A high resolution absolute dating holocene and deglacial asian asian dating thai
record, but appears to be significantly less variable as the stacked temperature record of this study is unable to preserve climate variability occurring on timescales of less than 300 years.In panels E and F, the researchers compare their results with an additional four temperature reconstructions ranging in length from the past ~400 years to the past ~1900 years.
These studies have used temperature records from proxies, including tree rings and lake and ocean sediments.
In panels C and D, the researchers show how their results vary based on different methods of calculating the global temperature anomaly—the different methods result in different magnitude of temperature changes, particularly at the most recent end of the data set, but generally preserve the overall temperature trend.
In A and B, the researchers compare their results with a previous study—Mann .
Finally, they estimate temperatures for the end of the 21st century will be greater than those of any period from the Holocene.
Surface temperature reconstructions of the past 1500 years suggest that recent warming is unprecedented in that time.
(G and H) Number of records used to construct the Holocene global temperature stack through time (orange line) and Mann Panels A to F show the researchers’ Holocene temperature reconstructions in different ways.