depth (LPD1fa4d0be): interpretation1_scope: '' has been replaced by 'climate'
depth (LPD1fa4d0be): interpretation2_scope: '' has been replaced by 'climate'
depth (LPD1fa4d0bf): interpretation1_scope: '' has been replaced by 'climate'
depth (LPD1fa4d0bf): interpretation2_scope: '' has been replaced by 'climate'
depth (LPD1fa4d0bg): interpretation1_scope: '' has been replaced by 'climate'
depth (LPD1fa4d0bg): interpretation2_scope: '' has been replaced by 'climate'
year (LPDf4934b2d): interpretation1_scope: '' has been replaced by 'climate'
year (LPDf4934b2d): interpretation2_scope: '' has been replaced by 'climate'
year (LPDf4934b2e): interpretation1_scope: '' has been replaced by 'climate'
year (LPDf4934b2e): interpretation2_scope: '' has been replaced by 'climate'
year (MATb21d5e7032): interpretation1_scope: '' has been replaced by 'climate'
year (MATb21d5e7032): interpretation2_scope: '' has been replaced by 'climate'
d18O (SP04YUCN01A): interpretation2_basis: 'To estimate absolute amounts of rainfall integrated from sources to southeast China, we must make assumptions about absolute humidity in tropical source regions. Even assuming a glacial relative humidity as high as today?s and only a modest tropical temper- ature depression (2.5i¿½C), we calculate an ab- solute tropical glacial vapor pressure that is 85% of today?s and 79% of mid-Holocene/ Last Interglacial values (at a mid-Holocene temperature 1i¿½C greater than today and con- stant relative humidity). Coupled with the Rayleigh calculations, the amount of precip- itation integrated between tropical sources and southeast China is today  87% of mid- Holocene/Last Interglacial values and was  65% of mid-Holocene/Last Interglacial val- ues at glacial times corresponding to the heaviest Hulu/Dongge calcite  18O values, indicating that this region was significantly drier during glacial times.' has been replaced by ''
d18O (SP04YUCN01A): interpretation2_direction: 'positive' has been replaced by ''
d18O (SP04YUCN01A): interpretation2_equilibriumEvidence: 'There is little evidence for kinetic fractionation on the basis of C and O isotope correlations. C and O isotope ratios do not correlate strongly for any of the three stalag- mites in this study or even for portions of these stalagmites. The highest R2 value for any of the three stalagmites is 0.27 (table S6). Because the top of D4 was deposited in isotopic equilibrium and because a portion of D4 replicates the Hulu record, D4 is less likely to have been affected by kinetic effects or water/rock interactions than D3.' has been replaced by ''
d18O (SP04YUCN01A): interpretation2_inferredMaterial: 'groundwater d18O' has been replaced by ''
d18O (SP04YUCN01A): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (SP04YUCN01A): interpretation2_rank: '2' has been replaced by ''
d18O (SP04YUCN01A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (SP04YUCN01A): interpretation2_seasonality: 'Wet Season' has been replaced by ''
d18O (SP04YUCN01A): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d18O (SP04YUCN01A): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d18O (SP04YUCN01A): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d18O (SP04YUCN01A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (SP04YUCN01A): interpretation4_rank: '' has been replaced by '2'
d18O (SP04YUCN01A): interpretation4_basis: '' has been replaced by 'To estimate absolute amounts of rainfall integrated from sources to southeast China, we must make assumptions about absolute humidity in tropical source regions. Even assuming a glacial relative humidity as high as today?s and only a modest tropical temper- ature depression (2.5i¿½C), we calculate an ab- solute tropical glacial vapor pressure that is 85% of today?s and 79% of mid-Holocene/ Last Interglacial values (at a mid-Holocene temperature 1i¿½C greater than today and con- stant relative humidity). Coupled with the Rayleigh calculations, the amount of precip- itation integrated between tropical sources and southeast China is today  87% of mid- Holocene/Last Interglacial values and was  65% of mid-Holocene/Last Interglacial val- ues at glacial times corresponding to the heaviest Hulu/Dongge calcite  18O values, indicating that this region was significantly drier during glacial times.'
d18O (SP04YUCN01A): interpretation4_direction: '' has been replaced by 'positive'
d18O (SP04YUCN01A): interpretation4_equilibriumEvidence: '' has been replaced by 'There is little evidence for kinetic fractionation on the basis of C and O isotope correlations. C and O isotope ratios do not correlate strongly for any of the three stalag- mites in this study or even for portions of these stalagmites. The highest R2 value for any of the three stalagmites is 0.27 (table S6). Because the top of D4 was deposited in isotopic equilibrium and because a portion of D4 replicates the Hulu record, D4 is less likely to have been affected by kinetic effects or water/rock interactions than D3.'
