global warming--are we on thin ice? convergence of evidence for anthropogenic global warming climate...
TRANSCRIPT
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Global Warming--Are We on Thin Global Warming--Are We on Thin Ice? Convergence of evidence Ice? Convergence of evidence
for anthropogenic global for anthropogenic global warmingwarming
• Climate forcing, feedback, response, committed warming
• Evidence of global warming• Projections of global warming
Compton Tucker
NASA/Goddard Space Flight Center and
Climate Change Science Program Office
Washington, D.C. USA
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Climate FeedbackClimate Feedback
Given a climate forcing (e.g. COGiven a climate forcing (e.g. CO22 increase) increase) initial warming initial warming
• Amplifying loopsAmplifying loops (positive feedback) (positive feedback) magnify the warmingmagnify the warming
• Diminishing loopsDiminishing loops (negative feedback) (negative feedback)
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Climate FeedbacksClimate Feedbacks
Warming
Evaporation from ocean,Increase water vapor in atmEnhance greenhouse effect
Increase cloud cover;Decrease absorption of solar energy
Decrease snow cover;Decrease reflectivity of surfaceIncrease absorption of solar energy
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Measured Surface Temperature Measured Surface Temperature the past 150 yearsthe past 150 years
6 warmest years: 1998, 2002, 2003, 2004, 2005, 20066 warmest years: 1998, 2002, 2003, 2004, 2005, 2006
.
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Warming Warming greatest at greatest at
high high latitudeslatitudes
Amplification of Amplification of warming due to warming due to
decrease of decrease of albedo (melting of albedo (melting of
snow and ice)snow and ice)
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Bore Hole LocationsBore Hole Locationsdifferent physics (different physics (thermal diffusivity) thermal diffusivity)
& 10s of years time steps& 10s of years time steps
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Bore Hole Temp. ReconstructionsBore Hole Temp. Reconstructions
~500 years
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Sub-surface Annual TemperatureSub-surface Annual Temperature12.8 m depth @ Wisconsin USA12.8 m depth @ Wisconsin USA
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Bore Hole Temperature Reconstructions
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Proxy surface Temperature data Proxy surface Temperature data density circa 1500 ADdensity circa 1500 AD
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Proxy surface Temperature data Proxy surface Temperature data density circa 1000 ADdensity circa 1000 AD
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National Research Council USA National Research Council USA June 2006 ReportJune 2006 Report
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Mann, Bradley, & Hughes (1998):Mann, Bradley, & Hughes (1998):The “hockey stick” surface temperatureThe “hockey stick” surface temperature
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Proxy data used by Mann et al. 1998Proxy data used by Mann et al. 1998
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McIntyre and McKitrick 2003McIntyre and McKitrick 2003a reanalysis with a subset of Mann et al. a reanalysis with a subset of Mann et al.
1998’s data1998’s data
15th century the warmest time 15th century the warmest time in the past 1000 to 2000 years?in the past 1000 to 2000 years?
Same result as Mann et al. 1998 when Same result as Mann et al. 1998 when 5 PCs are used for 15th century5 PCs are used for 15th century
Same result as Mann et al. 1998Same result as Mann et al. 1998
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Tree Ring DendrochronologyTree Ring Dendrochronology
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Some ring-width seriesSome ring-width series
Cook, 1989Four red spruce ring-width series from the same stand – different Four red spruce ring-width series from the same stand – different
trends related to competition and disturbance.trends related to competition and disturbance.
~40-50% of tree ~40-50% of tree ring data from ring data from
trees selected from trees selected from temperature- temperature-
limited areaslimited areas are are related to surface related to surface
air temperatureair temperature
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Coral 18O/16O TemperatureReconstruction
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Proxy Surface Temperaturesfrom corals, sediments, and
ice cores using 18O/16O18O = (18O/16O)sample - (18O/16O)SMOW x 103 ‰
(18O/16O)SMOW
SMOW = Standard Mean Ocean Water
1818O: O: 0.20%0.20%
1717O: O: 0.04%0.04%
1616O: O: 99.76%99.76%
The vapor pressure of HH221616O is > than that of O is > than that of
HH221818O; converselyO; conversely HH22
1818OO passes into the liquid state more readily. Because condensation is the result of cooling, the greater the fall in
temperature the lower the 1818O concentration O concentration in Hin H22O will be. Isotope concentration can thus O will be. Isotope concentration can thus
be considered a function of temperature.be considered a function of temperature.
