Daniel1960, on 2013-May-06, 19:39, said:
A: Our study did not directly address this question because the paleotemperature records used in our study have a temporal resolution of ~120 years on average, which precludes us from examining variations in rates of change occurring within a century. Other factors also contribute to smoothing the proxy temperature signals contained in many of the records we used, such as organisms burrowing through deep-sea mud, and chronological uncertainties in the proxy records that tend to smooth the signals when compositing them into a globally averaged reconstruction. We showed that no temperature variability is preserved in our reconstruction at cycles shorter than 300 years, 50% is preserved at 1000-year time scales, and nearly all is preserved at 2000-year periods and longer. Our Monte-Carlo analysis accounts for these sources of uncertainty to yield a robust (albeit smoothed) global record. Any small “upticks” or “downticks” in temperature that last less than several hundred years in our compilation of paleoclimate data are probably not robust, as stated in the paper.
What exactly is your point? The Marcott study looks at 11300 years of global temperatures by use of proxies. The methodology does not allow for measurements of small variables in small increments by geological timeframes. Fortunately, we have had thermometers for the past 100 years so there is no need to look at fossil proxies to know what has occurred recently.
By comparing the Marcott study showing cooling against the known temperatures of the past 100 years the result shows a temperature spike that is unprecedented and is paralleled by the advent of the industrial revolution and increased greenhouse gas emissions caused by man.
Marcott states his study cannot determine what has happened in the last 100 years. By pointing that out, you appear to be observing that a Chicago roller coaster won't take you to the New York Central train station. O.K. I buy that. And your point is?