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A list of all pages that have property "QCnotes" with value "no climate signal, end of seires biased". Since there have been only a few results, also nearby values are displayed.

Showing below up to 49 results starting with #1.

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List of results

  • 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 194.Sr Ca  + (annually banded record; multi-annual resolution)
  • Ocean2kHR 193.d18O  + (annually banded record; multi-annual resolution)
  • Ocean2kHR 191.Sr Ca  + (annually banded record; multi-annual resolution; no information on water depth, but coral likely growing in < 10 m water depth)
  • Ocean2kHR 190.d18O  + (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 192.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 184.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 182.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 180.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 176.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 170.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 168.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 165.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 155.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 153.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 151.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 148.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 146.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 136.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 117.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 111.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 109.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 101.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 024.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 017.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 015.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 009.d13C  + (d13C: not SST sensitive)
  • Ocean2kHR 004.d13C  + (d13C: not SST sensitive)
  • Asia 305.d18O  + (d18O in ice core in northern Tibetan Plateau is a proxy of temperature. Elevation estimated from GoogleEarth; rounded to 100 m)
  • Asia 247.d18O  + (d18O in ice core in northern Tibetan Plateau is a proxy of temperature. Elevation estimated from GoogleEarth; rounded to 100 m)
  • Ocean2kHR 162.d18O  + (d18Osw (residuals calculated from coupled SrCa and d18O measurements))
  • Ocean2kHR 013.d18O  + (d18Osw is probably the primary control on d18O of the coral at this site; authors found positive relation btwn 18O and temperature, opposite the expected)
  • Asia 329.temperature  + (decadal resolution)
  • Asia 326.temperature  + (decadal resolution)
  • Asia 321.temperature  + (decadal resolution)
  • Asia 318.temperature  + (decadal resolution)
  • NAm 1072.MXD  + (local correlation p-value = 0.056, and correlates regionally)
  • NAm 2656.trsgi  + (minor EPS problems)
  • Arc 036.temperature  + (multi-decadal MAT, 50-year or so averages of exactly dated historical documentary information. A hiatus in the 15th and part of the 16th centuries (FCL))