year (MAT1f7cb77c97): interpretation1_scope: '' has been replaced by 'climate'
year (MAT1f7cb77c97): interpretation2_scope: '' has been replaced by 'climate'
year (MAT1f7cb77c97): interpretation3_scope: '' has been replaced by 'climate'
d18O (TR12SAMU00): interpretation2_basis: 'As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched d18O in tree rings?..moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor...Although the mechanisms underlying variations in tree ring d18O can generally be attributed to d18O of source water and evaporative enrichment of leaf water d18O, in pluvial monsoon regions these effects seem to be well represented by the PDSI,' has been replaced by ''
d18O (TR12SAMU00): interpretation2_direction: 'negative' has been replaced by ''
d18O (TR12SAMU00): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (TR12SAMU00): interpretation2_rank: '1' has been replaced by ''
d18O (TR12SAMU00): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (TR12SAMU00): interpretation2_seasonality: 'May-Oct' has been replaced by ''
d18O (TR12SAMU00): interpretation2_variable: 'effectivePrecipitation' has been replaced by ''
d18O (TR12SAMU00): interpretation2_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (TR12SAMU00): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (TR12SAMU00): interpretation2_variableGroupOriginal: 'P_E' has been replaced by ''
d18O (TR12SAMU00): interpretation3_scope: '' has been replaced by 'climate'
d18O (TR12SAMU00): interpretation4_direction: '' has been replaced by 'negative'
d18O (TR12SAMU00): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (TR12SAMU00): interpretation4_rank: '' has been replaced by '1'
d18O (TR12SAMU00): interpretation4_scope: '' has been replaced by 'isotope'
d18O (TR12SAMU00): interpretation4_seasonality: '' has been replaced by 'May-Oct'
d18O (TR12SAMU00): interpretation4_variable: '' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU00): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (TR12SAMU00): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (TR12SAMU00): interpretation4_variableGroupOriginal: '' has been replaced by 'P_E'
d18O (TR12SAMU00): interpretation4_basis: '' has been replaced by 'As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched d18O in tree rings?..moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor...Although the mechanisms underlying variations in tree ring d18O can generally be attributed to d18O of source water and evaporative enrichment of leaf water d18O, in pluvial monsoon regions these effects seem to be well represented by the PDSI,'
d18O (TR12SAMU00): interpretation5_scope: '' has been replaced by 'isotope'
d18O (TR12SAMU00): interpretation6_scope: '' has been replaced by 'isotope'
d18O (TR12SAMU01): interpretation2_basis: 'As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.' has been replaced by ''
d18O (TR12SAMU01): interpretation2_direction: 'negative' has been replaced by ''
d18O (TR12SAMU01): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (TR12SAMU01): interpretation2_rank: '1' has been replaced by ''
d18O (TR12SAMU01): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (TR12SAMU01): interpretation2_seasonality: 'May-Oct' has been replaced by ''
d18O (TR12SAMU01): interpretation2_seasonalityOriginal: 'May-October' has been replaced by ''
d18O (TR12SAMU01): interpretation2_variable: 'effectivePrecipitation' has been replaced by ''
d18O (TR12SAMU01): interpretation2_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (TR12SAMU01): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (TR12SAMU01): interpretation2_variableGroupOriginal: 'P_E' has been replaced by ''
d18O (TR12SAMU01): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (TR12SAMU01): interpretation3_seasonalityOriginal: 'May-October' has been replaced by ''
d18O (TR12SAMU01): interpretation3_variableOriginal: 'Precipitation_amount' has been replaced by ''
d18O (TR12SAMU01): interpretation4_direction: '' has been replaced by 'negative'
d18O (TR12SAMU01): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (TR12SAMU01): interpretation4_rank: '' has been replaced by '1'
d18O (TR12SAMU01): interpretation4_seasonality: '' has been replaced by 'May-Oct'
d18O (TR12SAMU01): interpretation4_variable: '' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU01): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (TR12SAMU01): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (TR12SAMU01): interpretation4_variableGroupOriginal: '' has been replaced by 'P_E'
d18O (TR12SAMU01): interpretation4_basis: '' has been replaced by 'As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.'
