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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

• O2kLR 137.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to LPD30c5b95c; Datapoints close to 0 CE are not constrained and hence not included)
• LPDb44bf261.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to LPD57d40973)
• LPDe6c52b99.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to LPD7c7e19c5)
• LPD09e5a770.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to LPDa03ec713)
• LPDa97364db.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to LPDa2107e77)
• LPDd95394f2.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to LPDbd07f717)
• LPD708fb697.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to LPDe51d17e8)
• LPDc07746c5.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to LPDefb3d2b0)
• LPD9b023bc9.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to LPDf7bace53)
• O2kLR 019.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to O2kLR_017)
• O2kLR 032.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to O2kLR_030; Dataset truncated at -200 CE)
• O2kLR 068.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to O2kLR_066)
• O2kLR 076.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to O2kLR_074)
• O2kLR 149.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to O2kLR_148)
• O2kLR 177.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to O2kLR_175; Truncated at -200 CE)
• O2kLR 107.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Inadequate chronological constraints at the top of the core to include all data points)
• O2kLR 189.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Inadequate chronological constraints, final record that was entered contained an updated age model and dating constraints;)
• O2kLR 152.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.SST data is in anomaly-space and is not mean-shifted/raw)
• LPD6dbf8788.temperature  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Separate cores not combined in this dataset; Not QC)
• 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)
• Aus 067.trsgi  + (composite series, warm season T signal, approximate average/centroid values entered in elevation, lat and lon fields for completeness)
• Aus 062.trsgi  + (composite series, warm season T signal, elevation range 210-1060 m, approximate average/centroid values entered in elevation, lat and lon fields for completeness)
• Ocean2kHR 004.d13C  + (d13C: not SST sensitive)
• Ocean2kHR 009.d13C  + (d13C: not SST sensitive)
• Ocean2kHR 015.d13C  + (d13C: not SST sensitive)
• Ocean2kHR 017.d13C  + (d13C: not SST sensitive)
• Ocean2kHR 024.d13C  + (d13C: not SST sensitive)
• Ocean2kHR 101.d13C  + (d13C: not SST sensitive)
• Ocean2kHR 109.d13C  + (d13C: not SST sensitive)
• Ocean2kHR 111.d13C  + (d13C: not SST sensitive)
• Ocean2kHR 117.d13C  + (d13C: not SST sensitive)