prof alan rodger - the latest evidence on climate change, beyond ipcc
TRANSCRIPT
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Climate change –
beyond IPCCAlan Rodger
Introduction Some examples of changeExtreme events
Predicting the futureSurprises
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Hydrosphere Geosphere
Atmosphere
Cryosphere Biosphere
Anthropo-
sphere
EarthSun
Earth System
Astronomical
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Hydrosphere Geosphere
Atmosphere
Cryosphere Biosphere
Anthropo-
sphere
EarthSun
Earth System
Astronomical
Science
Cultural
Technology
Political
Social
Economics
Well beingWaterFoodShelterFuelHealthSecurity
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IPCC, 2007
The climate system
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IPCC Fourth Assessment Report
Climate Change 2007
•
Atmospheric GHG concentrations far exceed levels of last 650,000y as a result of human emissions
•
Warming of the climate system is “Unequivocal”
•
Climate forcing primarily human (x10 solar)
•
Agreed by delegates of 113 nations
IPCC does not capture non linear effects well
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0km 1,000km 2,000km
80S°
70S°
60S°
Dome C
Vostok
Dome F
TaylorDome
Byrd
DronningMaud Land
Siple Dome
Dome CDome CLaw Dome
BerknerIsland
European Project for Ice Coring in Antarctica (EPICA)Ice cores –
the gold standard climate change record?
EU/ESF project1996-2006 Drilling depth of 3.27km~890 000 years old
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Ice core processing and analysis
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Dome C Antarctica Ice Core
Now –
386 ppm
Luthi et al., Nature, 15 May 2008Siegenthaler et al., Science 2005 (EPICA gas consortium)
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• Increase ~0.8°C over the last century
• 2007 was 8th
warmest year on record
• 12 of the 13 warmest years on record occurred since 1995
• 2001-2007 was 0.21°C warmer than 1991-2000
Global Temperature
data source: Climatic Research Unit
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Temperatures 1951-2001
Precipitation 1961-2002
Blue: positive trend; Red: negative
China
18 more growing days in the Qinghai-
Tibetan Plateau500 hours fewer sunshine in North China Plain compared with 50 years ago
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Surface Temperature Rise
Polar amplification
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The Key Science Issues for Polar Regions
•
Greatest uncertainty in global sea level rise
•
World’s largest carbon sinks, and with the potential for surprise (methane/hydrates)
•
Critical role of polar ecosystems and biodiversity in the maintenance of the earth system
•
The major driver of global ocean system, and hence fundamental to predicting world’s weather
•
Understanding how the planet works –
the polar component
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Antarctic Peninsula Glacier Responses
244 glaciers -
87% have retreated over last 50yCook et al., 2005
Peninsula 1993-2003
Flow rate of over 300 glaciers
12% increase in glacier speed
Sea level rise: 0.16 ±
0.06 mm /y
Pritchard and Vaughan, 2007
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Ice-thickness change 1992-2003
Major dischargesPine Island, Thwaites and
Smith Glaciers
The West Antarctic Ice Sheet and sea level rise
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Bed elevation in Greenland and Antarctica
-2000
+2000
0
Bamber & Vaughan, BEDMAP.
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ICE
LITHOSPHERE
OCEAN
Grounded below sea level
West Antarctica –
last of the great marine ice sheets
After G Clarke
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11 Mar 2008Dublin Lecture no. 6 18
� Greenland is melting!
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11 Mar 2008 Dublin Lecture no. 6 19
Arctic sea ice Median Sept. Extent 09.09.2008 1979-2000
IMPACTS
Shorter trade routesEasier access to oil and gasOcean circulationEcosystems
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1
2
34
5
68
7
1: Barentshavet2: Sørlige Karahavet og Vest-Sibir3: Nordlige Karahavet4: Laptevhavet5: Øst-Sibirhavet6: Chuchihavet7: Alaska North Slope8: Øst-Grønnland
Resten av verdenArktis
Verdens uoppdagede petroleumspotensiale
N. AfrikaKaspihavetMidt-Østen
1
2
34
5
68
7
1: Barentshavet2: Sørlige Karahavet og Vest-Sibir3: Nordlige Karahavet4: Laptevhavet5: Øst-Sibirhavet6: Chuchihavet7: Alaska North Slope8: Øst-Grønnland
Resten av verdenArktis
Verdens uoppdagede petroleumspotensiale
N. AfrikaKaspihavetMidt-Østen
1.
