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Property:QCnotes

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Pages using the property "QCnotes"

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A
Asia 170.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 171.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 172.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 173.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 174.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 175.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 176.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 177.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 178.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 179.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 180.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 181.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 182.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 184.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 185.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 186.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 187.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 188.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 189.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 190.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 202.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 206.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 207.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 208.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 209.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 214.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 215.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 216.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 217.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 218.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 222.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 223.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 224.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 225.trsgi +Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 230.temperature +Half-centennial resolution. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 233.trsgi +Not a temperature proxy  +
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  +
Asia 236.d18O +Oxygen isotopes show positive correlation with NH temperature anomalies. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 237.dust +Hydro climate  +
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  +
Asia 317.temperature +Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 318.temperature +decadal resolution  +
Asia 319.temperature +Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 320.temperature +Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 321.temperature +decadal resolution  +
Asia 324.temperature +Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 325.temperature +Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 326.temperature +decadal resolution  +
Asia 327.temperature +Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 328.temperature +Decadal resolution. Elevation estimated from GoogleEarth; rounded to 100 m  +
Asia 329.temperature +decadal resolution  +
Asia 335.temperature +Species response to winter SST proved using redundancy analysis  +
Aus 010.trsgi +Warm season T signal. Elevation estimated from GoogleEarth; rounded to 100 m  +
Aus 015.trsgi +Composite series, spring T signal. Elevation estimated from GoogleEarth; rounded to 100 m  +
Aus 020.trsgi +Composite series, primarily winter T signal. Elevation estimated from GoogleEarth; rounded to 100 m  +
Aus 041.temperature +Calibrated temperature reconstruction from 2006 JQS paper. Elevation estimated from GoogleEarth; rounded to 100 m  +
Aus 057.temperature +Calibrated temperature reconstruction from 2006 JQS paper. Elevation estimated from GoogleEarth; rounded to 100 m  +
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  +
Aus 067.trsgi +composite series, warm season T signal, approximate average/centroid values entered in elevation, lat and lon fields for completeness  +
Aus 071.trsgi +warm season T signal  +
C
Can1101.trsgi +Data directly taken from 2013 NatGeo paper, already shifted by 1 year to match seasonality, RCS detrending  +
E
Eur 001.d18O +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.  +
Eur 002.temperature +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.  +
Eur 003.temperature +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.  +
Eur 005.temperature +Calibrating and verifying the MXD chronologies against the instrumental temperature data showed a promising opportunity to reconstruct warm-season (May through September) temperature variability  +
Eur 006.temperature +By refining dendroclimatological methods the time-series were composited to a mean series and calibrated (1756_1841; r2 = 66%) against Stockholm January_April temperatures.  +
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 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 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.  +
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)  +
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 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  +
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)  +
Eur 018.MXD +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).  +
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.  +
Eur 020.trsgi +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.  +
Eur 022.temperature +For overlapping period (1760-1854) the documentary data series correlate with instrumental temperatures most strongly in winter (86% explained variance in January) and least in autumn (56% in September). For annual average temperatures 81% of the variance is explained. Elevation estimated from GoogleEarth; rounded to 100 m  +
Eur 023.sampleID +Excluded related to sample information and error estimates  +
Eur 025.uncertainty temperature +Excluded related to sample information and error estimates  +
Eur 026.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.  +
Eur 027.JulianDay +The temperature reconstruction is preferred from this site  +
L
LPD016ef221.temperature +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Dataset contains NaN values and datapoints whose chronology is not QC'd  +
LPD027eca7f.Uk37 +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
LPD09e5a770.temperature +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Identical to LPDa03ec713  +
LPD0d8fd260.calcification7 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD0e0867fe.temperature +HVM, BM, 20/4/2016 Mediterranean1572bNieto-Moreno2012__TTR17-1_436B  +
LPD1079b4bb.calcification4 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD10e9f8f7.temperature +HVM, BM, 20/4/2016 Mediterranean1157abMoreno2012_MINMC-2_MINMC-1_alk(Muller) The higher-resolution alkenone record was selected. The authors also note that the G. bulloides Mg/Ca records spring upwelling SSTs whereas alkenones represent annual average SSTs. Alkenone data were measured in two cores (MINMC06-1 and MINMC06-2) from the same site. These two records were combined with the data sorted based on age.  +
LPD13a78f9b.temperature +HVM, BM, 20/4/2016 Atlantic0488Kuhnert2011__ GeoB9501-5_Mg/Ca(Anand) Combination of data from GeoB 9501–4 and GeoB 9501–5. Data combined based on age sort order.  +
LPD16c5b9d8.temperature +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.Dataset contains two records that have not been combined and whose chronology has not been QC'd  +
LPD17d4c9be.notes +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
LPD1a0245b7.temperature +HVM, BM, 20/4/2016 Pacific0185Stott2007_MD98-2181 WDC-paleoclimatology Data Contribution Series # 2007-092 Readme for Stott et al., (2007) notes calibration with Anand et al., (2003).  +
LPD1b77c35b.notes +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
LPD21b789e2.calcification1 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD24dd89b2.composite +Metadata available at: http://data.aims.gov.au/metadataviewer/uuid/4f39c641-8450-4ea0-b2b6-4f3d582645f8  +
LPD2757d69f.calcification4 +Individual coral growth records. Composites used in database instead (following approach of original publication)  +
LPD2a3997a7.temperature +HVM, BM, 20/4/2016 Southern0483aShevenell2011_ODP 1098B We used the publically archived data from PANGAEA, dated 2011.  +
LPD2d0bd641.Mg Ca +These are the original, not quality controlled data. O2kLR recommends only using the Quality controlled data.  +
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