d18O (TR12SAMU01): interpretation5_scope: '' has been replaced by 'isotope'
d18O (TR12SAMU01): interpretation5_seasonalityOriginal: '' has been replaced by 'May-October'
d18O (TR12SAMU01): interpretation5_variableOriginal: '' has been replaced by 'Precipitation_amount'
d18O (TR12SAMU01): interpretation6_scope: '' has been replaced by 'isotope'
d18O (TR12SAMU01): interpretation6_seasonalityOriginal: '' has been replaced by 'May-October'
d18O (TR12SAMU02): interpretation2_basis: 'As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.' has been replaced by ''
d18O (TR12SAMU02): interpretation2_direction: 'negative' has been replaced by ''
d18O (TR12SAMU02): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (TR12SAMU02): interpretation2_rank: '1' has been replaced by ''
d18O (TR12SAMU02): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (TR12SAMU02): interpretation2_seasonality: 'May-Oct' has been replaced by ''
d18O (TR12SAMU02): interpretation2_seasonalityOriginal: 'May-October' has been replaced by ''
d18O (TR12SAMU02): interpretation2_variable: 'effectivePrecipitation' has been replaced by ''
d18O (TR12SAMU02): interpretation2_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (TR12SAMU02): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (TR12SAMU02): interpretation2_variableGroupOriginal: 'P_E' has been replaced by ''
d18O (TR12SAMU02): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (TR12SAMU02): interpretation3_seasonalityOriginal: 'May-October' has been replaced by ''
d18O (TR12SAMU02): interpretation3_variableOriginal: 'Precipitation_amount' has been replaced by ''
d18O (TR12SAMU02): interpretation4_direction: '' has been replaced by 'negative'
d18O (TR12SAMU02): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (TR12SAMU02): interpretation4_rank: '' has been replaced by '1'
d18O (TR12SAMU02): interpretation4_seasonality: '' has been replaced by 'May-Oct'
d18O (TR12SAMU02): interpretation4_variable: '' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU02): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (TR12SAMU02): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (TR12SAMU02): interpretation4_variableGroupOriginal: '' has been replaced by 'P_E'
d18O (TR12SAMU02): interpretation4_basis: '' has been replaced by 'As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.'
d18O (TR12SAMU02): interpretation5_scope: '' has been replaced by 'isotope'
d18O (TR12SAMU02): interpretation5_seasonalityOriginal: '' has been replaced by 'May-October'
d18O (TR12SAMU02): interpretation5_variableOriginal: '' has been replaced by 'Precipitation_amount'
d18O (TR12SAMU02): interpretation6_scope: '' has been replaced by 'isotope'
d18O (TR12SAMU02): interpretation6_seasonalityOriginal: '' has been replaced by 'May-October'
d18O (TR12SAMU03): interpretation2_basis: 'As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.' has been replaced by ''
d18O (TR12SAMU03): interpretation2_direction: 'negative' has been replaced by ''
d18O (TR12SAMU03): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (TR12SAMU03): interpretation2_rank: '1' has been replaced by ''
d18O (TR12SAMU03): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (TR12SAMU03): interpretation2_seasonality: 'May-Oct' has been replaced by ''
d18O (TR12SAMU03): interpretation2_seasonalityOriginal: 'May-October' has been replaced by ''
d18O (TR12SAMU03): interpretation2_variable: 'effectivePrecipitation' has been replaced by ''
d18O (TR12SAMU03): interpretation2_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (TR12SAMU03): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (TR12SAMU03): interpretation2_variableGroupOriginal: 'P_E' has been replaced by ''
d18O (TR12SAMU03): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (TR12SAMU03): interpretation3_seasonalityOriginal: 'May-October' has been replaced by ''
d18O (TR12SAMU03): interpretation3_variableOriginal: 'Precipitation_amount' has been replaced by ''
d18O (TR12SAMU03): interpretation4_direction: '' has been replaced by 'negative'
d18O (TR12SAMU03): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (TR12SAMU03): interpretation4_rank: '' has been replaced by '1'
d18O (TR12SAMU03): interpretation4_seasonality: '' has been replaced by 'May-Oct'
d18O (TR12SAMU03): interpretation4_variable: '' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU03): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (TR12SAMU03): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (TR12SAMU03): interpretation4_variableGroupOriginal: '' has been replaced by 'P_E'
d18O (TR12SAMU03): interpretation4_basis: '' has been replaced by 'As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.'
