The NAS Panel claimed that MBH98 was the "first systematic" multiproxy study. It wasn’t; it didn’t even claim to be, citing Bradley and Jones 1993 and several other studies of the same vintage as predecessors. Crowley was a peer reviewer for the NAS panel, who presumably relied on him to catch this sort of mis-step. He should have caught this, but didn’t. So what was the distinctive contribution of MBH98 – if it wasn’t the “first” multiproxy study?
Rather than going at this from the point of view of statistical methods as I’ve spent most of my time doing recently, I’ve gone back to basics and looked at proxy selection. When you look at the proxy series in the studies leading up to MBH98 (and in the contemporary and somewhat rival Jones et al 1998), it’s remarkable to see how many series were taken directly from Bradley and Jones 1993 and the degree of overlap between the proxy selections. There are a couple of surprising conclusions that emerge from a simple parsing and comparison of selections.
Summary of Proxy Selections
The table below summarizes proxies by class for Bradley and Jones 1993, Barnett et al 1995 (coauthored by Jones), Jones et al 1998, Mann, Park and Bradley 1995 and MBH98. It’s curious that Bradley and Jones join forces in 1993, then seem to fall somewhat competitive paths over the next few years, before Mann and Jones re-joining forces in Mann and Jones 2003. Diaz and Bradley 1992 is reported in the NAS 1995 volume about which I posted a couple of days ago. Rob Wilson wrote me offline objecting to the fact that the chronologies discussed in the NAS 1995 volume were "limited", but, as you will see, these were nonetheless the core of the 1998 studies that were relied upon by IPCC TAR.
I’ve summarized the number of proxies in each study by different proxy classes. Most lables are self explanatory. I’ve distinguished ice cores into two classes: melt percentage and isotopic (dO18). Isotopic dO18 series were not used in Bradley and Jones 1993 and some concerns about dO18 as as a temperature proxy were expressed in the earlier literature (and have re-surfaced in recent literature for tropical ice cores); they became incresingly used.
I’ve divided tree ring series into 4 different classses: "tree ring temperature reconstructions" are series where tree ring site chronologies have been used to reconstruct gridcell temperatures. These reconstructions are linear combinations of one or a small number of site chronologies, but there has been at least a pretence of linking the site chronology to temperature. "Precipitation reconstructions" are self-explanatory. I’ve shown "site chronologies" and "PC series" separately, as in these cases, these are merely chronologies and do not themselves indicate any prior attempt to link the site chronology (or PC series) to temperature. I’ve provided separate summaries for the total network and the 15th century networks, after which I’ll comment on the choices and evolution.
Quickly, you’ll see that Bradley and Jones 1993 used 23 proxies. The majority continued in use in Barnett et al 1995, Jones et al 1998 on the one hand and Mann et al 1995 and MBH98. MBH98 differs from the other studies in that the coverage is far less homogeneous with the number of proxies going from 22 in the AD1400 step to 112 in the AD1820 step; while MBH98 uses virtually all the Bradley and Jones series, it introduces many new series – and these selections are interesting to consider.
Table 1. Proxy Types in 1990s Multiproxy Studies
|Ice Core Melt/Accum||2||4||4||2||4||4|
|Ice Core dO18||4||0||0||2||2||5|
|Tree Ring Temperature Recons||10||9||9||8||8||9|
|Tree Ring Precipitation Recons||0||0||0||0||0||3|
|Tree Ring Site Chronologies||0||0||0||0||11||27|
|Tree Ring PCs||0||0||0||0||0||31|
Table 2. For the Fifteenth Century
|Ice Core Melt/Accum||1||3||3||1||1||3|
|Ice Core dO18||2||0||0||1||1||3|
|Tree Ring Temperature Recons||4||4||4||5||3||4|
|Tree Ring Precipitation Recons||0||0||0||0||0||3|
|Tree Ring Site Chronologues||0||0||0||0||0||6|
|Tree Ring PCs||0||0||0||0||0||3|
PROXIES WHERE MBH98 IS MOSTLY SIMILAR
In many of the proxy classes, MBH98 selections are virtually identical to the other studies; I’ll consider these first and then consider proxy classes where major differences arise.
Tree Ring Temperature Reconstructions
The tree ring temperature reconstructions selected in Bradley and Jones 1993 provide a common core to all these studies. All 9 temperature reconstructions in Bradley and Jones 1993 are used either directly in MBH98 (8 cases) or, in the case of the Jacoby treeline reconstruction, by splitting the reconstruction into 11 component chronologies.
The tree ring temperature reconstructions in Bradley and Jones 1993 are mostly familiar to readers of this blog: Polar Urals, Tornetrask (Briffa), Jacoby’s North American treeline composite, Briffa’s North American reconstruction (MXD), Fritts North American reconstruction(RW), Cook’s Tasmania reconstruction, Norton and Palmer’s New Zealand reconstruction and two South American reconstructions from Villalba from Patagonia and Rio Alerce.
