Correlation with nearby Halley Station meteorological data 5thompson et al, 1994, fig 4)

Column 'IC95FI87-chron-NA1', with variable name 'yearEnsemble', was added to the dataset

year (LPD2e054fdc): interpretation3_scope: '' has been replaced by 'climate'
depth (LPDecd5ba45): interpretation3_scope: '' has been replaced by 'climate'

d18O (IC95FI8701A): paleoData_isPrimary: '' has been replaced by 'FALSE'
d18O (IC95FI8701A): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'
year (LPD2e054fdc): paleoData_isPrimary: '' has been replaced by 'TRUE'
year (LPD2e054fdc): paleoData_primaryAgeColumn: '' has been replaced by 'TRUE'
depth (LPDecd5ba45): paleoData_isPrimary: '' has been replaced by 'FALSE'
depth (LPDecd5ba45): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'

d18O (IC95FI8701A): interpretation1_seasonality: 'annual' has been replaced by 'Annual'
d18O (IC95FI8701A): interpretation1_variable: 'T' has been replaced by 'temperature'
d18O (IC95FI8701A): interpretation2_seasonality: 'annual' has been replaced by 'Annual'
d18O (IC95FI8701A): interpretation2_variable: 'P_isotope' has been replaced by 'precipitationIsotope'

d18O (IC95FI8701A): interpretation1_seasonality: 'annual' has been replaced by 'Annual'
d18O (IC95FI8701A): interpretation1_variable: 'T' has been replaced by 'temperature'
d18O (IC95FI8701A): interpretation2_seasonality: 'annual' has been replaced by 'Annual'
d18O (IC95FI8701A): interpretation2_variable: 'P_isotope' has been replaced by 'precipitationIsotope'

d18O (IC95FI8701A): paleoData_longName: '' has been replaced by 'AD'
year (LPD2e054fdc): paleoData_units: 'AD' has been replaced by 'yr AD'
year (LPD2e054fdc): paleoData_longName: '' has been replaced by 'AD'
depth (LPDecd5ba45): paleoData_longName: '' has been replaced by 'AD'

chronology based on annual layer counting, 36Cl reference horizon, and ice-flow modelling

TO: thermal year (Aug-Jul) annual values

Simple d18O-temperature relations used in polar regions (30), when applied to the d18O decrease of 8 per mil in LGS ice on Huascaran, suggest that air temperatures may have been lower by as much as 8A° to 12A°C at high elevation in the tropics.