knowledge is a challenge
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Today’s questions -• When “everything is changing fast”, what can
we be sure of?
• What is the basis for action in the context of change (especially when we are not sure)?
• Whose knowledge? Whose action? Whose sustainability?
Governance = the various ways that society steers itself
state
civil society
private sector
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• New integrated assessments that link social and ecological change
• Avoiding inadvertent ‘iatrogenic’ risks – ie, safeguards on policies so that the cure is not worse than the disease…
• Engagement and input from wider interests
• Embedding the plurality of values
Good or bad governance?
Precaution – Provisionality – Participation
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Global Responsibility?
• Researchers need to engage in social debates
• Researchers need to be policy-literate• Polymaths need to reflect on what they do
and how they do it:– Values – Practices
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Not conclusions (perhaps discussion points)
• Research challenges: knowledge integration, describing the state of the (whole) world
• Governance challenges: “one vision?”, history, expanding network of actors
+ BIG real-world challenges where these issues meet