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Testing the ‘Hockey Stick’
Mann, Bradley and Hughes McIntyre and McKitrick VS Laura Zaunbrecher EAS 4803 April 22, 2008
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Overview Proxy Data Methods Mann ‘Hockey Stick’ updates (vs. MM)
Data Calibration Principle Component Analysis Comparison to Mann ‘98 Results Temperature Reconstruction Mann ‘Hockey Stick’ updates (vs. MM) Conclusions
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Proxy Data 14 used here- Original used 415
2 Ice Core d18O records from Quelccaya Ice Cap in Peru 2 Ice Accumulation Records – Peru Svalbard Ice Melt (summer air temp) Greenland Ice Core d18O N. Patagonia, Tasmania, Yakutia, NC,SC, GA precipitation (tree ring widths) N. Patagonia, – dendrodensity NA Tree line Data
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Methods -Calibration Each Proxy series is calibrated to the instrumental NH temperature record from 1880 to 1980
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Mann EOF’s 1 and 2 Calibration should capture at least these first 2 EOFS
Increasing temp ENSO
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Principle Component Analysis
-Retain up to the 4th Principle Component -Ignore EOF Analysis -[u,s,v] =svd(A,’econ’) = A U • W • VT
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Principle Components NOISE!! =U(:,1) HOCKEY STICK!!! =U(:,2)
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Comparison to MBH98 MUCH Noiser (more variant) than the complete dataset Hockey Stick is captured in PC2 Other PC’s are just Noise – likely from using only 14 Proxies Versus the 415 used in MBH98
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Temperature Reconstruction
Mann et al., 1998 -’Hockey Stick Temperature Spike ~0.3°C -Smaller Amplitude than found by MBH -Large Interdecadal Oscillations -Lots of Noise!!!!
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McIntyre and McKitrick argue…
Mann’s NHtemp reconstruction gives too much weight to PC1 and bristlecone pine Corrcoef(MannNHtemp, MannPC1) = Coorcoef(MannNHtemp,Bristlecone) =0.5144
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Uses different calibration intervals
Psuedo-proxy study Uses different statiscital technique –RegEM STILL GET THE HOCKEY STICK!!!!
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Conclusions Majority of Signal is Noise
Do not capture ENSO in PC’s when using the 14 proxies in this study Skipped some important steps – Verification, Weights (proxies were weighted equally here) DO get the ‘Hockey Stick’ as the major form of temperature variation (after noise) Global Warming is REAL!
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Questions?
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