d2H (IC13STSP01A): interpretation3_scope: '' has been replaced by 'isotope'
d2H (IC13STSP01A): interpretation4_scope: '' has been replaced by 'isotope'

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

d18O (IC13STWD01A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (IC13STWD01A): interpretation4_scope: '' has been replaced by 'isotope'
d18O (IC13STWD02A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (IC13STWD02A): interpretation4_scope: '' has been replaced by 'isotope'
d18O (IC13STWD02A2): interpretation3_scope: '' has been replaced by 'isotope'
d18O (IC13STWD02A2): interpretation4_scope: '' has been replaced by 'isotope'

AO: added isotope interpretation. Isotope interpretation is tied to atmospheric circulation, should we change the primary interpretation field?

The F10 record is significantly correlated (r = 0.44, P = 0.01) with ERA-Interim temperature (t850, 1979a€“2009), and we observe that the pattern of corre- lation with atmospheric pressure and sea surface tempera- tures (SSTs) is similar for both observational I´D and local temperature from reanalysis; however, we do not assume that I´D is a quantitative temperature proxy.

d2H (IC13THFE01A): interpretation3_scope: '' has been replaced by 'isotope'
d2H (IC13THFE01A): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addRXRmM6pZEqzRqObWK', with variable name 'yearEnsemble', was added to the dataset

Thomas, E. R., Bracegirdle, T. J., Turner, J. and Wolff, E. W.: A 308 year record of climate variability in West Antarctica, Geophysical Research Letters, 40(20), 5492–5496, doi:10.1002/2013gl057782, 2013.

; paleoData_variableName changed - was originally d18OiceSMOW; paleoData_units changed - was originally per mil SMOW; climateInterpretation_seasonality changed - was originally austral winter; archiveType changed - was originally ice core

Three-year running mean significantly correlated to SST Nino 4 region

There is no significant relationship between stable isotopes and precipitation (net accumulation) on the Quelccaya ice cap. In other words, the precipitation “amount effect” does not appear to govern the stable isotopic chemistry on this tropical glacier. Because 70 to 80% of the precipitation falling on Quelccaya arrives during the wet season, the δ18O history reflects primarily conditions during austral summer. Decadal averages of precipitation amount and δ18O are not strongly related