d18O (SP04YUCN01A): interpretation4_inferredMaterial: '' has been replaced by 'groundwater d18O'
d18O (SP04YUCN01A): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (SP04YUCN01A): interpretation4_seasonality: '' has been replaced by 'Wet Season'
d18O (SP04YUCN01A): interpretation4_variable: '' has been replaced by 'precipitationIsotope'
d18O (SP04YUCN01A): interpretation4_variableGroup: '' has been replaced by 'P_isotope'
d18O (SP04YUCN01A): interpretation4_variableGroupDirection: '' has been replaced by 'positive'
d18O (SP04YUCN01A): interpretation5_scope: '' has been replaced by 'isotope'
d18O (SP04YUCN01A): interpretation6_scope: '' has been replaced by 'isotope'
d18O (SP04YUCN02A): interpretation2_basis: 'To estimate absolute amounts of rainfall integrated from sources to southeast China, we must make assumptions about absolute humidity in tropical source regions. Even assuming a glacial relative humidity as high as today?s and only a modest tropical temper- ature depression (2.5i¿½C), we calculate an ab- solute tropical glacial vapor pressure that is 85% of today?s and 79% of mid-Holocene/ Last Interglacial values (at a mid-Holocene temperature 1i¿½C greater than today and con- stant relative humidity). Coupled with the Rayleigh calculations, the amount of precip- itation integrated between tropical sources and southeast China is today  87% of mid- Holocene/Last Interglacial values and was  65% of mid-Holocene/Last Interglacial val- ues at glacial times corresponding to the heaviest Hulu/Dongge calcite  18O values, indicating that this region was significantly drier during glacial times.' has been replaced by ''
d18O (SP04YUCN02A): interpretation2_direction: 'positive' has been replaced by ''
d18O (SP04YUCN02A): interpretation2_equilibriumEvidence: 'There is little evidence for kinetic fractionation on the basis of C and O isotope correlations. C and O isotope ratios do not correlate strongly for any of the three stalag- mites in this study or even for portions of these stalagmites. The highest R2 value for any of the three stalagmites is 0.27 (table S6). Because the top of D4 was deposited in isotopic equilibrium and because a portion of D4 replicates the Hulu record, D4 is less likely to have been affected by kinetic effects or water/rock interactions than D3.' has been replaced by ''
d18O (SP04YUCN02A): interpretation2_inferredMaterial: 'groundwater d18O' has been replaced by ''
d18O (SP04YUCN02A): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (SP04YUCN02A): interpretation2_rank: '1' has been replaced by ''
d18O (SP04YUCN02A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (SP04YUCN02A): interpretation2_seasonality: 'Annual' has been replaced by ''
d18O (SP04YUCN02A): interpretation2_seasonalityOriginal: 'Annual' has been replaced by ''
d18O (SP04YUCN02A): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d18O (SP04YUCN02A): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d18O (SP04YUCN02A): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d18O (SP04YUCN02A): interpretation3_rank: '2' has been replaced by ''
d18O (SP04YUCN02A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (SP04YUCN02A): interpretation4_rank: '' has been replaced by '1'
d18O (SP04YUCN02A): interpretation4_basis: '' has been replaced by 'To estimate absolute amounts of rainfall integrated from sources to southeast China, we must make assumptions about absolute humidity in tropical source regions. Even assuming a glacial relative humidity as high as today?s and only a modest tropical temper- ature depression (2.5i¿½C), we calculate an ab- solute tropical glacial vapor pressure that is 85% of today?s and 79% of mid-Holocene/ Last Interglacial values (at a mid-Holocene temperature 1i¿½C greater than today and con- stant relative humidity). Coupled with the Rayleigh calculations, the amount of precip- itation integrated between tropical sources and southeast China is today  87% of mid- Holocene/Last Interglacial values and was  65% of mid-Holocene/Last Interglacial val- ues at glacial times corresponding to the heaviest Hulu/Dongge calcite  18O values, indicating that this region was significantly drier during glacial times.'
d18O (SP04YUCN02A): interpretation4_direction: '' has been replaced by 'positive'
d18O (SP04YUCN02A): interpretation4_equilibriumEvidence: '' has been replaced by 'There is little evidence for kinetic fractionation on the basis of C and O isotope correlations. C and O isotope ratios do not correlate strongly for any of the three stalag- mites in this study or even for portions of these stalagmites. The highest R2 value for any of the three stalagmites is 0.27 (table S6). Because the top of D4 was deposited in isotopic equilibrium and because a portion of D4 replicates the Hulu record, D4 is less likely to have been affected by kinetic effects or water/rock interactions than D3.'
