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A list of all pages that have property "QCnotes" with value "MXD record replaces the TRW; duplicate record omited from EuroMed". Since there have been only a few results, also nearby values are displayed.

Showing below up to 51 results starting with #1.

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List of results

  • O2kLR 175.temperature  + (HVM, BM, 20/4/2016 Pacific1580Isono2009_KR02-06A MC GC The authors combined the multicore and gravity core data (both cores from same location).)
  • O2kLR 183.temperature  + (HVM, BM, 20/4/2016 Pacific1582Zhao2000_Hen
    HVM, BM, 20/4/2016 Pacific1582Zhao2000_Hendy2012_Schimmelmann2013_SABA87-2, SABA88-1 Zhao et al., (2000) alkenone record with the age model from Hendy et al., (2012) and Schimmelmann et al., (2013). Combination of two cores (SABA87-2 and SABA88-1) recovered from the same drill site. Data sorted based on age.
    same drill site. Data sorted based on age.)
  • O2kLR 187.temperature  + (HVM, BM, 20/4/2016 Southern0045aLamy2002_GeoB3313-1)
  • LPD2a3997a7.temperature  + (HVM, BM, 20/4/2016 Southern0483aShevenell2011_ODP 1098B We used the publically archived data from PANGAEA, dated 2011.)
  • O2kLR 195.temperature  + (HVM, BM, 20/4/2016 Southern0485aMohtadi2007_GeoB7186-3)
  • LPD6315f935.temperature  + (HVM, BM, 20/4/2016 Southern1159aSepulveda2009_CF7-PC33)
  • O2kLR 045.temperature  + (HVM, BM, 20/4/2016; MSS, 07/10/2016; Atlan
    HVM, BM, 20/4/2016; MSS, 07/10/2016; Atlantic0234Sicre2011__MD99-2275_alkenone Sicre et al., (2011) (alkenone) was selected and not Jiang et al., (2005) (diatoms) for core MD22-9975. Sicre et al., (2011) has a much higher resolution record but both records show the same trend. Diatoms have now been published at higher resolution by Jiang et al (2015; Geology, doi: doi:10.1130/G36377.1) after the completion of the compilation.
    ) after the completion of the compilation.)
  • O2kLR 148.temperature  + (HVM, BM, 20/4/2016Pacific0335aOppo2009_MC31,BJ8-03-32GGC,BJ8-03-34GGC Combination of Oppo et al., (2009) data from the three cores recovered from the same drill site. Data sorted based on age.)
  • Asia 230.temperature  + (Half-centennial resolution. Elevation estimated from GoogleEarth; rounded to 100 m)
  • Eur 009.d18O  + (Here we reconstruct thermocline temperature and salinity in this region from AD 818 to 1780 using paired _18O and Mg/Ca ratio measurements of foraminifer shells from a subdecadally resolved marine sediment core.)
  • Asia 237.dust  + (Hydro climate)
  • Eur 026.temperature  + (In order to extend the Tallinn temperature
    In order to extend the Tallinn temperature series backward in time three different climate proxies were used. These were: the first day of ice break-up in Tallinn port a proxy for the mean winter air temperature (December to March); the first day of ice break-up on the rivers in northern Estonia a proxy for the beginning of spring; and the first day of the rye harvest a proxy for the mean air temperature in spring and summer (April to July). On the basis of these proxies the mean winter temperature could be extended back to the year AD 1500 and the spring and summer temperature back to 1731.
    pring and summer temperature back to 1731.)
  • LPDfc71e6bc.calcification2  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPDf7af3f2e.calcification1  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPDf316b97e.calcification4  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPDf2047c95.calcification2  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPDe897b7c7.calcification3  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPDe85bf987.calcification3  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPDdcf3abca.calcification5  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPDd376af3b.calcification3  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPDc95b8887.calcification3  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPDae761fd0.calcification3  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPD81e7ab49.calcification1  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPD7d948e2c.calcification3  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPD7be6185d.calcification1  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPD796b99d7.calcification2  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPD74bc6584.calcification5  