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A list of all pages that have property "QCnotes" with value "Rejected - not 300 years long". Since there have been only a few results, also nearby values are displayed.

Showing below up to 26 results starting with #1.

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List of results

  • Ant 031dD.dD  + (MicS revised dating, NOAA National Climatic Data Center https://www.ncdc.noaa.gov/paleo/study/20246 (2016))
  • Ant 031.d18O  + (MicS revised dating, NOAA National Climatic Data Center https://www.ncdc.noaa.gov/paleo/study/20246 (2016))
  • Arc 073.temperature  + (Mind dating uncertainty)
  • Arc 040.temperature  + (Mind dating uncertainty)
  • Ocean2kHR 103.Sr Ca  + (NM: Marked as false because it has <50 years of continuous data)
  • Arc 016.trsgi  + (No low frequency;updated detrending in DArrigo et al. (2006) but data not available. Likely divergence issues but the only existing record from northeastern Siberia so it must be used to increase coverage.(FCL))
  • NAm 3760.MXD  + (No low-frequency signal. Elevation estimated from GoogleEarth; rounded to 100 m)
  • NAm 3748.MXD  + (No low-frequency signal. Elevation estimated from GoogleEarth; rounded to 100 m)
  • LPDa7a4074f.uncertainty temperature  + (Not a temperature proxy)
  • Asia 233.trsgi  + (Not a temperature proxy)
  • Ocean2kHR 139.d18O  + (Note: floating fossil coral sections have greater uncertainty in absolute temperature for palaeoclimate reconstructions (NJA))
  • Ocean2kHR 102.d18O  + (Note: floating fossil coral sections have greater uncertainty in absolute temperature for palaeoclimate reconstructions (NJA))
  • Ocean2kHR 007.d18O  + (Note: floating fossil coral sections have greater uncertainty in absolute temperature for palaeoclimate reconstructions (NJA))
  • Asia 236.d18O  + (Oxygen isotopes show positive correlation with NH temperature anomalies. Elevation estimated from GoogleEarth; rounded to 100 m)
  • NAm 880.trsgi  + (PI interp of climate sensitivity confirmed. Could be a gridded climate data problem)
  • NAm 868.trsgi  + (PI interp of climate sensitivity confirmed. Could be a gridded climate data problem)
  • NAm 664.trsgi  + (PI interp of climate sensitivity confirmed. Could be a gridded climate data problem)
  • NAm 628.trsgi  + (PI interp of climate sensitivity confirmed. Could be a gridded climate data problem)
  • NAm 052.trsgi  + (PI interp of climate sensitivity confirmed. Could be a gridded climate data problem)
  • NAm 3280.trsgi  + (Passes with McKenney ANUSPLIN, not coarse CRU.)
  • NAm 2056.MXD  + (Poor low frequency retention, but passes correlation and EPS screening)
  • Arc 053.temperature  + (QC under question, negative correlation to local temperature (FCL), should be negative accoriding to NickMcKay, keep it.)
  • Arc 023.trsgi  + (QC under question. Very weak correlation to temperature and not well described in the literature (FCL))
  • Arc 011.d18O  + (QC wait for VMD)
  • Eur 020.trsgi  + (Regional chronologies based on nested PCs …
    Regional chronologies based on nested PCs display high correlation coefficients in the two calibration periods: both regression-calibrated (r1900_1952 = 0.81 and r1953_2005 = 0.75 on average) and scaling-calibrated (r1900_1952 = 0.73 and r1953_2005 = 0.80 on average). Similarly REs are also high (well above 0) for the two verifications.
     (well above 0) for the two verifications.)
  • NAm 616.trsgi  + (Retain, climate data problem?)
  • NAm 640.trsgi  + (Retain, climate data problem?)
  • Eur 010.temperature  + (SST determinations based on the alkenone index UK37 indicate annual upwelling in tensity as the determinant factor for SST variability confirming the Tagus results (Abrantes et al. 2009))
  • NAm 028.trsgi  + (Salzer's composite from MWK PILO: https:// …
    Salzer's composite from MWK PILO: https://www.ncdc.noaa.gov/paleo/study/8518 ; Sheep Mountain PILO: https://www.ncdc.noaa.gov/paleo/study/8542 ; and PRL PILO: https://www.ncdc.noaa.gov/paleo/study/8541. Elevation estimated from GoogleEarth; rounded to 100 m
    timated from GoogleEarth; rounded to 100 m)
  • SAm 010.trsgi  + (Signal free detrending)
  • SAm 015.trsgi  + (Signal free detrending)
  • SAm 020.trsgi  + (Signal free detrending)
  • Asia 335.temperature  + (Species response to winter SST proved using redundancy analysis)
  • NAm 2824.trsgi  + (Still an early end effect. Might want to truncate?)
  • Arc 093.trsgi  + (Strong sign-to-noise ratio in the mean div …
