stephen mcintyre toronto ontario ross mckitrick guelph ontario washington dc, march 2 2006

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1 Presentation to the National Academy of Sciences Expert Panel, “Surface Temperature Reconstructions for the Past 1,000-2,000 Years.” Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006.

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Presentation to the National Academy of Sciences Expert Panel, “Surface Temperature Reconstructions for the Past 1,000-2,000 Years.”. Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006. Guiding Questions (Boehlert). 2) - PowerPoint PPT Presentation

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Page 1: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Presentation to the National Academy of Sciences Expert Panel, “Surface Temperature Reconstructions for the Past 1,000-2,000 Years.”

Stephen McIntyreToronto Ontario

Ross McKitrickGuelph Ontario

Washington DC, March 2 2006.

Page 2: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Guiding Questions (Boehlert)2)

(b) What are the principal scientific criticisms of their [MBH] work and how significant are they?

(c) Has the information needed to replicate their work been available?

(d) Have other scientists been able to replicate their work?

3)(b) How central is the work of Drs. Mann, Bradley and Hughes to the consensus on the temperature record?

Page 3: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Our Answers

2b) Principal Criticisms “new” statistical methods mined for hockey stick shaped series. These methods were not accurately described Reconstruction failed an important verification test said to have

used in the study and this failure was unreported and the statistical skill was misrepresented both in the original article and by the IPCC.

Dominant weight was placed on proxies known to be inappropriate temperature proxies and a false claim of robustness was made;

The method of confidence interval calculation leads to unrealistically narrow confidence intervals.

Page 4: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Our Answers

2c) Information available for replication?

No.

Many obstructions encountered in replication attempts. The underlying data as used has not always been available. The methodology was not accurately described in the paper and

requests for source code were refused.

Page 5: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Our Answers

2d) Have others replicated MBH?

No.

Ammann and Wahl have not confirmed MBH claims of statistical skill and robustness

In fact, their code actually confirms our claims that MBH verification statistics are insignificant.

Their emulation of MBH is almost identical to ours. Differences between us pertain entirely to interpretation

Page 6: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Our Answers

3b) How central is hockey stick?

Origin of claims of “warmest decade of millennium”

Relied upon by IPCC and governments

Became standard for subsequent studies

Results and methods continue to affect papers published today

Page 7: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Hockey stick is still iconic

Page 8: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Why was the hockey stick so influential? “New” Statistical Approach

Skill

Robustness

Confidence Intervals

Page 9: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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New statistical method

PC methods “Climate fields”

PC methods on tree ring networks

Novel multivariate method for regression

Page 10: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Changes the picture

Figure 2: Top – Average of 450 series in MBH98 “dataall” dataset archived in July 2004.

Bottom – MBH98 reconstruction.

Page 11: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Bias in Tree Ring PC method Data decentered against post-1902 mean

Preferentially adds weight to hockey stick-shaped series in PC1

Page 12: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Questions about multivariate methodology

Sui generis method with unknown statistical properties

No literature on estimating confidence intervals

Page 13: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Skill claims

The reconstruction failed an important verification test (r2) said to have been used in the study.

This failure was not reported

The statistical skill was misrepresented both in the original article and by the IPCC.

Page 14: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Claim in MBH98

• β [or RE] is a quite rigorous measure of the similarity between two variables, measuring their correspondence not only in terms of the relative departures from mean values (as does the correlation coefficient r) but also in terms of the means and absolute variance of the two series. For comparison, correlation (r) and squared-correlation (r2) statistics are also determined.

Page 15: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Claim in IPCC

IPCC TAR WG1, Pages 133, 136

…they [MBH] estimated the Northern Hemisphere mean temperature back to AD 1400, a reconstruction which had significant skill in independent cross-validation tests. Self-consistent estimates were also made of the uncertainties…. Taking into account these substantial uncertainties, Mann et al. (1999) concluded that the 1990s were likely to have been the warmest decade, and 1998 the warmest year, of the past millennium for at least the Northern Hemisphere.

Page 16: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Failed r2 test value

Verification RE

Verification R2 CE

MBH98 0.48 n.r. n.r.

MM05a Emulation 0.46 0.02 -0.26 Ammann&Wahl Code 0.47 0.02 -0.24

Page 17: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Robustness – warnings about bristlecones IPCC 1996

“the extent to which multidecadal, century and longer time-scale variability is expressed can vary, depending on the length of individual …series that make up the chronologies and the way in which these series have been processed to remove non-climatic trends. In addition, the possible confounding effects of carbon dioxide fertilization needs to be taken into account when calibrating tree ring data against climate variations

Biondi et al. (1999)• “[Bristlecone”] are not a reliable temperature proxy for the last

150 years as it shows an increasing trend in about 1850 that has been attributed to atmospheric CO2 fertilization (Graybill and Idso 1993)

Page 18: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Claims about robustness

MBH98:• the long-term trend in NH is relatively robust to the

inclusion of dendroclimatic indicators in the network, suggesting that potential tree growth trend biases are not influential in the multiproxy climate reconstructions. (p. 783, emphasis added.)