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPD7457ad38.calcification4  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPD7311e829.calcification4  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPD72b1e1cd.calcification1  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPD70878a8b.calcification1  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPD6c1fc0ed.calcification2  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPD5024de7f.calcification6  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPD41213ce8.calcification2  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPD33714919.calcification2  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPD2757d69f.calcification4  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPD21b789e2.calcification1  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPD1079b4bb.calcification4  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • LPD0d8fd260.calcification7  + (Individual coral growth records. Composites used in database instead (following approach of original publication))
  • Eur 018.MXD  + (Instrumental measurements from high- (low-
    Instrumental measurements from high- (low-) elevation grid boxes back to 1818 (1760) reveal strongest growth response to current-year June_September mean temperatures. The reconstruction correlates at 0.7 with high-elevation temperatures back to 1818 with a greater signal in the higher-frequency domain (r 0.8).
    al in the higher-frequency domain (r 0.8).)
  • NAm 3352.trsgi  + (Looks like post 1950s decorrelation, that or this is a snowpack sensitive Mountain Hemlock)
  • Arc 034.d18O  + (Low frequency)
  • Arc 033.d18O  + (Low frequency)
  • Arc 032.d18O  + (Low frequency)
  • Arc 026.d18O  + (Low frequency)
  • NAm 3772.MXD  + (Low-freq goes inverse of the observed temperature record after the 50s)
  • NAm 3436.MXD  + (Low-freq goes inverse of the observed temperature record after the 50s)
  • NAm 2560.trsgi  + (Low-freq goes inverse of the observed temperature record after the 50s)
  • NAm 172.trsgi  + (Low-freq goes inverse of the observed temperature record after the 50s)
  • NAm 1816.MXD  + (Low-freq goes inverse of the observed temperature record after the 50s. Elevation estimated from GoogleEarth; rounded to 100 m)
  • NAm 2164.trsgi  + (Low-frequency variability is inverse of the observed record. Passes the local correlation p-value screening though.)
  • NAm 1828.trsgi  + (Meets criteria but the record is a bit strange looking. Elevation estimated from GoogleEarth; rounded to 100 m)
  • LPD24dd89b2.composite  + (Metadata available at: http://data.aims.gov.au/metadataviewer/uuid/4f39c641-8450-4ea0-b2b6-4f3d582645f8)
  • LPD3100fe0a.composite  + (Metadata available at: http://data.aims.gov.au/metadataviewer/uuid/4f39c641-8450-4ea0-b2b6-4f3d582645f8)
  • LPD378db911.composite  + (Metadata available at: http://data.aims.gov.au/metadataviewer/uuid/4f39c641-8450-4ea0-b2b6-4f3d582645f8)
  • LPD8bd4e07e.composite  + (Metadata available at: http://data.aims.gov.au/metadataviewer/uuid/4f39c641-8450-4ea0-b2b6-4f3d582645f8)
  • LPDaa786707.composite  + (Metadata available at: http://data.aims.gov.au/metadataviewer/uuid/4f39c641-8450-4ea0-b2b6-4f3d582645f8)
  • LPDe1fb72db.composite  + (Metadata available at: http://data.aims.gov.au/metadataviewer/uuid/4f39c641-8450-4ea0-b2b6-4f3d582645f8)
  • Ant 031.d18O  + (MicS revised dating, NOAA National Climatic Data Center https://www.ncdc.noaa.gov/paleo/study/20246 (2016))
  • Ant 031dD.dD  + (MicS revised dating, NOAA National Climatic Data Center https://www.ncdc.noaa.gov/paleo/study/20246 (2016))
  • Arc 040.temperature  + (Mind dating uncertainty)
  • Arc 073.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 3748.MXD  + (No low-frequency signal. Elevation estimated from GoogleEarth; rounded to 100 m)
  • NAm 3760.MXD  + (No low-frequency signal. Elevation estimated from GoogleEarth; rounded to 100 m)
  • Asia 233.trsgi  + (Not a temperature proxy)
  • LPDa7a4074f.uncertainty temperature  + (Not a temperature proxy)
  • Ocean2kHR 007.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 139.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 052.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 664.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 880.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.)
  • Arc 096.d18O  + (Rejected - not 300 years long)
  • 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.)