mheslep
Gold Member
- 364
- 719
Ah, finally a new page! Guys let's shrink those image posts that explode the page width?
Okay, here's the entire tail end of the http://dels.nas.edu/dels/rpt_briefs/Surface_Temps_final.pdf" without omission. I think it is helpful to post here.
Then note the last part I bold faced. The 'less confidence' in that sentence from the NA does not refer to the wide error bars Mann et al associated with its prior to 1600AD estimates, but rather it refers to the high time resolution claims made in Mann et al's use of the terms 'decade' and 'year', i.e., because not all of the proxies record "information on such short timescales." Specifically on this point of making claims re short timescales, NA is not in agreement with Mann et al.
NA also prefers the word "plausible" over "likely" about the warmest period in a 1000 years. As an amateur, I agree.
Okay, here's the entire tail end of the http://dels.nas.edu/dels/rpt_briefs/Surface_Temps_final.pdf" without omission. I think it is helpful to post here.
In addition to this text, the NA report includes Figure S-1 showing other well known reconstructions in which at least two, Moberg et al and Esper et al, are showing circa 1000AD was the warmest part of their proxy reconstructions in the last 1000 years (though they may end in 1980?)NA Report said:[...]
o 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.
The main reason that our confidence in large-scale surface temperature reconstructions
is lower before A.D. 1600 and especially before A.D. 900 is the relative scarcity of precisely
dated proxy evidence. Other factors limiting our confidence in surface temperature reconstructions include the relatively short length of the instrumental record (which is used to calibrate and validate the reconstructions); the fact that all proxies are influenced by a variety of climate variables; the possibility that the relationship between proxy data and local surface temperatures may have varied over time; the lack of agreement as to which methods are most appropriate for calibrating and validating large-scale reconstructions
and for selecting the proxy data to include; and the difficulties associated with constructing
a global or hemispheric mean temperature estimate using data from a limited number of sites and with varying chronological precision. All of these considerations introduce uncertainties that are difficult to quantify.
Despite these limitations, the committee finds that efforts to reconstruct temperature histories for broad geographic regions using multiproxy methods are an important contribution to climate research and that these large-scale surface temperature reconstructions contain meaningful climatic signals. The individual proxy series used to create these reconstructions generally exhibit strong correlations with local environmental conditions, and in most cases there is a physical, chemical, or physiological reason why the proxy reflects local temperature variations. Our confidence in the results of these reconstructions becomes stronger when multiple independent lines of evidence point to the same general result, as in the case of the Little Ice Age cooling and the 20th century warming.
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 that includes both additional large-scale surface temperature reconstructions and pronounced changes in a variety of local proxy indicators, such as melting on icecaps and the retreat of glaciers around the world, which in many cases appear to be unprecedented during at least the last 2,000 years. Not all individual proxy records indicate that the recent warmth is unprecedented, although a larger fraction of geographically diverse sites experienced exceptional warmth during the late 20th century than during any other extended period from A.D. 900 onward.
Based on the analyses presented in the original papers by Mann et al. and this newer supporting evidence, the committee finds 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. The substantial uncertainties currently present in the quantitative assessment of large scale surface temperature changes prior to about A.D. 1600 lower our confidence in this conclusion compared to the high level of confidence we place in the Little Ice Age cooling and 20th century warming. Even less confidence can be placed in the original conclusions by Mann et al. (1999) that “the 1990s are likely the warmest decade, and 1998 the warmest year, in at least a millennium” because the uncertainties inherent in temperature reconstructions for individual years and decades are larger than those for longer time periods, and because not all of the available proxies record temperature information on such short timescales.
Then note the last part I bold faced. The 'less confidence' in that sentence from the NA does not refer to the wide error bars Mann et al associated with its prior to 1600AD estimates, but rather it refers to the high time resolution claims made in Mann et al's use of the terms 'decade' and 'year', i.e., because not all of the proxies record "information on such short timescales." Specifically on this point of making claims re short timescales, NA is not in agreement with Mann et al.
NA also prefers the word "plausible" over "likely" about the warmest period in a 1000 years. As an amateur, I agree.
Last edited by a moderator: