d2H (LS11KOMA01A): interpretation2_basis: 'Leaf wax dD reflects "...variations in the ?D of precipitation (?Dprecip) through time in many systems (Hou et al., 2008; Huang et al., 2004). Observational data and isotope-enabled climate models indicate that ?Dprecip reflects the integrated atmospheric history of a water parcel, including source region, transport history, and convective, evaporative, and distillation processes." / "The Lake Malawi ?Dwax likely reflects the ?D of precipitation and associated changes in precipitation and vapor transport, not bio- synthetic or temperature effects."' has been replaced by ''
d2H (LS11KOMA01A): interpretation2_direction: 'positive' has been replaced by ''
d2H (LS11KOMA01A): interpretation2_inferredMaterial: 'soil water' has been replaced by ''
d2H (LS11KOMA01A): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d2H (LS11KOMA01A): interpretation2_rank: '1' has been replaced by ''
d2H (LS11KOMA01A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d2H (LS11KOMA01A): interpretation2_seasonality: 'Annual' has been replaced by ''
d2H (LS11KOMA01A): interpretation2_seasonalityOriginal: 'Annual' has been replaced by ''
d2H (LS11KOMA01A): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d2H (LS11KOMA01A): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d2H (LS11KOMA01A): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d2H (LS11KOMA01A): interpretation3_basis: 'Relatively depleted dDwax values at Lake Malawi from ~3.1 ka to present likely reflect the modern hydrological controls on dDprecip, with source changes constituting a more limited role than the amount effect and overall intensity of the hydrological cycle.' has been replaced by ''
d2H (LS11KOMA01A): interpretation3_direction: 'negative' has been replaced by ''
d2H (LS11KOMA01A): interpretation3_inferredMaterial: 'soil water' has been replaced by ''
d2H (LS11KOMA01A): interpretation3_rank: '2' has been replaced by ''
d2H (LS11KOMA01A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d2H (LS11KOMA01A): interpretation3_seasonality: 'Annual' has been replaced by ''
d2H (LS11KOMA01A): interpretation3_seasonalityOriginal: 'Annual' has been replaced by ''
d2H (LS11KOMA01A): interpretation3_variable: 'precipitation' has been replaced by ''
d2H (LS11KOMA01A): interpretation3_variableGroup: 'EffectiveMoisture' has been replaced by ''
d2H (LS11KOMA01A): interpretation3_variableGroupDirection: 'negative' has been replaced by ''
d2H (LS11KOMA01A): interpretation3_variableGroupOriginal: 'P_amount' has been replaced by ''
d2H (LS11KOMA01A): interpretation4_basis: '' has been replaced by 'Leaf wax dD reflects "...variations in the ?D of precipitation (?Dprecip) through time in many systems (Hou et al., 2008; Huang et al., 2004). Observational data and isotope-enabled climate models indicate that ?Dprecip reflects the integrated atmospheric history of a water parcel, including source region, transport history, and convective, evaporative, and distillation processes." / "The Lake Malawi ?Dwax likely reflects the ?D of precipitation and associated changes in precipitation and vapor transport, not bio- synthetic or temperature effects."'
d2H (LS11KOMA01A): interpretation4_direction: '' has been replaced by 'positive'
d2H (LS11KOMA01A): interpretation4_inferredMaterial: '' has been replaced by 'soil water'
d2H (LS11KOMA01A): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d2H (LS11KOMA01A): interpretation4_rank: '' has been replaced by '1'
d2H (LS11KOMA01A): interpretation4_scope: '' has been replaced by 'isotope'
d2H (LS11KOMA01A): interpretation4_seasonality: '' has been replaced by 'Annual'
d2H (LS11KOMA01A): interpretation4_seasonalityOriginal: '' has been replaced by 'Annual'
d2H (LS11KOMA01A): interpretation4_variable: '' has been replaced by 'precipitationIsotope'
d2H (LS11KOMA01A): interpretation4_variableGroup: '' has been replaced by 'P_isotope'
d2H (LS11KOMA01A): interpretation4_variableGroupDirection: '' has been replaced by 'positive'
d2H (LS11KOMA01A): interpretation5_basis: '' has been replaced by 'Relatively depleted dDwax values at Lake Malawi from ~3.1 ka to present likely reflect the modern hydrological controls on dDprecip, with source changes constituting a more limited role than the amount effect and overall intensity of the hydrological cycle.'
d2H (LS11KOMA01A): interpretation5_direction: '' has been replaced by 'negative'
d2H (LS11KOMA01A): interpretation5_inferredMaterial: '' has been replaced by 'soil water'
d2H (LS11KOMA01A): interpretation5_rank: '' has been replaced by '2'
d2H (LS11KOMA01A): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS11KOMA01A): interpretation5_seasonality: '' has been replaced by 'Annual'
d2H (LS11KOMA01A): interpretation5_seasonalityOriginal: '' has been replaced by 'Annual'
d2H (LS11KOMA01A): interpretation5_variable: '' has been replaced by 'precipitation'
d2H (LS11KOMA01A): interpretation5_variableGroup: '' has been replaced by 'EffectiveMoisture'
d2H (LS11KOMA01A): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d2H (LS11KOMA01A): interpretation5_variableGroupOriginal: '' has been replaced by 'P_amount'
d2H (LS11KOMA01A): interpretation6_scope: '' has been replaced by 'isotope'
year (MAT15c72e1504): interpretation1_scope: '' has been replaced by 'climate'
year (MAT15c72e1504): interpretation2_scope: '' has been replaced by 'climate'
year (MAT15c72e1504): interpretation3_scope: '' has been replaced by 'climate'
depth (MAT3c131c959e): interpretation1_scope: '' has been replaced by 'climate'
depth (MAT3c131c959e): interpretation2_scope: '' has been replaced by 'climate'
depth (MAT3c131c959e): interpretation3_scope: '' has been replaced by 'climate'