Global Warming--Are We on Thin Global Warming--Are We on Thin Ice? Convergence of evidence for Ice? Convergence of evidence for anthropogenic global warming anthropogenic global warming • 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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Global Warming--Are We on Thin Ice? Convergence of evidence for anthropogenic global warming Climate forcing, feedback, response, committed warming Evidence.
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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
Proxy data used by Mann et al. 1998Proxy data used by Mann et al. 1998
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
Tree Ring DendrochronologyTree Ring Dendrochronology
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
Coral 18O/16O TemperatureReconstruction
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.
Greenland ice core: high resolution/distinct layers
Bore Hole - Hockey Stick Bore Hole - Hockey Stick ComparisonComparison
‘‘Adjusted’ by Mann et al.Adjusted’ by Mann et al.
Bore Hole - Hockey Stick Bore Hole - Hockey Stick ComparisonComparison
Bore Hole Data for Eastern & Bore Hole Data for Eastern & Western North America Western North America
((Huang & Pollack)Huang & Pollack)
Bore Hole - Briffa et al Bore Hole - Briffa et al ComparisonComparison
Bore Hole - Overpeck et al Bore Hole - Overpeck et al ComparisonComparison
Satellite EraSatellite Era1970s ---> now1970s ---> now
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
Tropospheric Temperature TrendsChristy and Spencer were wrong
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
Arctic Sea Ice Trends
2005 summer minima
1979 summer minima
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)
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
Atmospheric CO2 measurements
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?
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
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
Atmospheric COAtmospheric CO22 since 1740 since 1740
Different CO2 slopes reflect time
techno-economic conditions
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
Colder temperatures -> more snow Colder temperatures -> more snow and ice -> colder temperatures…and ice -> colder temperatures…
Distance accuracy Distance accuracy 0.001 mm0.001 mm
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?
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.