global environmental change and delta risk · 2015. 7. 30. · overeem) different climo-meterologic...
TRANSCRIPT
Z. Tessler, CCNY
Global Environmental Change and Delta Risk
Zachary TesslerCharles VörösmartyCity College of New York
Z. Tessler, CCNY
Relative Sea Level Rise is a major concern in deltas
Approx. Global Mean
Newest estimates put rate of global mean SLR at 2.6-2.9+-0.4 mm/yr over satellite altimetry era (Watson et al. 2015)
Z. Tessler, CCNY
But, consequences of RSLR are not equal across deltas
Coastal development:
vs.
Z. Tessler, CCNY
But, consequences of RSLR are not equal across deltas
vs.
Coastal development:
Coastal defense:
vs.
Ganges Delta (photo: Irina Overeem)
Z. Tessler, CCNY
But, consequences of RSLR are not equal across deltas
vs.
Coastal development:
Coastal defense:
vs.
Ganges Delta (photo: Irina Overeem)
Different climo-meterologic conditions:
Z. Tessler, CCNY
But, consequences of RSLR are not equal across deltas
vs.
Coastal development:
Coastal defense:
vs.
Ganges Delta (photo: Irina Overeem)
Different climo-meterologic conditions:
RSLR will impact the communities living
on these deltas very differently
Z. Tessler, CCNY
Goal: Estimate impact of RSLR on delta risk, globally
Z. Tessler, CCNY
Delta Flood Risk Model
● Model risk as expected loss
● Loss from a single hazardous event, h0
● E is exposure, the number of people exposed to hazardous conditions by h0
● V is vulnerability, is the average harm or loss endured by those exposed
L=Eh0∗V h0
Z. Tessler, CCNY
Delta Flood Risk Model
● Total risk or expected loss, R, is the sum of losses over all possible hazardous events, weighted by probability H(h):
R=∑h
H (h)E (h)V (h)
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Delta Flood Risk Model
● Simplify range of hazards down to single representative hazard class:
● How can we estimate H, E, and V for each delta?● How does this relate to RSLR?
H EV
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Estimating H, E, V
● Direct estimation:– From historical event database, estimate exposed population
and total loss with respect to event intensity
– But, for many deltas, historical data is inadequate
● Indirect estimation:– Identify variables that are both indicative of risk factors, and
also measured or estimated at the global scale
– Sample from global datasets to obtain consistent estimates for each delta
– Normalize and weight indicators
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Delta Extent Maps
Indus
KrishnaGodavari
BrahmaniMahanadi
Ganges
Irrawaddy
Chao Phraya
Mekong
HongPearl
Yangtze
Yellow
Mahakam
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Delta Extent Maps
Population: GRUMPv1(based on administrative data and night-light remote sensing)
These maps will soon be available, website is under construction now
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Hazard Frequency and Intensity (H)
● Indicators:– Tropical cyclone
intensity and frequency
– M2 tidal amplitude
– River discharge 30yr return value (standardized)
– Wave energy 30yr return value (standardized)
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Hazard Frequency and Intensity (H)
● Indicators:– Tropical cyclone
intensity and frequency
– M2 tidal amplitude
– River discharge 30yr return value (standardized)
– Wave energy 30yr return value (standardized)
Z. Tessler, CCNY
Vulnerability (V)
● Many variables have been used in local/regional studies to estimate social vulnerability
● Here, restricting ourselves to datasets available at the global scale– Belmont GDVI efforts to develop a more comprehensive index will
be very helpful here!!
