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This page provides a simple browsing interface for finding entities described by a property and a named value. Other available search interfaces include the page property search, and the ask query builder.

List of results

• Arc 150.MXD  + (This MXD chronology supersedes Arc_019)
• Eur 017.trsgi  + (This composite record includes living trees historical timber and subfossil wood and correlates at 0.72 to 0.92 with interannual to multidecadal variations in instrumental June-to-August (JJA) temperature (1864_2003))
• Arc 025.X radiograph dark layer  + (Time series truncated at 1800 CE. Actual m …
  Time series truncated at 1800 CE. Actual measurement is not the thickness of the organic-rich layer as stated in orignial data citation. Instead, a measure of organic content within a year is estimated by the cumulative sum of the dark component of pixels of radiographs for each varve\
  t of pixels of radiographs for each varve\)
• NAm 1600.trsgi  + (Truncate early portion with low sample depth, pass)
• NAm 040.trsgi  + (Updated dataset by Salzer and Kipfmueller (2005) used in this study; temperature sensitivity reconfirmed by Salzer, despite poor correlation with coarse (TS3.2) reanalysis data over high-relief terrain.)
• Arc 065.d18O  + (Use Arc_66 (same location, other variable))
• Arc 075.thickness  + (Use calibrated temperatures instead of varve thickness)
• NAm 2008.trsgi  + (Use original chronology and truncate at 1700)
• NAm 2128.trsgi  + (Use original chronology. Neg temp relationship after 1950.)
• Eur 016.trsgi  + (Using AD 1901_1950 as the calibration period the Pearson's correlation coefficient between grid data and reconstruction is 0.34 and for verification is 0.47)

• Arc 024.thickness  + (Valid only for > 3yr time scales)

• Aus 010.trsgi  + (Warm season T signal. Elevation estimated from GoogleEarth; rounded to 100 m)
• Eur 002.temperature  + (We used multiple linear regression (MLR) t …
  We used multiple linear regression (MLR) to establish a calibration model that explains 84% of the variance of summer (JJAS) temperature during the calibration period 1864_1950. We then applied the calibration model downcore to develop a quantitative summer temperature reconstruction extending back to AD 1177.
  reconstruction extending back to AD 1177.)
• NAm 1852.trsgi  + (Weak temp relatinship with border line p-value.)
• Eur 007.temperature  + (When compared to local and regional instrumental records since ca 1760 AD significant (p < 0.01) relationships (rPearson > 0.5) are obtained suggesting that chironomids accurately register the changes in temperature for the past ca 250 years)
• Eur 019.trsgi  + (While the highest correlation of 0.53 is gained from the HISTALP southwest subset significantly lower correlation of 0.27 originates from the low-resolution HadCRUT3v data (Brohan et al. 2006) both against June_August temperature means.)
• LPD335d863f.RABD660 670  + (annual T signal is negative (note erratum to original paper). Relative absorption band depth from 660 to 670 nm is a proxy for concentration of chlorophyll a and its derivatives. Note data gap.)
• Ocean2kHR 193.d18O  + (annually banded record; multi-annual resolution)
• Ocean2kHR 194.Sr Ca  + (annually banded record; multi-annual resolution)
• Ocean2kHR 190.d18O  + (annually banded record; multi-annual resolution; no information on water depth, but coral likely growing in < 10 m water depth)
• Ocean2kHR 191.Sr Ca  + (annually banded record; multi-annual resolution; no information on water depth, but coral likely growing in < 10 m water depth)