Barents Sea2.
Southern Kara Sea and Western Siberia
3.
Northern Kara Sea4.
Laptev Sea5.
East Siberian Sea6.
Chukchi Sea7.
Alaska North Slope8.
East Greenland
World’s Petroleum Potential
Arctic
Rest of
World
North Africa,
Middle East
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Sea Level Rise -
Tide Gauge Observations
-100
-50
0
50
100
150
1880 1900 1920 1940 1960 1980 2000
ΔMSL
(mm
)
Year
Average Rate ~ 1.8 mm/year
0.8 mm/year
2.0 mm/year
3.2 mm/year
Source: Church and White, 2006Source: Church and White, 2006
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Sea level trends between January 1993 and December 1999 from satellite data in mm/yearRed = sea level rise : Blue = sea level fall
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Tuvalu 8°S, 179°E
•
Land area 26 square kilometres•
Population 4492•
Third least populated independent country•
Second smallest member of the UN•
Tuvalu has very poor land; soil is hardly usable•
Almost no reliable supply of drinking water
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Sea level rise and the EU
Within 500 m of the coast
•
14% of population (70 m people)
•
economic assets located of the EU's coastline valued of €1,000B
•
47,500 km2
of sites of high ecological value
15 countries have substantial coasts that are open to the world’s oceans
•
coastal flooding,
•
increased rates of erosion
•
destruction of natural sea defences
•
threats to human lives and livelihoods
Annual expense of protection €3.2 billion and rising non-
linearly
Managed retreat only option in some areas
.
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Extreme events
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Ciais et al., Nature 2005
effect of the 2003 heat wave in Europe
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Hurricane frequency not changing
Katrina from space
HannaIke
Josephine
Gustav
Karina
3 September 2008
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Webster, et al., Science 2005
Hurricane intensity is increasing
Number of hurricanes unchanged
Katrina from space
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60% of rice from Irrawaddy Delta
Mangroves swamps cleared for crops -
protection lost
Crops destroyed by storm surge
The saltiest areas will have to be drained and flushed with fresh water before they can be re-planted
Draining a challenge as designed to hold water
Cyclone Nargis hits Burma May 2008
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Heavier precipitation, more intense and longer droughts….
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Drought areas already expanding and predicted to expand further
1960 1980 2000 2020 2040 2060 2080 2100
Perc
enta
ge in
dro
ught
50
40
30
20
10
0
Percentage of world's land area in drought
Source: Burke, EJ and SJ Brown. Modelling the recent evolution of global drought andprojections for the 21st century. Journal of Hydrometeorology, 2006
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Vulnerable
LowModerateHighVery high
Desertification
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IPCC Temperature Projections
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Uncertainties in prediction
1.
Future emissions are not known2.
Computer models are not perfect
3.
