Temperature record of the past 1000 years
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The temperature record of the past 1000 years describes the reconstruction of temperature for the last 1000 years on the Northern Hemisphere. A reconstruction is needed because a reliable surface temperature record exists only since about 1850. Studying past climate is of interest for scientists in order to improve the understanding of current climate variability and, relatedly, providing a better basis for future climate projections. In particular, if the nature and magnitude of natural climate variability can be established, scientists will be better positioned to identify and quantify human generated climate variability (commonly referred to as 'anthropogenic global warming' (AGW)).
The reconstructions of temperature of the last 1000 years vary between:
- ones with significant variability prior to the current century with particular warmth during the Medieval Warm Period and particular coolness during the Little Ice Age; and,
- ones with minimal variability prior to the current century, generally involving a slight cooling until the 20th century.
In all cases, the increase in temperature in the 20th century is the largest of any century in the record. This conclusion has now been strongly reinforced by the National Research Council's report to the U.S. Congress for 1600 onwards. The panel finds it plausible that this also holds on a millennium time scale, but notes that larger uncertainties reduce the confidence in these long-term comparisons [link].
- 1 Instrumental temperature record
- 2 General techniques
- 3 Reconstructions with minimal variability
- 4 Reconstructions with greater variability
- 5 Reconciliation of the two approaches
- 6 Criticism
- 6.1 Historical temperature estimates
- 6.2 Mann, Bradley and Hughes temperature reconstructions
- 6.3 National Research Council Report
- 7 External links
Instrumental temperature record
The recent instrumental temperature record dates from approximately 1850. These records of thermometer readings show a general warming in global temperatures.
For general information about temperature records see the main article: Temperature record.
General techniques
Reconstructions of temperature rely on 'proxy' records. For example, the width of tree rings is related to temperature as is the amount of snowfall over many glacial sites. Further, the isotopic composition of snow, corals, and stalactites can also record temperature changes. Other techniques which have been used include examining the time of crop harvests, the treeline in various locations and other historical records to make inferences about the temperature.
In general, the recent history of the proxy records is calibrated against local temperature records to estimate the relationship between temperature and the proxy. The longer history of the proxy is then used to reconstruct temperature from earlier periods. These records must then be averaged in some fashion if a "global" or "hemispheric" record is desired. Since certain regions contain, for example, a large number of tree ring records, a simple average of all the data would strongly over-weight some small regions - hence data-reduction techniques (PCA) are used to combine some of these regional records before they are globally combined.
An important distinction is between so-called 'multi-proxy' reconstructions, which attempt to obtain a global temperature reconstructions by using multiple proxy records distributed over the globe and more regional reconstructions.
Usually, the data are combined arithmetically, in some weighted average. More recently, Osborn and Briffa used a simpler technique, counting the proportion of records that are positive, negative or neutral in any time period [link]. This produces a result in general agreement with the conventional multi-proxy studies.
Reconstructions with minimal variability
Several reconstructions that suggested there was minimal variability in temperatures prior to the past century were generated by Mann and his co-authors. (See, for example, Mann, Jones and Briffa, Pollack et al. [link] [link].) More recently, they have extended their reconstructions to cover the last 2000 years (Mann and Jones, GRL, 2003 [link]). The work has recently been reproduced by Wahl and Ammann [link] [link].
The Mann, Bradley and Hughes (1998) version of the temperature record has an unofficial name, the "Hockey Stick" graph, first coined by Jerry Mahlman, a colleague of Mann's.
The work of Mann et al., Jones et al., Briffa and others [link] [link] forms a major part of the IPCC's conclusion that "the rate and magnitude of global or hemispheric surface 20th century warming is likely to have been the largest of the millennium, with the 1990s and 1998 likely to have been the warmest decade and year" [link]. In 2006, a National Academy of Sciences panel concluded that data was too sparse to fully support the decadal and single year conclusions. They did, however, find plausible the more general conclusion that the last 25 years have been the warmest for a millennium. (see below) [link] For a comparison of the common temperature plots, see [link].
