Assessing Threats from Natural Disasters and Climate...
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Assessing Threats from Natural Disasters and
Climate ChangeMarc A. Levy
CIESIN, Earth InstituteColumbia University
World Data Center for Human Interactions in the
Environment
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Why it matters
1. More people are living in harm’s way2. There are more harms on the way3. The patterns are uneven, and surprising
catastrophes are likely4. There are no easy responses – it will take
sustained, coordinated, focused effort
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1) More People are Living in Harm’s Way
Breakthroughs in how georeferenced data can be processed, integrated and analyzed make it possible to characterize natural disaster risks much more precisely than before
We try to focus on risks from multiple hazards
We try to focus on multiple impacts – disasters can affect- development - conflict potential- humanitarian crises- public health- migration
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Global Natural Disaster “Hotspots” - Mortality
• Areas of high relative risk based on mortalityHazards examined: drought, flood, landslides, earthquakes, volcanoes, cyclones
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Global Natural Disaster “Hotspots” – Economic Losses
• Areas of high relative risk based on economic lossesHazards examined: drought, flood, landslides, earthquakes, volcanoes, cyclones
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Global Natural Disaster “Hotspots” – Economic Losses Relative to GDP
• Areas of high relative risk based on economic losses as a proportion of GDP densityHazards examined: drought, flood, landslides, earthquakes, volcanoes, cyclones
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These hotspots are defined by locating places in highest 3 deciles, globally, of physical exposure
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These hotspots are defined by locating places in highest 3 deciles, globally, of physical exposure
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These hotspots are defined by locating places in highest 3 deciles, globally, of deaths attributed to hazard exposure
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These hotspots are defined by locating places in highest 3 deciles, globally, of deaths attributed to hazard exposure
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These hotspots are defined by locating places in highest 3 deciles, globally, of deaths attributed to hazard exposure
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2) There are more harms on the way
Global change is underway on unprecedented scale
It’s more than just climate change – multiple stresses threaten ecological and social systems
These changes will alter historical patterns of some natural disasters – including floods, droughts, landslides, cyclones
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Atmosphere
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Slide courtesy James Hansen
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Melt descending into a moulin, a vertical shaftcarrying water to ice sheet base.
Source: Roger Braithwaite, University of Manchester (UK). Slide courtesy James Hansen
Surface Melt on Greenland
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Jakobshavn Ice Stream in Greenland
Discharge from major Greenland ice streams is accelerating markedly.
Source: Prof. Konrad
Steffen, Univ. of Colorado. Slide courtesy James Hansen
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~80% of world’s land surface has been significantly altered by direct human transformation
~40% of all photosynthesis appropriate by humans
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Unprecedented change in structure and function of ecosystems
More land was converted to cropland since 1945 than in the 18th
and 19th centuries combined
Cultivated Systems in 2000 cover 25% of Earth’s terrestrial surface
(Defined as areas where at least 30% of the landscape is in croplands, shifting cultivation, confined livestock production, or freshwater aquaculture)
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Unprecedented change: Aquatic Ecosystems
– Amount of water in reservoirs quadrupled since 1960
– Withdrawals from rivers and lakes doubled since 1960
Intercepted Continental Runoff: 3-6 times as much water in reservoirs as
in natural rivers
(Data from a subset of large reservoirs totaling ~65% of the global total
storage)
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Unprecedented change: Biogeochemical Cycles
Since 1960:– Flows of biologically
available nitrogen in terrestrial ecosystems doubled
– Flows of phosphorus tripled
> 50% of all the synthetic nitrogen fertilizer ever used has been used since 1985
Human-produced Reactive Nitrogen
Humans produce as much biologically available N as all natural pathways and this may grow a further 65% by
2050
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Significant and largely irreversible changes to species diversity
– Humans have increased the species extinction rate by as much as 1,000 times over background rates typical over the planet’s history
– 10–30% of mammal, bird, and amphibian species are currently threatened with extinction
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Geographic extent of maximum fish catch
Source: Daniel Pauly, University of British Columbia)
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Drylands are a special case: very dangerous combination of
- Poor baseline conditions-Socioeconomic stresses increasing (esp. populationgrowth)
-Climatic stresses increasing(droughts likely to increase)- Weak institutional capacity
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Coastal areas also under extreme pressure; some are very vulnerable
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The 1990s increase in population density in the coastal zone is greater than current total density worldwide, for most of the world’s land surface
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Total Population in 10-m LECZ
Percentage of Population in 10-m LECZ
To help characterize sea-level rise risk, we identified 10- meter “Low-Elevation Coastal Zones” (LECZs) and counted population within them, by country
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46% of pop.
37% of pop.
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3) The patterns are uneven, and surprising catastrophes are likely
Vulnerability is a function of physical exposure to hazards and underlying socioeconomic patterns of resilience.
Both exposure and resilience are distributed highly unevenly, in complex ways
We can identify some regions as more dangerous than others, but we cannot reliably predict end-of-chain consequences
There are good reasons to be worried about high-impact catastrophes
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Drought (3 consecutive overlapping 3-month seasons with rainfall at least 50% below normal)
Not poor Somewhat poor Moderately poor
Poor Extremely poor
10.00
20.00
30.00
40.00
50.00
% o
f pop
ulat
ion
0 1 2 3 4 5 6 7 8 9 1011 121314 15 19
Drought frequency 1980-2000
10.00
20.00
30.00
40.00
50.00
% o
f pop
ulat
ion
0 1 2 3 4 5 6 7 8 9 10 11 121314 1519
Drought frequency 1980-2000
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Emerging Infectious Disease Outbreak Risk
Determined through analysis of historical spatial pattern of all known EIDs, examining effect of human population, wildlife population, and climate
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1 2 3 4 5 6 7 8 9 10
Deciles of Rainfall Deviation(1=below normal; 10=above normal)
0.05
0.10
0.15
0.20
Prob
abili
ty o
f Hig
h-In
tens
ity O
utbr
eak ] ]
]
]
]]
]
]
]
]
Conditional Probability of High-IntensityOutbreak, by Rainfall Deviation Decile,given ongoing Low or Medium Intensity Conflict
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Illustration: Nepal 2002 Outbreak
1
21
4
n=decile of rainfall deviation measure
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Rainfall Deviations in Nepal 1979 - 2002
-15
-10
-5
0
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10
15
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25
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1979 1984 1989 1994 1999
Year
Sum
of m
onth
ly d
evia
tions
-15
-10
-5
0
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10
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20
25
30
Non-conflict Zone .Conflict Zone .
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Source: Vörösmarty et al. 2000
• 80% of future stress frompopulation
& development, not climate change!
• Future distortions of thewater cycle are inevitable
Water Stress Changes to 2025
UNH
Less stressNo changeMore stress
•
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4) There are no easy responses – it will take sustained, focused efforts
What would be most helpful:
Comprehensive assessment of vulnerability to natural hazards in context of both global change and socioeconomic change
- Baseline vulnerability to natural hazards- Plausible projections of physical and social stresses- Identification of simple, direct threats (floods, droughts, disease, etc)- Elaboration of complex scenarios of interest- Articulation of strategies to increase resilience and preparedness
Military sector cannot do this in a vacuum
What’s at stake is more than simple ability to cope with disasters; government legitimacy also vulnerable