Proxy-to-proxy calibration: Increasing the temporal resolution of quantitative climate reconstructions
Gunten
Lucien von
author
D'Andrea
William Joseph
author
Columbia University. Lamont-Doherty Earth Observatory
Bradley
Raymond S.
author
Huang
Yongsong
author
Columbia University. Lamont-Doherty Earth Observatory
originator
text
Articles
2012
English
High-resolution paleoclimate reconstructions are often restricted by the difficulties of sampling geologic archives in great detail and the analytical costs of processing large numbers of samples. Using sediments from Lake Braya Sų, Greenland, we introduce a new method that provides a quantitative high-resolution paleoclimate record by combining measurements of the alkenone unsaturation index (UK 37) with non-destructive scanning reflectance spectroscopic measurements in the visible range (VIS-RS). The proxy-to-proxy (PTP) method exploits two distinct calibrations: the in situ calibration of UK 37 to lake water temperature and the calibration of scanning VIS-RS data to down core UK 37 data. Using this approach, we produced a quantitative temperature record that is longer and has 5 times higher sampling resolution than the original UK 37 time series, thereby allowing detection of temperature variability in frequency bands characteristic of the AMO over the past 7,000 years.
Paleoclimate science
Scientific Reports
2
609
1
6
2012-08
http://dx.doi.org/10.1038/srep00609
http://hdl.handle.net/10022/AC:P:14820
NNC
NNC
2012-10-02 16:41:52 -0400
2012-10-08 10:18:14 -0400
8825
eng