Column 'addRtud8wAMzYsSUfkik', with variable name 'yearEnsemble', was added to the dataset

Bohleber, P., Wagenbach, D., Schoener, W. and Boehm, R.: To what extent do water isotope records from low accumulation Alpine ice cores reproduce instrumental temperature series?, Tellus B: Chemical and Physical Meteorology, 65(1), 20148, doi:10.3402/tellusb.v65i0.20148, 2013.

accumulation (annual thickness ice water equivalent)

volcanic horizons used to support the annual layer counting

d18O (IC13OPAN01A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (IC13OPAN01A): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addRpNVCYbpHy3Tjcrd9', with variable name 'yearEnsemble', was added to the dataset

Opel, T., Fritzsche, D. and Meyer, H.: Eurasian Arctic climate over the past millennium as recorded in the Akademii Nauk ice core (Severnaya Zemlya), Climate of the Past, 9(5), 2379–2389, doi:10.5194/cp-9-2379-2013, 2013.

AO :fixed primary reference and isotope interpretation

Van Ommen et al., 1997 : seasonal cycle calibration. This comparison yields an isotopea€temperature relation with a gradient (dI´/dT) of 0.44A±0.02a€°/A°C

d18O (IC13PALD01A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (IC13PALD01A): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addRmJG3S85SC2sRbJ2S', with variable name 'yearEnsemble', was added to the dataset

Morgan, V. I., Wookey, C. W., Li, J., van Ommen, T. D., Skinner, W. and Fitzpatrick,  Μ. F.: Site information and initial results from deep ice drilling on Law Dome, Antarctica, Journal of Glaciology, 43(143), 3–10, doi:10.3189/s0022143000002768, 1997.

Morgan, V. and van Ommen, T. D.: Seasonality in late-Holocene climate from ice-core records, The Holocene, 7(3), 351–354, doi:10.1177/095968369700700312, 1997.

Steig et al. 2013 suppl: Scaling between I´18O and temperature in West Antarctica can be estimated in a number of ways, all yielding similar results.  The local interannual scaling between WAIS Divide I´18O and Byrd temperature is 0.5a€°/A°C; the ratio of 50-year trends also yields 0.5a€°/A°C (1957-2006, Byrd temperature trend7 = 0.48A°C/decade; WAIS Divide I´18O trend = 0.24a€°/decade).  Regional interannual scaling between the composite I´18O series in Figure 1 and the West-Antarctic average temperature from Steig et al.4 is also 0.5a€°/A°C; the ratio of 50-year trends is 0.6a€°/A°C (1957-2006, West Antarctic temperature trend = 0.19A°C/decade4; composite I´18O trend = 0.12a€°/decade).  Comparison betweenI´18O and the borehole temperature reconstruction from WAIS Divide6 over the last 2000 years also results in similar scaling. See also Kuttel et al, 2012 for more interpretation