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A list of all pages that have property "QCnotes" with value "Truncate early portion with low sample depth, pass". Since there have been only a few results, also nearby values are displayed.

Showing below up to 103 results starting with #1.

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List of results

    • 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)
    • Ocean2kHR 136.d13C  + (d13C: not SST sensitive)
    • Ocean2kHR 146.d13C  + (d13C: not SST sensitive)
    • Ocean2kHR 148.d13C  + (d13C: not SST sensitive)
    • Ocean2kHR 151.d13C  + (d13C: not SST sensitive)
    • Ocean2kHR 153.d13C  + (d13C: not SST sensitive)
    • Ocean2kHR 155.d13C  + (d13C: not SST sensitive)
    • Ocean2kHR 165.d13C  + (d13C: not SST sensitive)
    • Ocean2kHR 168.d13C  + (d13C: not SST sensitive)
    • Ocean2kHR 170.d13C  + (d13C: not SST sensitive)
    • Ocean2kHR 176.d13C  + (d13C: not SST sensitive)
    • Ocean2kHR 180.d13C  + (d13C: not SST sensitive)
    • Ocean2kHR 182.d13C  + (d13C: not SST sensitive)
    • Ocean2kHR 184.d13C  + (d13C: not SST sensitive)
    • Ocean2kHR 192.d13C  + (d13C: not SST sensitive)
    • Asia 247.d18O  + (d18O in ice core in northern Tibetan Plateau is a proxy of temperature. Elevation estimated from GoogleEarth; rounded to 100 m)
    • Asia 305.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 318.temperature  + (decadal resolution)
    • Asia 321.temperature  + (decadal resolution)
    • Asia 326.temperature  + (decadal resolution)
    • Asia 329.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))
    • NAm 3712.trsgi  + (no climate signal, end of seires biased)
    • NAm 304.MXD  + (no low-freq retained)
    • NAm 1024.MXD  + (no low-frequency signal)
    • NAm 1108.trsgi  + (no low-frequency signal)
    • NAm 1120.MXD  + (no low-frequency signal)
    • NAm 1168.MXD  + (no low-frequency signal)
    • NAm 1492.MXD  + (no low-frequency signal)
    • NAm 1588.MXD  + (no low-frequency signal)
    • NAm 160.MXD  + (no low-frequency signal)
    • NAm 1636.trsgi  + (no low-frequency signal)
    • NAm 1648.MXD  + (no low-frequency signal)
    • NAm 1660.trsgi  + (no low-frequency signal)
    • NAm 1672.MXD  + (no low-frequency signal)
    • NAm 2080.MXD  + (no low-frequency signal)
    • NAm 2236.trsgi  + (no low-frequency signal)
    • NAm 2512.MXD  + (no low-frequency signal)
    • NAm 2704.MXD  + (no low-frequency signal)
    • NAm 2752.MXD  + (no low-frequency signal)
    • NAm 2800.MXD  + (no low-frequency signal)
    • NAm 2848.trsgi  + (no low-frequency signal)
    • NAm 3124.MXD  + (no low-frequency signal)
    • NAm 3244.MXD  + (no low-frequency signal)
    • NAm 3520.trsgi  + (no low-frequency signal)
    • NAm 3616.trsgi  + (no low-frequency signal)
    • NAm 3652.MXD  + (no low-frequency signal)
    • NAm 3700.MXD  + (no low-frequency signal)
    • NAm 520.MXD  + (no low-frequency signal)
    • NAm 568.MXD  + (no low-frequency signal)
    • NAm 760.MXD  + (no low-frequency signal)
    • NAm 976.MXD  + (no low-frequency signal)
    • NAm 088.MXD  + (poor low freq, but modern corr still good)
    • NAm 3867.temperature1  + (pre-European calibration set, validated by early climate data)
    • NAm 3868.temperature  + (pre-European calibration set, validated by early climate data)
    • Arc 100.temperature  + (replaces Esper 2002 and Briffa2008)
    • Arc 078.temperature  + (strong correlation. However, opposite long-term (orbital) trend to most other Arctic records (FCL))
    • Ocean2kHR 016.d18O  + (used in Tierney et al, as a composite with HR_014; the original records are provided here rather than composites)
    • Ocean2kHR 014.d18O  + (used in Tierney et al, as a composite with HR_016; the original records are provided here rather than composites)
    • Ocean2kHR 150.d18O  + (used in Tierney et al, as a composite with HR_147 and HR _152; the original records are provided here rather than composites)
    • Ocean2kHR 152.d18O  + (used in Tierney et al, as a composite with HR_147 and HR_150; the original records are provided here rather than composites)
    • Ocean2kHR 147.d18O  + (used in Tierney et al, as a composite with HR_150 and HR _152; the original records are provided here rather than composites)
    • Ocean2kHR 157.d18O  + (used in Tierney et al, as a composite with HR_156; the original records are provided here rather than composites)
    • Ocean2kHR 156.d18O  + (used in Tierney et al, as a composite with HR_157; the original records are provided here rather than composites)
    • Aus 071.trsgi  + (warm season T signal)
    • LPD692315c3.ageMax  + (yearOld_AD)
    • LPDb2294566.ageMin  + (yearYoung_AD)
    • Arc 057.density  + (Δdensity = MXD - minimum density, more focused summer temp. signal than MXD (Björklund et al., 2014, CP, doi:10.5194/cp-10-877-2014))
    • Arc 058.density  + (Δdensity = MXD - minimum density, more focused summer temp. signal than MXD (Björklund et al., 2014, CP, doi:10.5194/cp-10-877-2014))
    • Arc 059.density  + (Δdensity = MXD - minimum density, more focused summer temp. signal than MXD (Björklund et al., 2014, CP, doi:10.5194/cp-10-877-2014))
    • Arc 060.density  + (Δdensity = MXD - minimum density, more focused summer temp. signal than MXD (Björklund et al., 2014, CP, doi:10.5194/cp-10-877-2014))
    Retrieved from "https://wiki.linked.earth/Special:SearchByProperty/:QCnotes/Truncate-20early-20portion-20with-20low-20sample-20depth,-20pass"