Natural variability of climate occurs
Therefore
Improve understanding and modelling of the climate system
Quantify uncertainty: probabilistic forecasts
Incorporate probabilistic forecasts into decision making tools
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geological reservoirs
fossil fuel emissions land use
changeland sink
ocean sink
7.2 1.5 2.3
2.2
atmosphere4.2
The carbon cycle2000-2005 CO2
budget (GtC/y)
Canadell et al. 2007
Natural and man-made sources and sinks changing
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Raupach et al., 2007
fossil fuel CO2
emissions for the world
CO2
emissions increase 1990s
1.3% y-1
2000-2006 3.3% y-1
CO2
growth rate65±16% from increasing global economic activity17±6% from the increasing carbon intensity of the global economy18±15% from the increase in airborne fraction
Canadell et at., PNAS, 2007
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Less carbon draw down from the atmosphere into the oceans
Cause: Increase in
Southern Ocean winds
Le Quéré
et al., Science, 2007
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The other carbon problem 1-
ocean acidification
800 ppm
CO2
is corrosive to the shells of many marine organisms
Phytoplankton assemblages will change
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The other carbon problem 2 -
methane
800 ppm
More carbon locked up in methane than in oil and gas
Methane from the tundra
Methane from the ocean
Methane from farming
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Surface area 17,160 km²
(2004, three lakes)
28,687 km²
(1998, two lakes)
68,000 km²
(1960, one lake)
Fivefold increase in salinity
Weapons testing
Wind blown salt damages crops
Polluted drinking water
Salt and dust laden air causing health problems
“The Aral Sea, the worst man-made environmental disaster”
says UN
Aral Sea
1989 2003 Water
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Water
Change of rainfall in 2090 compared with 1990
Lack of melting snow Changes in precipitation –
very hard to predict
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•
The Earth system is highly coupled
•
Change occurring everywhereRates of change increasingFastest at the polesRate of change unprecedentedHumans are affecting the planet
•
IPCC -
conservative•
Predicting the future: the big challenge
•
BUT challenge the climate scientist
Conclusions
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Probabilistic forecasts
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geoengineering
options
Keith, Nature, 2001 Problems:• difficult to scale up• difficult to prove efficiency• difficult to reverse• possible side-effects• decades of research needed
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Model Improvements
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The economics of ecosystems and biodiversityEuropean Commission, 2008
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The glacial cycle
Temperature rises a little because of the orbit of the Earth
Warmer waters cannot dissolve as much CO2
Increase in temperatureIncrease CO2
leads to more heating
Other feedbacksincrease phytoplankton at high latitudesless sea ice
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Earth‘s OrbitEarthEarth‘‘s Orbits Orbit
Milankovitch cycles
Temperature precedes CO2
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Variations/uncertainties
Long term –
cryosphere years/decades -
m
Storm surges –
pressure/winds 1–5 days -
up to 5 m
Ocean surface topography (changes in water density and currents) -
days to weeks -
up to 1 m
El Niño-Southern Oscillation (ENSO) -
up to 0.6 m
River runoff/floods -
2 months -
1 m
Seasonal water density changes (temperature/ salinity) -
6 months 0.2 m
Sea-Level Rise Could Wipe Out Bangladesh by 2100Proudman Oceanography Laboratory, 2008X 4 IPCC estimates of sea level rise
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Serengeti2005 2006January
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South Sandwich Trench 6348 m © Diaz & Carpenter, VIMS
Unexpected high diversity in the Southern Ocean deep sea: > 1400 species, > 700 new, undescribed species
Isothermal environment Southern Ocean warmingAnimals susceptible to change
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Impacts of change on the Antarctic Peninsula
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Natural Variability
Variability on long term trends
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Long term and abrupt climate change
Methane hydrates
Methane from tundra
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The Intergovernmental Panel on Climate Change (IPCC) has been established by WMO and UNEP to assess scientific, technical and socio-economic information relevant for the understanding of climate change, its potential impacts and options for adaptation and mitigation.
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11 Mar 2008 Dublin Lecture no. 6 60
Projected patterns of precipitation changes 2090/2099 : 1980/1999
Dec-Feb Jun-Aug
Stippled areas: uncertain40% of the world’s food supply requires irrigation
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Socolow
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Zachos
et al. 2008
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385
180
1850
2008
650 thousand years
atmospheric CO2
(ppm)
280
1958
Siegenthaler et al. 2006
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Atmospheric increase = Emissions from
fossil fuels + Net emissions from changes in land use - Oceanic
uptake - Missing carbon sink
3.2 (±0.2) = 6.3 (±0.4) + 2.2 (±0.8) - 2.4 (±0.7) - 2.9 (±1.1)
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Plantations in Campo-Maan
in Cameroon now dominate the landscape (right)30 years ago the forest appears largely intact
Declining water levels in Lake Chad. Persistent droughts and increased agricultural irrigation have reduced the Lake’s extent in the past 35 years to one tenth of its former state
The drying up of Lake Faguibine
in Mali. When the lake was full (left) it was amongst the largest lakes in Africa but in the 1990s it dried up completely (right)
The disappearing Damietta
Promontory in Egypt. The promontory has eroded dramatically in the last 30 years as waves and currents have stripped its sands faster than the river can replenish them
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Antarctic ice shelf 'hanging by a thread'
Vast iceberg breaks off Wilkins Ice Shelf in Antarctic
28 Feb 2008
17 March 2008
Vaughan et al., 2008
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Ecosystems
Ecosystem services are the benefits that people obtain from ecosystems
Examples include food, freshwater, timber, climate regulation, protection from natural hazards, erosion control, pharmaceutical ingredients, clean air recreation etc.
