depth (MAT3af707cf26): interpretation1_scope: '' has been replaced by 'climate'
depth (MAT3af707cf26): interpretation2_scope: '' has been replaced by 'climate'
depth (MAT3af707cf26): interpretation3_scope: '' has been replaced by 'climate'
year (MAT96e244a128): interpretation1_scope: '' has been replaced by 'climate'
year (MAT96e244a128): interpretation2_scope: '' has been replaced by 'climate'
year (MAT96e244a128): interpretation3_scope: '' has been replaced by 'climate'
d18O (SP08ZHCN01A): interpretation2_basis: 'Summer AM precipitation is driven by the thermal contrast between Asia and the tropical Indo-Pacific and therefore should be linked to regional temperature change (16). Based on an ECHO-G climate model simulation (SOM), we modeled Chinese air temperature for the past millennium, with results that were broadly con- sistent with our record (r = ?0.46 and n = 345 data points), particularly with regard to centen- nial and multicentennial time scales and with regard to the distinct double peak in both model output and record during the MWP (Fig. 3A).' has been replaced by ''
d18O (SP08ZHCN01A): interpretation2_direction: 'positive' has been replaced by ''
d18O (SP08ZHCN01A): interpretation2_equilibriumEvidence: 'A Hendy Test (S3) shows no substantial isotopic fractionation along the same growth layer and correlations between ?18O and ?13C are statistically insignificant, suggesting that the stalagmite calcite was deposited in isotopic equilibrium (Fig. S3). This agrees with observations from modern carbonate?water stable isotope systematics (S4) from the same cave.' has been replaced by ''
d18O (SP08ZHCN01A): interpretation2_inferredMaterial: 'groundwater d18O' has been replaced by ''
d18O (SP08ZHCN01A): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (SP08ZHCN01A): interpretation2_rank: '1' has been replaced by ''
d18O (SP08ZHCN01A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (SP08ZHCN01A): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d18O (SP08ZHCN01A): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d18O (SP08ZHCN01A): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d18O (SP08ZHCN01A): interpretation3_rank: '2' has been replaced by ''
d18O (SP08ZHCN01A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (SP08ZHCN01A): interpretation4_rank: '' has been replaced by '1'
d18O (SP08ZHCN01A): interpretation4_basis: '' has been replaced by 'Summer AM precipitation is driven by the thermal contrast between Asia and the tropical Indo-Pacific and therefore should be linked to regional temperature change (16). Based on an ECHO-G climate model simulation (SOM), we modeled Chinese air temperature for the past millennium, with results that were broadly con- sistent with our record (r = ?0.46 and n = 345 data points), particularly with regard to centen- nial and multicentennial time scales and with regard to the distinct double peak in both model output and record during the MWP (Fig. 3A).'
d18O (SP08ZHCN01A): interpretation4_direction: '' has been replaced by 'positive'
d18O (SP08ZHCN01A): interpretation4_equilibriumEvidence: '' has been replaced by 'A Hendy Test (S3) shows no substantial isotopic fractionation along the same growth layer and correlations between ?18O and ?13C are statistically insignificant, suggesting that the stalagmite calcite was deposited in isotopic equilibrium (Fig. S3). This agrees with observations from modern carbonate?water stable isotope systematics (S4) from the same cave.'
d18O (SP08ZHCN01A): interpretation4_inferredMaterial: '' has been replaced by 'groundwater d18O'
d18O (SP08ZHCN01A): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (SP08ZHCN01A): interpretation4_variable: '' has been replaced by 'precipitationIsotope'
d18O (SP08ZHCN01A): interpretation4_variableGroup: '' has been replaced by 'P_isotope'
d18O (SP08ZHCN01A): interpretation4_variableGroupDirection: '' has been replaced by 'positive'
d18O (SP08ZHCN01A): interpretation5_rank: '' has been replaced by '2'
d18O (SP08ZHCN01A): interpretation5_scope: '' has been replaced by 'isotope'
d18O (SP08ZHCN01A): interpretation6_scope: '' has been replaced by 'isotope'