● Vulnerability of a delta varies at the household scale (strength/quality of housing) and the delta scale (coastal infrastructure)
● Indicators:– Per capita GDP (household vulnerability)
– Aggregate GDP (Capacity for infrastructure investment)
– Government effectiveness index (Capacity/will for preparedness)
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Exposure (E)
● Challenges estimating population exposure:– (Topography + Population Distribution) is not
enough due to coastal protections, data resolution
While low-lying areas in the Mekong and Irrawaddy are flooded, <0m elevation land in the Pearl is protected by coastal and channel barriers (From Syvitski 2009)
Z. Tessler, CCNY
Exposure (E)
● ΔE is a more tractable measure than E● RSLR results in lower elevation, increased
population exposed (for a given hazard)● Estimate RSLR from available indicators● Obtain estimate for changing flood risk due to
RSLR
ΔR=H (ΔE)V
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RSLR Indicators
● Delta:– Population Density
– Wetland Disconnectivity
– Impervious Surface Area
– Groundwater Depletion
– Hydrocarbon Extraction
● Upstream Basin:– Population Density
– Wetland Disconnectivity
– Impervious Surface Area
● Offshore:– Local sea level rise trend
Estimates from Ericson (2006) and Syvitski (2009)
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Change in Exposure (ΔE)
Mek
ong
Am
azon
Gan
ges
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Hazard Frequency and Intensity (H)
Mek
ong
Am
azon
Gan
ges
Z. Tessler, CCNY
Investment Capacity - inverse of Vulnerability (V)
Mek
ong
Am
azon
Gan
ges
High VulnerabilityLow
Vulnerability
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ΔRisk SpaceΔ R=H (Δ E)V
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ΔRisk SpaceΔ R=H (Δ E)V
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Low vulnerability is very important!Δ R=H (Δ E)V
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A thought experiment...
● How might vulnerability change in an energy-constrained future?– Increased energy prices
– Require stronger infrastructure to maintain constant level of protection due to future SLR
– Overall, more expensive to reduce vulnerability
● Re-weight Vulnerability Index to reduce the relative importance of GDP– (more difficult to “buy your way out of trouble”)
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Future Changes in Vuln, and Exposure Both future
vulnerability and exposure increases
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ΔRisk
Wealthy deltas currently invest in protective infrastructure, reducing risk from increasing RSLR despite geophysical setting
If this is not an option in the future, risk “rebounds” and approaches the risk state with no investment.
Seen most dramatically in wealthy deltas in hazardous locations – Mississippi, Rhine, Han, Yangzte...
Z. Tessler, CCNY
ΔRisk
Wealthy deltas currently invest in protective infrastructure, reducing risk from increasing RSLR despite geophysical setting
If this is not an option in the future, risk “rebounds” and approaches the risk state with no investment.
Seen most dramatically in wealthy deltas in hazardous locations – Mississippi, Rhine, Han, Yangzte...
Z. Tessler, CCNY
ΔRisk
Wealthy deltas currently invest in protective infrastructure, reducing risk from increasing RSLR despite geophysical setting
If this is not an option in the future, risk “rebounds” and approaches the risk state with no investment.
Seen most dramatically in wealthy deltas in hazardous locations – Mississippi, Rhine, Han, Yangzte...
Z. Tessler, CCNY
ΔRisk
ΔR
Δ RF−Δ R
Δ R
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Delta Risk Profiling Conclusions
● Krishna, Ganges, Brahmani, Godavari deltas are most sensitive to increased RSLR (per capita risk basis)
● Several wealthy deltas (Mississippi, Rhine) have low ΔR despite high hazard and high RSLR estimates due to low vulnerability
● Future changes to vulnerability due to changing economics of coastal protection will have outsized effects on these systems. These particular systems are highly sensitive to changing vulnerability.
Z. Tessler, CCNY
Delta Characterization by Environmental Stress Patterns
● Looking across deltas, are some patterns of environmental stress more common?
● What are the implications for sustainable management?
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Indicator Correlations
Indicators projected into first 2 PCA components
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Indicator Correlations
Indicators projected into first 2 PCA components
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K-means Clustering
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K-means Clustering
Blue: Mean indicator values within clusterPink: Min-Max range of indicator values
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Sensitivity to Clustering MethodColors indicate Kmeans clustering with k=8Line width: How often two deltas are clustered together in all clustering
methods (KM-6, KM-7, KM-8, KM-9, Affinity Propogation)
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Delta Clustering For Improved Management
● Clusters identify systems under similar suites of environmental stress
● First take on address “deltas as snowflakes” challenge
● Provide an apples-to-apples context for comparing delta change
● Opportunities for sharing of effective management strategies between other systems