Since 1900 50% of the world’s wetlands have been lost
30% of coral reefs have been seriously damaged through fishing, pollution, disease and coral bleaching
In the past two decades 35% of mangroves have disappeared
Rates of species extinction are 1000 times more rapid than the natural rate
The economics of ecosystems and biodiversityEuropean Commission, 2008
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Southern Ocean Ecosystem
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Ocean ecosystems
High productivity in the Southern Ocean
Least exploited fishery
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The unknown
The deep sea
Lakes and river systems under the ice
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Woods Hole Research Centre, 2007
The carbon cycle
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King et al, in prep.
Hudson Mountain Subglacial
Volcano
Estimated date of eruption - 220 BC
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Rahmstorf
et al. 2007
Is the IPCC Conservative?
Comparison of reality with IPCC 2001 predictions
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BAS Mission
•
to undertake a world-class programme of science
•
to sustain for the UK an active and influential regional presence, and a leadership role in Antarctic affairs
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Broader Context
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60 yr historyApprox 500 staff
Annual budget approx £40 MScience Logistics
Stations
BAS in Summary
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The greenhouse effect –
a misnomer?
Transmission of visible light and infrared radiation the same
Greenhouses work by lack of convection
The ‘greenhouse’
effect has been understood for nearly 200 years
The ‘natural’
CO2
keeps the Earth around 30°C warmer than it would otherwise be
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Survey by BAS and University of Texas, 2005
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Pine Island Season 2006-07
Ice accessible for discharge ~1.5m msl
equivalent
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20052004 2006
2007
Harlequin Ladybird
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Impacts of climate change and mankind
Wandering albatross-
1% decline p.a. (pre-1997)-
4% decline p.a. (post-1997) 19
60
1964
1972
1976
1980
1984
1988
1992
1996
2000
2004
2008
8 0 0
1 2 0 0
1 6 0 0
2 0 0 0
80% reduction of krill in 30 years –
key food for birds, seals and whales
By catch
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Ecology
Evolution
Physiology and molecular processes
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Precipitation changes Frost changes
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Gentoo penguin breeding success at Bird Island
Year1985 1990 1995 2000
Bre
edin
g S
ucce
ss a
t Bird
Isla
nd
0.0
0.2
0.4
0.6
0.8
1.0Years of extremely low performance
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Long term trend 1976-2004
The interconnected world
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Southern Ocean Ecosystem
•
Clear link between warm conditions and breeding failure in penguins, seals and whales
•
Long-term decline in krill abundance
•
New interest in krill fishing - aquaculture, pharma
and
neutraceuticals
•
The largest under-exploited protein resource -
managing sustainable
fishing critical
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Lake Faguibine, Mali
1974 2005
590 km 2 in 1974Red= vegetation
traditional livelihoods of fishing, agriculture, and livestock herding became impractical
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Lenton, T. M. et al. (2008) Proc. Natl. Acad. Sci. USA 105, 1786-1793
Tipping points
Subsystems indicated could exhibit threshold-type behaviour in response to anthropogenic climate forcing, where a small perturbation at a critical point qualitatively alters the future fate of the system.
Tipping points
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Fisheries
•
Over exploitation
•
Global problem
•
Ecosystem change
•
By-catch
Convention on the Conservation of Antarctic Marine Living Resources
In 2002 fish provided more than 2.6 billion people with at least
20
percent of their average per capita animal protein intake
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CO2
emis
sion
s (G
tC/y
)World
N. America
W. EU
China
Indiadata source: CDIAC and EIA
CO2
emissions increase 1990s
1.3% y-1
2000-2006 3.3% y-1
CO2
growth rate65±16% from increasing global economic activity17±6% from the increasing carbon intensity of the global economy18±15% from the increase in airborne fraction
Canadell
et at., PNAS, 2007
Carbon dioxide increases