    Strong sign-to-noise ratio in the mean divergence-free regional chronology (representing a network of 29 sites in the Mackenzie Delta region) with Expressed Population Signal (EPS) > 0.85 since AD 1400, and EPS > 0.7 back to AD 1245. The chronology shares a moderate to strong positive correlation with local summer temperatures (r = 0.6, p < 0.001) over the calibration period, and moderate to strong correlations with several other reconstructions from surrounding regions spanning the last millenium.
    om surrounding regions spanning the last millenium.)
  • NAm 2776.trsgi  + (Suspect climate data problems here, doesn't pass the local correlation test …)
  • Ant 029.temperature  + (Temp inferred from accumulation rate; defer to isotopes)
  • Africa 001.d18O  + (Temperature estimates determined using lin …
    Temperature estimates determined using linear regression between speleothem d18O and annual mean temperature. An "anomalous" period, from AD 1956-1976 was removed from this calibration. In the context of the Holocene, the application of this calibration results in temperature trends contrary to other published records for the last 10,000 years.
    blished records for the last 10,000 years.)
  • Asia 235.temperature  + (Temperature history of Kunashir Island based on the joint borehole temperature and tree-ring data. Elevation estimated from GoogleEarth; rounded to 100 m)
  • Eur 003.temperature  + (The average inferred July temperatures bet …
    The average inferred July temperatures between ca 1900 and 2001 AD were significantly warmer (p < 0.05) than the climate reference period (1961-1990) by 1C which is in agreement with the instrumental data. The inferred July temperatures were in the same range as the inferred temperatures during the last part of the MCA suggesting that during the 20th century at Lake Silvaplana the chironomid-inferred temperatures do not exceed the natural climate variability of the past millennium.
    l climate variability of the past millennium.)
  • Eur 014.MXD  + (The final reconstruction (N-scan) was calibrated against regional JJA temperature (r 1876_2006 = 0.77) and spans the 138 bc_ ad 2006 period.)
  • Eur 008.d18O  + (The positive correlation between 013C series of the stalagmites and the surface temperature series shown in the previous section is robust in the three samples but requires some further discussion.)
  • Eur 027.JulianDay  + (The temperature reconstruction is preferred from this site)
  • LPD775e8bad.year old  + (The timescale for the Common Era of WDC06A …
    The timescale for the Common Era of WDC06A was recently revised. The former timescale (“WDC06A-7”, Sigl et al., 2013) was based on manually interpreting annual-layers with multi-parameter aerosol records and was used in PAGES 2k Consortium (2013). This timescale is now replaced by a timescale (“WD2014”) based on the same aerosol datasets, but interpreted with an objective layer-counting algorithm and constrained with a distinctive, global-scale, marker horizon in 775 AD detected by annual 10Be ice-core measurements (see additional details in Sigl et al., 2015). During the first millennium WD2014 differs from WDC06A-7 by on average 7 years (maximum of 9 years), with the revised timescale giving always younger ages. The time period 1258 AD to present is identical for both timescales. WD2014 is considered more accurate than WDC06A-7 (Sigl et al., 2015), and is the recommended timescale, but both timescales are reported in the PAGES2k database Ant_031 and Ant_031WD2014.
    AGES2k database Ant_031 and Ant_031WD2014.)
  • Eur 001.d18O  + (The uppermost point marks the present-day …
    The uppermost point marks the present-day conditions in Spannagel at +1.8C and y18O= 7.8x. The average temperature in the Alps during the coldest period between 1688 and 1698 coincided with the Maunder Minimum. As derived from Luterbacher's data the average temperature in this period was 1.0 (F0.5) 8C about 1.8 8C lower than in the period between 1995 and 1998.
     than in the period between 1995 and 1998.)
  • LPD027eca7f.Uk37  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.)
  • LPD17d4c9be.notes  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.)
  • LPD1b77c35b.notes  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.)
  • LPD2d0bd641.Mg Ca  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.)
  • LPD35442a44.Uk37  + (These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.)
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