The basic selection framework was already set out in Diaz and Bradley 1992. The only Bradley and Jones 1993 series not in Diaz and Bradley 1992 is the Norton and Palmer series; otherwise, the only other change is the consolidation of 3 regional Fritts series listed in Diaz and Bradley 1992 into one series in Bradley and Jones 1993.
Barnett et al 1995 used the identical set of tree ring proxies as Bradley and Jones 1993.
Mann et al 1995 used 8 of the 9 Bradley and Jones tree ring reconstructions — they only dropped the Fritts reconstruction (re-inserted in MBH98). They added one new tree ring series — Kolyma River, Russia, also carried forward into MBH98. However, Mann et al 1995 made one major change presaging MBH98 — instead of using the Jacoby temperature reconstruction as one series, they split them into 11 component site chronologies. The listing in Mann’s thesis shows all the versions as extending from 1515-1982 (but this is probably not correct as a number of chronologies don’t start that early. A 1515 start is also later than some series – Gaspé, in particular, start in MBH98.)
Jones et al 1998, one of the “independent” reconstructions in most spaghetti graphs, used 6 of the 9 tree ring reconstructions of Bradley and Jones 1993. It added the Jasper, Alberta reconstruction of Luckman et al, which becomes used in nearly every subsequent study (but is not used in MBH98), and a Lenca, Chile reconstruction which is not used in subsequent studies. (One has HS, the other doesn’t). Discontinued between Bradley and Jones 1993 and Jones et al 1998 are the Fritts reconstruction and the Northern Patagonia (araucaria) reconstruction. Also, the Briffa et al 1995 version of Polar Urals replaced the Graybill and Shiyatov version (a switch also made in MBH98).
MBH98 did not use any tree ring temperature reconstructions not used in previous studies. The only tree ring temperature reconstruction not used in Bradley and Jones 1993 is the Kolyma River reconstruction. As noted above, the Jacoby treeline reconstruction is replaced by 11 individual site chronologies, themselves not individually calibrated to temperature. The Polar Urals version of Briffa et al 1995 is substitued for the earlier Graybill and Shiyatov version. Otherwise, my surmise is that identical digital versions were used in both studies.
As noted above, Rob Wilson complained that the temperature reconstructions discussed in the NAS1995 were not necessarily constructed according to methods better suited to extracting millennial information. Maybe so. But there was NO material change in the versinos used in MBH98 and Jones et al 1998. So the better question is: if these studies don’t capture centennial variation, why was MBH98 able to extract a HS from them?
Corals have very short coverage – none go back to the MWP. They merely enhance the appearance of being "multiproxy".
In Bradley and Jones 1993, no coral series were used. Two series were introduced in Barnett et al 1995 (Great Barrier Reef, Galapagos). The same two series were used in Mann et al 1995 and were carried forward to MBH98 and Jones et al 1998. Jones et al 1998 added a coral series from New Caledonia, also used in MBH98. MBH98 added 6 other coral series, including a C-13 series with a very strong HS.
None of the coral series affect 15th century results.
Here there is somewhat of a change from Bradley and Jones 1993, with a de-emphasis of documentary series in the later studies.
Bradley and Jones 1993 had 9 documentary series – the most of any of the studies, even MBH98. In addition to the Central England and Central Europe series (used by all subsequent studies), they used one Russian, five Chinese and one Japanese documentary series.
Barnett et al cut back to 5 documentary series, dropping the Russian, Japanese and two Chinese series. Mann et al 1995 cut back to 7, dropping the Russian and Japanese series. Both Jones et al 1998 and MBH98 cut back further, just to the two European series, both of which had annual resolution, whereas the others were reported in decadal versions.
Two Chinese series made a re-appearance in Jones and Mann 2004. I’ve only been able to locate digital versions of 4 documnetary series – these two and the two European series.
Bradley and Jones 1993 used 4 ice core series based on melt percentage (Agassiz, Devon, Greenland (Kameda) and Svalbard) and did not use any isotopic dO18 series. This was a departure from Diaz and Bradley 1992 which used two melt series (Agassiz, Devon), but also used 4 isotopic series (Camp Century and Milcent, Greenland; Quelccaya, Dunde).
Barnett et al 1995 used the same 4 melt series as Bradley and Joens 1993, as did Mann et al 1995, which additionally used two isotopic series (Quelccaya, Dunde).
Jones et al 1998 dropped two ice core melt series (Agassiz, Devon) both of which had 5-year resolution; and used two different isotope series (Fisher’s Greenland stack, which included Milcent, and Law Dome, Antarctica).