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Greenland ice core: high resolution/distinct layers
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Bore Hole - Hockey Stick Bore Hole - Hockey Stick ComparisonComparison
‘‘Adjusted’ by Mann et al.Adjusted’ by Mann et al.
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Bore Hole - Hockey Stick Bore Hole - Hockey Stick ComparisonComparison
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Bore Hole Data for Eastern & Bore Hole Data for Eastern & Western North America Western North America
((Huang & Pollack)Huang & Pollack)
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Bore Hole - Briffa et al Bore Hole - Briffa et al ComparisonComparison
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Bore Hole - Overpeck et al Bore Hole - Overpeck et al ComparisonComparison
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Satellite EraSatellite Era1970s ---> now1970s ---> now
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Total Solar Irradiance
~1 watt/m~1 watt/m22 variation out of ~1400 w/m variation out of ~1400 w/m22 over 30 years over 30 years
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Tropospheric Temperature TrendsChristy and Spencer were wrong
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Sea Level Rise from thermal expansion Sea Level Rise from thermal expansion & input of water from melting glaciers& input of water from melting glaciers
20 cm (7 inches) in a century20 cm (7 inches) in a century
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Arctic Sea Ice Trends
2005 summer minima
1979 summer minima
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Satellite Detection of Sea IceSatellite Detection of Sea IceHigher rate of microwave Higher rate of microwave
emission from sea ice than emission from sea ice than from open water. Emissivities from open water. Emissivities indicated are for wavelength indicated are for wavelength of 1.55 cm (19 GHz)of 1.55 cm (19 GHz)
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Warmer Earth Warmer Earth Greener NorthGreener North
Arctic Sea Ice Extent 1979 to 1999Arctic Sea Ice Extent 1979 to 1999
Claire Parkinson et al. 2002
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Atmospheric CO2 measurements
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Outstanding QuestionsOutstanding Questions
• Only half of the COOnly half of the CO22 produced produced
by human activities is by human activities is remaining in the atmosphereremaining in the atmosphere
• Where are the Where are the sinkssinks that are that are absorbing over 40% of the COabsorbing over 40% of the CO22
that we emit?that we emit?
– Land or ocean?Land or ocean?
– Eurasia/North America?Eurasia/North America?
• Why does COWhy does CO22 buildup vary buildup vary
dramatically with nearly dramatically with nearly uniform emissions? uniform emissions?
• How will COHow will CO22 sinks respond to sinks respond to
climate change?climate change?
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Observed Halting of the Greening Trend
(NDVI) / t : Summer 1982-1991
(NDVI) / t : Summer 1994-2002
Summer drying reduced photosynthesis Recent slowing of the land C sink Angert et al. “Drier summers cancel out the CO2 uptake enhancement induced by warmer springs”
PNAS 2005
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Equilibrium Climate from Ice Core DataEquilibrium Climate from Ice Core Data
J. HansenJ. Hansen
• Estimate Estimate climate climate
forcing (W/mforcing (W/m22) ) from from
atmospheric atmospheric composition composition
changeschanges
• Regress Regress Temperature Temperature
anomalies anomalies against against climate climate forcing forcing
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Atmospheric COAtmospheric CO22 since 1740 since 1740
Different CO2 slopes reflect time
techno-economic conditions
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Climate Forcing: expressed as a change in Climate Forcing: expressed as a change in radiative heating (W/m2) at surface for a given radiative heating (W/m2) at surface for a given
change in trace gas composition or other change change in trace gas composition or other change external to the climate systemexternal to the climate system
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Colder temperatures -> more snow Colder temperatures -> more snow and ice -> colder temperatures…and ice -> colder temperatures…
Earth TOA actual W/m^2 1365
Total Watts Temp. (K)"Albedo" absorbed
0.20 5.58E+17 263.40.25 5.23E+17 259.20.30 4.88E+17 254.80.35 4.54E+17 250.10.40 4.19E+17 245.1
1365*(1-albedo)*4*pi*radius*radiusMore snow and ice ---> higher albedoMore snow and ice ---> higher albedo
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J. Hansen
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What? Me worry?