d18O (TR12SAMU03): interpretation5_scope: '' has been replaced by 'isotope'
d18O (TR12SAMU03): interpretation5_seasonalityOriginal: '' has been replaced by 'May-October'
d18O (TR12SAMU03): interpretation5_variableOriginal: '' has been replaced by 'Precipitation_amount'
d18O (TR12SAMU03): interpretation6_scope: '' has been replaced by 'isotope'
d18O (TR12SAMU03): interpretation6_seasonalityOriginal: '' has been replaced by 'May-October'
d18O (TR12SAMU04): interpretation2_basis: 'As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.' has been replaced by ''
d18O (TR12SAMU04): interpretation2_direction: 'negative' has been replaced by ''
d18O (TR12SAMU04): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (TR12SAMU04): interpretation2_rank: '1' has been replaced by ''
d18O (TR12SAMU04): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (TR12SAMU04): interpretation2_seasonality: 'May-Oct' has been replaced by ''
d18O (TR12SAMU04): interpretation2_seasonalityOriginal: 'May-October' has been replaced by ''
d18O (TR12SAMU04): interpretation2_variable: 'effectivePrecipitation' has been replaced by ''
d18O (TR12SAMU04): interpretation2_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (TR12SAMU04): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (TR12SAMU04): interpretation2_variableGroupOriginal: 'P_E' has been replaced by ''
d18O (TR12SAMU04): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (TR12SAMU04): interpretation3_seasonalityOriginal: 'May-October' has been replaced by ''
d18O (TR12SAMU04): interpretation3_variableOriginal: 'Precipitation_amount' has been replaced by ''
d18O (TR12SAMU04): interpretation4_direction: '' has been replaced by 'negative'
d18O (TR12SAMU04): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (TR12SAMU04): interpretation4_rank: '' has been replaced by '1'
d18O (TR12SAMU04): interpretation4_seasonality: '' has been replaced by 'May-Oct'
d18O (TR12SAMU04): interpretation4_variable: '' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU04): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (TR12SAMU04): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (TR12SAMU04): interpretation4_variableGroupOriginal: '' has been replaced by 'P_E'
d18O (TR12SAMU04): interpretation4_basis: '' has been replaced by 'As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.'
d18O (TR12SAMU04): interpretation5_scope: '' has been replaced by 'isotope'
d18O (TR12SAMU04): interpretation5_seasonalityOriginal: '' has been replaced by 'May-October'
d18O (TR12SAMU04): interpretation5_variableOriginal: '' has been replaced by 'Precipitation_amount'
d18O (TR12SAMU04): interpretation6_scope: '' has been replaced by 'isotope'
d18O (TR12SAMU04): interpretation6_seasonalityOriginal: '' has been replaced by 'May-October'
d18O (TR12SAMU05): interpretation2_basis: 'As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.' has been replaced by ''
d18O (TR12SAMU05): interpretation2_direction: 'negative' has been replaced by ''
d18O (TR12SAMU05): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (TR12SAMU05): interpretation2_rank: '1' has been replaced by ''
d18O (TR12SAMU05): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (TR12SAMU05): interpretation2_seasonality: 'May-Oct' has been replaced by ''
d18O (TR12SAMU05): interpretation2_seasonalityOriginal: 'May-October' has been replaced by ''
d18O (TR12SAMU05): interpretation2_variable: 'effectivePrecipitation' has been replaced by ''
d18O (TR12SAMU05): interpretation2_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (TR12SAMU05): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (TR12SAMU05): interpretation2_variableGroupOriginal: 'P_E' has been replaced by ''
d18O (TR12SAMU05): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (TR12SAMU05): interpretation3_seasonalityOriginal: 'May-October' has been replaced by ''
d18O (TR12SAMU05): interpretation3_variableOriginal: 'Precipitation_amount' has been replaced by ''
d18O (TR12SAMU05): interpretation4_direction: '' has been replaced by 'negative'
d18O (TR12SAMU05): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (TR12SAMU05): interpretation4_rank: '' has been replaced by '1'
d18O (TR12SAMU05): interpretation4_seasonality: '' has been replaced by 'May-Oct'
d18O (TR12SAMU05): interpretation4_variable: '' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU05): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (TR12SAMU05): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (TR12SAMU05): interpretation4_variableGroupOriginal: '' has been replaced by 'P_E'
d18O (TR12SAMU05): interpretation4_basis: '' has been replaced by 'As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.'