MBH98 also dropped the two ice core melt series with 5 year resolution; also added Fisher’s Greenland stack. Strangely, where Mann et al 1995 had used one Quelccaya series, MBH98 used 4 different series from the same site: different dO18 series from two nearby cores; and two accumulation series from the same cores. These were not pre-processed into one index. Why would 4 different series from Quelccaya be used? Isn’t the theory of "teleconnections" being taken to its reducito ad absurdum if two cores only tens of meters apart can be taken to record different teleconnections with climate fields all over the world?
The Dunde series continued in use in later studies as a strong component of the Yang Chinese composite. The Agassiz melt series, after falling out of favor, re-emerged in Moberg et al 2005, where it is one of the largest single contributors to 20th century HS.
A low-frequency temperature reconstruction from sediments (Cloud Lake) in Bradley and Jones 1993, is not used further except in Mann et al 1995. Some sediment series recur in later studies (Crowley and Lowery 2000; and especially Moberg et al 2005)
PROXIES WHERE MBH98 IS DIFFERENT
So far the proxy usage in MBH98 is remarkably similar to the other sites and within the range of variability of the other studies. Now it gets interesting – here are the differences.
Unlike the other studies, MBH98 included a large number of long instrumental temperature series (although the Central England “documentary” series, used in many studies, is, through most of its history, an instrumental series, and, in this case, the distinction between documentary and instrumental is a bit arbitrary.) In addition to the Central England series, MBH98 included 11 long instrumental series as “proxies”.
This has always caused a bit of controversy, even among pliant climate scientists. However, the impact of using instrumental temperature series is a little different than people thinkg, though I will only allude to it here. Although actual instrumental results for 12 gridcells are available to it, MBH98 methods do not really "peek" at the answer. If I recall correctly, the North American PC1 is weighted more strongly in (say) the reconstruction of 18th century Vienna gridcell reconstruction than the available local instrumental measurements. Some instrumental temperature series actually have negative coefficients in contributing to the final reconstruction (which are more strongly influenced by tree ring PC1s.)
The use of instrumental temperature series as a “proxy” is an MBH innovation and one that has not been followed in other studies (other than the continued use of the Central England series as a "proxy").
An unusual and undiscussed MBH98 innovation is the use of instrumental precipitation series in a temperature reconstruction. I guess this is part of theory of "teleconnections". In introducing instrumental precipitation as a temperature proxy, MBH98 did not require that any evidence of a relationship to gridcell temperature be proved. Proving such connections would have been difficult as MBH98 had incorrect gridcell assignments for most of its instrumental precipitation series – sometimes bizarrely so. The Paris precipitation series was re-located to the New England gridcell (“The rain from Maine falls mainly in the Seine”). The Toulouse series was re-located to South Carolina. Identifying these mislocations was not easy as MBH provided incorrect data citations and, even in the Corrigendum, have refused to provide sources for their precipitation data (other than "NOAA"). Their series attributed to Bombay comes from somewhere else – perhaps Philadelphia. Teleconnections indeed.
The MBH98 innovation of using instrumental precipitation series in a temperature reconstruction was not continued in later studies, other than studies by Mann or Ammann continuing the use of the MBH98 network (Rutherford et al 2005, Wahl and Ammann 2006).
Tree Ring Precipitation Reconstructions
Another MBH98 innovation, related to their use of instrumental precipitation records, was their use of tree ring precipitation reconstructions. Here I’m not talking about site chronologies which may be affected by precipitation, but by series actually denominated in mm of precipitation, calculated by relating tree ring chronologies to instrumental precipitation records. Three such series were used in MBH98, all of which were in the 15th century network.
Again, this innovation was not continued other than in Rutherford et al 2005 and Wahl and Ammann 2006.
Tree Ring Site Chronologies
In addition to the 11 Jacoby site chronologies used individually, MBH98 used 16 individual site chronologies – here I’m contrasting the direct use of a chronology with a tree ring temperature reconstruction where the site chronology has been related to gridcell temperature and the resulting series is expressed in deg C. I’m also distinguishing the direct use of a site chronology from its use as part of a tree ring regional network.
In some cases, the individual chronologies have been identified in the literature as precipitation-related (e.g. the Moroccan site chronologies.)
It’s hard to see why some sites are used individually, while others are included in tree ring networks for principal component summarization and some are used more than once. The sites used in the precipitation reconstructions mentioned above are also used in the NOAMER principal components network. The Gaspé site is used individually and in the NOAMER network. Spruce Canyon is used in the NOAMER and STAHLE networks. There’s no obvious rhyme or reason to the methods. Some sites listed as being used are not used and the explanation in the Corrigendum is false.