Reconstructions with greater variability
In the 22 October 2004 issue of Science, Hans von Storch and his colleagues claimed that the particular method of Mann et al. probably underestimates the temperature fluctuations in the past by a factor of two or more; however, this conclusion rests at least in part on the reasonableness of the GCM simulation used, which has been questioned. Anders Moberg and his Swedish and Russian collaborators who published their results in Nature on February 10, 2005 [link] [link] have also generated reconstructions with significantly more variability than the reconstructions of Mann et al.
Scientists such as astrophysicist Sallie Baliunas have argued that these ups and downs correlate with solar activity and that the number of observed sunspots give us a rough measure of how bright the sun is. Balunias and others believe that periods of decreased solar radiation are responsible for historically recorded periods of cooling such as the Maunder Minimum and the Little Ice Age. Similarly, they say, periods of increase solar radiation contributed to the Medieval Warm Period, when Greenland's icy coastal areas thawed enough to permit farming and colonization.
Reconciliation of the two approaches
The apparent differences between the statistical and historical approaches are not fully reconciled. One possibility is that the fluctuations recorded in the historical records are regional rather than hemispheric in scale.
Criticism
The reconstructions mentioned above rely on various assumptions to generate their results. The most fundamental are that the proxy records vary linearly with temperature and that there are no non-temperature factors that confound the results. If these assumptions do not hold, the reconstructions would be unreliable.
Other criticisms are directed at the statistical methods employed in creating reconstructions. The methodology of papers by Mann et al (MBH98 and MBH99) have been criticised by Stephen McIntyre and Ross McKitrick (M&M) on various grounds. In the February 11, 2005 issue of Science, Richard A. Kerr discusses the Geophysical Research Letters paper that appeared on February 12, 2005 [link] by McIntyre and McKitrick. This has been reinforced by an independent team of statisticians led by Edward J. Wegman, George Mason University and chair of the National Academy of Sciences’ (NAS) Committee on Applied and Theoretical Statistics at the behest of Sen. Joe Barton. [link]
Mann counters that the criticisms directed at his statistical methodology are purely political and adds nothing new to the debate [link].
Historical temperature estimates
For information on the description of the Medieval Warm Period and Little Ice Age in various reports of the United Nations Intergovernmental Panel on Climate Change, see the main article: MWP and LIA in IPCC reports
Mann, Bradley and Hughes temperature reconstructions
[Quantitative hemispheric temperature reconstructions] were showing the pattern of slow cooling followed by more rapid warming.
Stephen McIntyre and Ross McKitrick attempted an audit of MBH98 [link] in [Corrections to the Mann et. al. (1998) Proxy Data Base and Northern Hemispheric Average Temperature Series]. This publication claimed various errors, but M&M offered no explanation as to why their analysis also differs from other reconstructions [link]. In turn, Mann (supported by Tim Osborn, Keith Briffa and Phil Jones of the Climatic Research Unit) has disputed the claims made by McIntyre and McKitrick [link] [link], saying "...MM have made critical errors in their analysis that have the effect of grossly distorting the reconstruction of MBH98...". In 2004 Mann, Bradley, and Hughes published a corrigendum to their Nature 392, 779-787 (1998) article, correcting a number of mistakes in the online supplementary information that accompanied their article but leaving the actual results unchanged.
M&M have published another Geophysical Research Letters article [link] on February 12, 2005, claiming that the "Hockey Stick" shape was a result of a flawed principal component analysis, and that using the same steps like Mann et al., they were able to obtain the Hockey Stick graph in 99 percent of cases even if red noise was used as input. Mann and his collaborators have responded to the M&M articles via various means, including posts at the blog [RealClimate].
In 2006, a panel report of the National Academy of Sciences ordered by the U.S. Congress was published. The basic conclusion of Mann et al. (1998, 1999) was that the late 20th century warmth in the Northern Hemisphere was unprecedented during at least the last 1,000 years. This conclusion has subsequently been supported by an array of evidence. The committee found it plausible that the Northern Hemisphere was warmer during the last few decades of the 20th century than during any comparable period over the preceding millennium. However the panel expressed reservations that uncertainties make it difficult to compare individual years and decades of the 20th century with any similarly short period prior to around 1600.