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280
320
360
400
440
480
520
560
600
1900 1950 2000 2050 2100 2150
Atmospheric CO
2 (ppmv)
Oil
Gas
Coal
Biosphere
Business-as-Usual(2% annual growth until 50% depletion, then 2% annual decline)
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280
320
360
400
440
480
520
560
600
1900 1950 2000 2050 2100 2150
Atmospheric CO
2 (ppmv)
Oil
Gas
Coal
Biosphere
Alternative Case: Coal Phaseout(+2%/yr to 2012; +1%/yr to 2022; linear shutdown between 2025-2050)
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Majority of Glaciers are recedingMajority of Glaciers are receding
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Greenland--where the rubber Greenland--where the rubber hits the climate roadhits the climate road
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It’s only a matter of time…
400 km3 ice = 1 mm sea level
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> Streaming, >Earthquakes> Streaming, >Earthquakes
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Satellite record melt of 2002 was exceeded in 2005
Surging Surging glaciers & glaciers &
meltingmelting
Greenland Ice: Greenland Ice: 70 m thinning in 5 years70 m thinning in 5 years
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Greenland Mass Loss from GRACEGreenland Mass Loss from GRACE
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Gravity Recovery & Gravity Recovery & Climate ExperimentClimate Experiment
500 km orbit500 km orbit
220 km separation220 km separation
Distance accuracy Distance accuracy 0.001 mm0.001 mm
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SummarySummary• Global warming is real and happeningGlobal warming is real and happening• 2121stst C: drying of tropics C: drying of tropics reduce C uptake reduce C uptake
accelerate global warming accelerate global warming• 2121stst C: stable stratification in ocean, reduce C: stable stratification in ocean, reduce
thermohaline circulation thermohaline circulation reduce C uptake reduce C uptake accelerate global warming accelerate global warming
• Fossil Fuel emission faster than land & ocean uptake Fossil Fuel emission faster than land & ocean uptake bottlenecks bottlenecks accelerate global warming accelerate global warming
• Rapid destablization of glaciers Rapid destablization of glaciers ice-albedo feedback ice-albedo feedback accelerate global warming accelerate global warming raise sea level raise sea level
Uncertainty: how much faster? Uncertainty: how much faster?
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Global Warming SkepticsGlobal Warming Skeptics
Dr. S. Fred SingerDr. S. Fred Singer
““Ozone, Skin Cancer, and Ozone, Skin Cancer, and the SST” S. Fred Singerthe SST” S. Fred Singer
Aerospace AmericaAerospace America July 1994 July 1994
““The hole truth about CFCs”The hole truth about CFCs”S. Fred Singer in S. Fred Singer in Chemistry Chemistry and Industryand Industry March 21, 1994 March 21, 1994
““The EPA and the Science of The EPA and the Science of Environmental Tobacco Smoke”Environmental Tobacco Smoke”
S. Fred Singer and Kent S. Fred Singer and Kent ScholarScholar
Alexis de Tocqueville Alexis de Tocqueville InstitutionInstitutionDr. Singer has a sordid history of opposition to second-hand
tobacco smoke and health, the role of chloro-floro-carbons and ozone depletion, and most recently global warming.
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Pollack & Huang Pollack & Huang Bore Hole DataBore Hole Data
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Holgate Glacier July 24, 1909Holgate Glacier July 24, 1909
Holgate Glacier August 13, 2004Holgate Glacier August 13, 2004
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2121ststC warming depends on COC warming depends on CO2 2 increaseincrease
20thC stabilizn:CO2 constant at 380 ppmv for the 21stC
21thC “Business as usual”:CO2 increasing 380 to 680 ppmv
Meehl et al. (Science 2005)
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