Mann et al. 2000:• possible low-frequency bias due to non-climatic influences on

dendroclimatic (tree-ring) indicators is not problematic in our temperature reconstructions…Whether we use all data, exclude tree rings, or base a reconstruction only on tree rings, has no significant effect on the form of the reconstruction for the period in question. (http://www.ngdc.noaa.gov/paleo/ei/ei_nodendro.html, emphasis added.)

Page 19: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Dominant PC weight on Bristlecones 70 series in the North American AD1400 network

15 are Graybill-Idso bristlecone/foxtail pines

In MBH method they account for 93% of PC1 weights; PC1 assigned 38% explained variance

Under conventional (covariance) PC method they fall to PC4 and get < 8% explained variance

Page 20: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Role of Bristlecones

Removing them eliminates the hockey stick shape from PCs and final reconstruction

Contradicts robustness claim

Page 21: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Role of bristlecones

From Mann’s FTP site (CENSORED folder)

Page 22: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Robustness

Burger and Cubasch (2005)

Page 23: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Confidence Intervals

Confidence intervals based on calibration-period residuals not verification-period residuals, thus understating actual uncertainty

Page 24: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Red Zone autocorrelation properties …

Modeled as ARMA(1,1), AR1 ρ > 0.9 in all cases and sometimes >0.97. Above figure: left- AR1 coefficient ρ; right – MA1 coefficient.

CRU J98 MBH99 MJ03 CL00 BJ00 BJ01 Esp02 Mob05

-1.0

0.0

1.0

Page 25: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Durbin-Watson Statistic

All multiproxy reconstructions as archived, except MBH99, fail Durbin-Watson statistic (minimum 1.5).

Passing a DW test is a necessary but not sufficient test of model validity.

J98 MBH99 MJ03 CL00 BJ00 BJ01 Esp02 Mob05

0.0

1.0

2.0

Page 26: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Cross-Validation R2 Statistic

Multiproxy reconstructions show decreased and insignificant cross-validation R2 statistics. BJ01 does not have MWP results and is reported not to verify after 1960. Left – calibration; right – verification R2.

J98 MBH99 MJ03 CL00 BJ00 BJ01 Esp02 Mob05

0.0

0.4

0.8

Cross-Validation R2

Page 27: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Replication

MBH results are not limited to a squiggly line: they include claims of skill and robustness

Ammann and Wahl claim to have replicated MBH results but they have only confirmed ours

Page 28: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Replication: Statistical Skill

Ammann and Wahl code yields the same conclusion as ours

There is no support for MBH skill claims

Verification RE

Verification R2 CE

MBH98 0.48 n.r. n.r.

MM05a Emulation 0.46 0.02 -0.26 Ammann&Wahl Code 0.47 0.02 -0.24

Page 29: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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SKILL: The dot.com reconstruction

Page 30: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Replication: Robustness

Ammann and Wahl code shows results hinge on bristlecones

There is no support for MBH claims of robustness

Page 31: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Problems with other studies

ReplicationRobustnessProxy selectionProxy validityLack of independence of authorship

and proxies

Page 32: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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MBH outputs used in other studies PC methods used in Mann and Jones (2003), Jones and

Mann (2004) PC series used in Rutherford et al. (2005) NOAMER PC1 used a few weeks ago in Osborne and

Briffa (2006, Science)

Page 33: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Greenland

Dahl-Jensen boreholes

Page 34: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Why do VZ differ?Did PC on decentered correlation matrix and

not on decentered data matrix: only the same if centered

Assumed >0.3 proxy correlation to temperature

Page 35: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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The “Divergence” Problem:large population of 387 temperature-sensitive sites

Page 36: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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The “Explanation” Briffa et al. (1998b) discuss various causes for this decline in tree growth parameters, and Vaganov et al. (1999) suggest a role for increasing winter snowfall.… In the absence of a substantiated explanation for the decline, we make the assumption that it is likely to be a response to some kind of recent anthropogenic forcing. On the basis of this assumption, the pre-twentieth century part of the reconstructions can be considered to be free from similar events and thus accurately represent past temperature variability. [Briffa et al. 2002]

Page 37: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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“Divergence” in action

Page 38: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Site Spaghetti: Polar Urals

Page 39: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Robustness?Little changes make big differences

Crowley & Lowery (2000) without bristlecones and Dunde

1000 1200 1400 1600 1800 2000

0.3

0.4

0.5

0.6

Page 40: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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End of Presentation

Medieval foxtail pineCalifornia

Thank you.

Page 41: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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Variance is already rescaled

CRU J98

0.0

0.2

0.4

CRU MBH 1902-80

0.0

0.2

0.4

Page 42: Stephen McIntyre Toronto Ontario Ross McKitrick Guelph Ontario Washington DC, March 2 2006

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CO2 Adjustment

MBH claim to have fixed bristlecone problem with CO2 adjustment.

What is CO2 adjustment in MBH99?