The use of uncalibrated site chronologies also opens up other potential problems – non-normality, nonlinearity. There was surely an impression attached to MBH98 that some process of checking for the validity of proxies had taken place and some series had had such checking. But then there was the vast unflux of uncalibrated site chronologies. This is the first such use. After MBH98, one starts to see more use of uncalibrated site chronologies, reserving a "check" only for the final answer.
Tree Ring Principal Component Series
The other big innovation of MBH98 was simply throwing vast populations of disparate tree ring chronologies into a hopper, applying an unsupervised algorithm to them (which in their case was the biased MBH principal components method) and then using the resultant PC series without verifying that they had any connection to temperature. Prior to MBH98, there was no suggestion that something like this could be done. The relevant test for a temperature series is not whether it is "significant" under Preisendorfer’s Rule N as a pattern within a network, but whether it is a temperature proxy. This point has been debated at length in the past 2 years. However, here, I’m just noting that, prior to MBH98, even climate scientists made some attempt to ensure that proxies were temperature proxies.
Although MBH purported to rely on prior peer-reviewed literature, the grab-bag of series in the principal component networks and the PC series themselves were never reviewed prior to their use in MBH98. We made this point in our EE 2005 article as follows (and the associated illustration is worth reviewing):
Despite the reliance of MBH98 on the North American PC1, the validity of this series as a temperature proxy was not independently established in peer-reviewed literature….The strong negative bias of the MBH98 PC1 is evident in comparison to the Briffa reconstruction. The strong negative bias of the MBH98 PC1 is also evident in periods where we have instrumental records in North America. There is no reason to believe that average temperatures in the 18th century were negative 3 standard deviation units.
Original caption. Figure 6. Solid: North American temperature reconstruction of Briffa et al. [1992a]. Dashed: the MBH98 North American PC1. All series smoothed with a 25-year Gaussian filter. Both series are standardized by subtracting the 1902-1980 mean and dividing by the 1902-1980 standard deviation (re-scaling is not an issue here, since the PC calculations have already been done.)
A hidden result of the tree ring grab-bag networks in which anything could be dumped in was the introduction of bristlecones into temperature reconstructions – a definite MBH98 innovation. Caveats had been expressed about CO2 fertilization at the highest levels of the climate reconstruction world (even IPCC 2AR). There were explicit cautions about them in the specialist literature. None of the predecessor studies used bristlecones. This in itself is an extraordinary and remarkable finding that even I had not explicitly considered before. think about it – none of the temperature reconstructions in any multiproxy reconstruction prior to MBH98 used bristlecones (or foxtails).
Afterwards, bristlecones (and foxtails) became commonplace – Crowley and Lowery 2000, Esper et al 2002, Cook et al 2004, Moberg et al 2005, Rutherford et al 2005, Hegerl et al 2006, Osborn and Briffa 2006. These weren’t recent collections (they were mostly done in the mid-1980s by Graybill); but they were introduced into multiproxy studies by MBH98. They were not re-introduced explicitly but through these "networks" and principal component analysis applied to the networks – deep cover indeed.
Overall, what’s new about the proxies in MBH98? Many of the proxies overlap with Bradley and Jones 1993 and Jones et al 1998. Indeed, 14 of 17 proxies in Jones et al 1998 are also used in MBH98. The distinctive features of MBH98 proxy selection appear in retrospect to be the following:
· the use of proxies without any effort to ensure that they were temperature proxies, including even using instrumental precipitation series, taken to the extreme of even using grab-bag "networks";
· the ignoring of specialist warnings about bristlecones, previously excluded from every multiproxy study, and their introduction into multiproxy studies under deep cover.
Diaz and Bradley 1992 Documenting Natural Climatic Variations: How Different is the Climate of the Twentieth Century from That of Previous Centuries?in National Academy of Sciences 1995. Natural Climate Variability on Decade-to-Century Time Scales (1995) http://darwin.nap.edu/books/0309054494/html/17.html
Barnett, T. P., Santer, B., Jones, P. D., Bradley, R. S. & Briffa, K. R. Estimates of low frequency natural variability in near-surface air temperature. Holocene 6, 255–263 (1996).
Mann, M. E., Park, J. & Bradley, R. S. Global interdecadal and century-scale oscillations during the past five centuries. Nature 378, 266–270 (1995). Series are listed in chapter 3 of Mann’s thesis available from Mann’s FTP site.
Bradley, R. S. & Jones, P. D. “ÅLittle Ice Age’ summer temperature variations: their nature and relevance to recent global warming trends. Holocene 3, 367–376 (1993).
Hughes, M. K. & Diaz, H. F. Was there a “ÅMedieval Warm Period’ and if so, where and when? Clim. Change 26, 109–142 (1994).
Diaz, H. F. & Pulwarty, R. S. An analysis of the time scales of variability in centuries-long ENSO-sensitive records in the last 1000 years. Clim. Change 26, 317–342 (1994).