d18O (TR12SAMU05): interpretation5_scope: '' has been replaced by 'isotope'
d18O (TR12SAMU05): interpretation5_seasonalityOriginal: '' has been replaced by 'May-October'
d18O (TR12SAMU05): interpretation5_variableOriginal: '' has been replaced by 'Precipitation_amount'
d18O (TR12SAMU05): interpretation6_scope: '' has been replaced by 'isotope'
d18O (TR12SAMU05): interpretation6_seasonalityOriginal: '' has been replaced by 'May-October'
d18O (TR12SAMU06): interpretation2_basis: 'As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.' has been replaced by ''
d18O (TR12SAMU06): interpretation2_direction: 'negative' has been replaced by ''
d18O (TR12SAMU06): interpretation2_inferredMaterial: 'soil water' has been replaced by ''
d18O (TR12SAMU06): interpretation2_integrationTime: '1' has been replaced by ''
d18O (TR12SAMU06): interpretation2_integrationTimeUnits: 'years' has been replaced by ''
d18O (TR12SAMU06): interpretation2_mathematicalRelation: 'Linear' has been replaced by ''
d18O (TR12SAMU06): interpretation2_rank: '1' has been replaced by ''
d18O (TR12SAMU06): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (TR12SAMU06): interpretation2_seasonality: 'May-Oct' has been replaced by ''
d18O (TR12SAMU06): interpretation2_seasonalityOriginal: 'May-October' has been replaced by ''
d18O (TR12SAMU06): interpretation2_variable: 'effectivePrecipitation' has been replaced by ''
d18O (TR12SAMU06): interpretation2_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (TR12SAMU06): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (TR12SAMU06): interpretation2_variableGroupOriginal: 'P_E' has been replaced by ''
d18O (TR12SAMU06): interpretation3_basis: 'calibration with instrumental record' has been replaced by ''
d18O (TR12SAMU06): interpretation3_direction: 'negative' has been replaced by ''
d18O (TR12SAMU06): interpretation3_mathematicalRelation: 'linear' has been replaced by ''
d18O (TR12SAMU06): interpretation3_rank: '2' has been replaced by ''
d18O (TR12SAMU06): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (TR12SAMU06): interpretation3_seasonality: 'May-Oct' has been replaced by ''
d18O (TR12SAMU06): interpretation3_seasonalityOriginal: 'May-October' has been replaced by ''
d18O (TR12SAMU06): interpretation3_variable: 'precipitation' has been replaced by ''
d18O (TR12SAMU06): interpretation3_variableGroup: 'P' has been replaced by ''
d18O (TR12SAMU06): interpretation3_variableOriginal: 'Precipitation_amount' has been replaced by ''
d18O (TR12SAMU06): interpretation4_direction: 'positive' has been replaced by 'negative'
d18O (TR12SAMU06): interpretation4_mathematicalRelation: 'linear' has been replaced by 'Linear'
d18O (TR12SAMU06): interpretation4_rank: '3' has been replaced by '1'
d18O (TR12SAMU06): interpretation4_variable: 'temperature' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU06): interpretation4_variableGroup: 'Temperature' has been replaced by 'EffectiveMoisture'
d18O (TR12SAMU06): interpretation4_variableGroupOriginal: 'T_air' has been replaced by 'P_E'
d18O (TR12SAMU06): interpretation4_basis: '' has been replaced by 'As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.'
d18O (TR12SAMU06): interpretation4_inferredMaterial: '' has been replaced by 'soil water'
d18O (TR12SAMU06): interpretation4_integrationTime: '' has been replaced by '1'
d18O (TR12SAMU06): interpretation4_integrationTimeUnits: '' has been replaced by 'years'
d18O (TR12SAMU06): interpretation5_basis: '' has been replaced by 'calibration with instrumental record'
d18O (TR12SAMU06): interpretation5_direction: '' has been replaced by 'negative'
d18O (TR12SAMU06): interpretation5_mathematicalRelation: '' has been replaced by 'linear'
d18O (TR12SAMU06): interpretation5_rank: '' has been replaced by '2'
d18O (TR12SAMU06): interpretation5_scope: '' has been replaced by 'isotope'
d18O (TR12SAMU06): interpretation5_seasonality: '' has been replaced by 'May-Oct'
d18O (TR12SAMU06): interpretation5_seasonalityOriginal: '' has been replaced by 'May-October'
d18O (TR12SAMU06): interpretation5_variable: '' has been replaced by 'precipitation'
d18O (TR12SAMU06): interpretation5_variableGroup: '' has been replaced by 'P'
d18O (TR12SAMU06): interpretation5_variableOriginal: '' has been replaced by 'Precipitation_amount'
d18O (TR12SAMU06): interpretation6_direction: '' has been replaced by 'positive'
d18O (TR12SAMU06): interpretation6_mathematicalRelation: '' has been replaced by 'linear'
d18O (TR12SAMU06): interpretation6_rank: '' has been replaced by '3'
d18O (TR12SAMU06): interpretation6_scope: '' has been replaced by 'isotope'
d18O (TR12SAMU06): interpretation6_seasonality: '' has been replaced by 'May-Oct'
d18O (TR12SAMU06): interpretation6_seasonalityOriginal: '' has been replaced by 'May-October'
d18O (TR12SAMU06): interpretation6_variable: '' has been replaced by 'temperature'
d18O (TR12SAMU06): interpretation6_variableGroup: '' has been replaced by 'Temperature'
d18O (TR12SAMU06): interpretation6_variableGroupDirection: '' has been replaced by 'negative'
d18O (TR12SAMU06): interpretation6_variableGroupOriginal: '' has been replaced by 'T_air'