d18O (SP04YUCN02A): interpretation4_inferredMaterial: '' has been replaced by 'groundwater d18O'
d18O (SP04YUCN02A): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (SP04YUCN02A): interpretation4_seasonality: '' has been replaced by 'Annual'
d18O (SP04YUCN02A): interpretation4_seasonalityOriginal: '' has been replaced by 'Annual'
d18O (SP04YUCN02A): interpretation4_variable: '' has been replaced by 'precipitationIsotope'
d18O (SP04YUCN02A): interpretation4_variableGroup: '' has been replaced by 'P_isotope'
d18O (SP04YUCN02A): interpretation4_variableGroupDirection: '' has been replaced by 'positive'
d18O (SP04YUCN02A): interpretation5_rank: '' has been replaced by '2'
d18O (SP04YUCN02A): interpretation5_scope: '' has been replaced by 'isotope'
d18O (SP04YUCN02A): interpretation6_scope: '' has been replaced by 'isotope'
d18O (SP04YUCN03A): interpretation2_basis: 'To estimate absolute amounts of rainfall integrated from sources to southeast China, we must make assumptions about absolute humidity in tropical source regions. Even assuming a glacial relative humidity as high as today?s and only a modest tropical temper- ature depression (2.5i¿½C), we calculate an ab- solute tropical glacial vapor pressure that is 85% of today?s and 79% of mid-Holocene/ Last Interglacial values (at a mid-Holocene temperature 1i¿½C greater than today and con- stant relative humidity). Coupled with the Rayleigh calculations, the amount of precip- itation integrated between tropical sources and southeast China is today  87% of mid- Holocene/Last Interglacial values and was  65% of mid-Holocene/Last Interglacial val- ues at glacial times corresponding to the heaviest Hulu/Dongge calcite  18O values, indicating that this region was significantly drier during glacial times.' has been replaced by ''
d18O (SP04YUCN03A): interpretation2_direction: 'positive' has been replaced by ''
d18O (SP04YUCN03A): interpretation2_equilibriumEvidence: 'There is little evidence for kinetic fractionation on the basis of C and O isotope correlations. C and O isotope ratios do not correlate strongly for any of the three stalag- mites in this study or even for portions of these stalagmites. The highest R2 value for any of the three stalagmites is 0.27 (table S6). Because the top of D4 was deposited in isotopic equilibrium and because a portion of D4 replicates the Hulu record, D4 is less likely to have been affected by kinetic effects or water/rock interactions than D3.' has been replaced by ''
d18O (SP04YUCN03A): interpretation2_inferredMaterial: 'groundwater d18O' has been replaced by ''
d18O (SP04YUCN03A): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (SP04YUCN03A): interpretation2_rank: '2' has been replaced by ''
d18O (SP04YUCN03A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (SP04YUCN03A): interpretation2_seasonality: 'Wet Season' has been replaced by ''
d18O (SP04YUCN03A): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d18O (SP04YUCN03A): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d18O (SP04YUCN03A): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d18O (SP04YUCN03A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (SP04YUCN03A): interpretation4_rank: '' has been replaced by '2'
d18O (SP04YUCN03A): interpretation4_basis: '' has been replaced by 'To estimate absolute amounts of rainfall integrated from sources to southeast China, we must make assumptions about absolute humidity in tropical source regions. Even assuming a glacial relative humidity as high as today?s and only a modest tropical temper- ature depression (2.5i¿½C), we calculate an ab- solute tropical glacial vapor pressure that is 85% of today?s and 79% of mid-Holocene/ Last Interglacial values (at a mid-Holocene temperature 1i¿½C greater than today and con- stant relative humidity). Coupled with the Rayleigh calculations, the amount of precip- itation integrated between tropical sources and southeast China is today  87% of mid- Holocene/Last Interglacial values and was  65% of mid-Holocene/Last Interglacial val- ues at glacial times corresponding to the heaviest Hulu/Dongge calcite  18O values, indicating that this region was significantly drier during glacial times.'
d18O (SP04YUCN03A): interpretation4_direction: '' has been replaced by 'positive'
d18O (SP04YUCN03A): interpretation4_equilibriumEvidence: '' has been replaced by 'There is little evidence for kinetic fractionation on the basis of C and O isotope correlations. C and O isotope ratios do not correlate strongly for any of the three stalag- mites in this study or even for portions of these stalagmites. The highest R2 value for any of the three stalagmites is 0.27 (table S6). Because the top of D4 was deposited in isotopic equilibrium and because a portion of D4 replicates the Hulu record, D4 is less likely to have been affected by kinetic effects or water/rock interactions than D3.'
d18O (SP04YUCN03A): interpretation4_inferredMaterial: '' has been replaced by 'groundwater d18O'
d18O (SP04YUCN03A): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (SP04YUCN03A): interpretation4_seasonality: '' has been replaced by 'Wet Season'
d18O (SP04YUCN03A): interpretation4_variable: '' has been replaced by 'precipitationIsotope'
d18O (SP04YUCN03A): interpretation4_variableGroup: '' has been replaced by 'P_isotope'
d18O (SP04YUCN03A): interpretation4_variableGroupDirection: '' has been replaced by 'positive'
d18O (SP04YUCN03A): interpretation5_scope: '' has been replaced by 'isotope'
d18O (SP04YUCN03A): interpretation6_scope: '' has been replaced by 'isotope'