The report also confirmed some of the points of the criticism by M&M: the bristlecone pines are not a good temperature proxy; the data and the software should have been made available; and the principal component analysis as used by Mann et. al. "tends to bias the shape of the reconstruction", however this "does not appear to unduly influence reconstructions of hemispheric mean temperature" [link].
There is an ongoing debate about the details of the temperature record and the means of its reconstruction.
Updates
There are ongoing updates and future events related to the MBH work.- [RealClimate] - Climate scientists blog, including Mann
- [ClimateAudit] - McIntyre blog
National Research Council Report
These are the five conclusions of the NRC report. [link]
- The instrumentally measured warming of about 0.6°C during the 20th century is also reflected in borehole temperature measurements, the retreat of glaciers, and other observational evidence, and can be simulated with climate models.
- Large-scale surface temperature reconstructions yield a generally consistent picture of temperature trends during the preceding millennium, including relatively warm conditions centered around A.D. 1000 (identified by some as the “Medieval Warm Period”) and a relatively cold period (or “Little Ice Age”) centered around 1700. The existence and extent of a Little Ice Age from roughly 1500 to 1850 is supported by a wide variety of evidence including ice cores, tree rings, borehole temperatures, glacier length records, and historical documents. Evidence for regional warmth during medieval times can be found in a diverse but more limited set of records including ice cores, tree rings, marine sediments, and historical sources from Europe and Asia, but the exact timing and duration of warm periods may have varied from region to region, and the magnitude and geographic extent of the warmth are uncertain.
- It can be said with a high level of confidence that global mean surface temperature was higher during the last few decades of the 20th century than during any comparable period during the preceding four centuries. This statement is justified by the consistency of the evidence from a wide variety of geographically diverse proxies.
- Less confidence can be placed in large-scale surface temperature reconstructions for the period from A.D. 900 to 1600. Presently available proxy evidence indicates that temperatures at many, but not all, individual locations were higher during the past 25 years than during any period of comparable length since A.D. 900. The uncertainties associated with reconstructing hemispheric mean or global mean temperatures from these data increase substantially backward in time through this period and are not yet fully quantified.
- Very little confidence can be assigned to statements concerning the hemispheric mean or global mean surface temperature prior to about A.D. 900 because of sparse data coverage and because the uncertainties associated with proxy data and the methods used to analyze and combine them are larger than during more recent time periods.
External links
- [Mann's home page]
- [A collection of various reconstructions of global and local temperature from centuries on up:]
- [An NOAA collection of individual data records]
- [Supplementary information] for Mann, M. E. et al. corrigendum: Global-scale temperature patterns and climate forcing over the past six centuries Nature 430, 105(2004) Letters to Nature. http://www.nature.com/nature/journal/v430/n6995/suppinfo/nature02478.html
- [Corrections to the Mann et al (1998) Proxy Data Base and Northern Hemisphere Average Temperature Series]. Steven McIntyre, Ross McKitrick. Energy and Environment 14(6) 751-772. http://www.uoguelph.ca/~rmckitri/research/trc.html
- http://www.climate2003.com/ Webpage of Stephen McIntyre
- http://www.realclimate.org/index.php?p=98 - comment by Mann on M&M on "RealClimate" blog
- ["A Global Warming Bombshell"] by Richard A. Muller, Technology Review , Oct. 2004; calls into question famous graph by Michael Mann
- [What is the ‘Hockey Stick’ Debate About?] McKitrick reviews the criticisms of the Mann hockey stick for a general scientific audience.
- [Rebuttal of the McIntyre and McKitrick dispute of the "Hockey Stick" extrapolation] — Real Climate
- [Was the climate of the 20th century unusual?]
- [Surface Temperature Reconstructions for the Last 2,000 Years]
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