Thermo Quest Delta Plux XP mass spectrometer
Changed isotopeInterpretation1_name from 'Palmer Draought Severity Index(combined effect o f temperature and precipitation amount)' to standardized equivalent P_E - check direction (GF)
; archiveType changed - was originally Tree ring cellulose (TR); archiveType changed - was originally Tree ring cellulose
OCh-S: In 1 file has been presented 6 graphs, which were presented later on again. Either leave 1 file with 6 graphs, or present only 1 graph with own link. Label is desapeer 06, 01, 02, 03, 04, 05. Same graphs repeated 5 times with different links.
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,
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.
; archiveType changed was originally Tree ring cellulose
Please add isotopeInterpretation1_name (GF)
TP (31/12/19): climate interpretations (P-negative, T_air-positive) were removed from isotopeInterpretation2 and 3; OCh-S: added
TP: this is a derived average of all other trees from the site, with d18O values normalised to zero.
Generally, lower precipitation levels correlate with higher d18O values of the precipitation (amount effect); at the same time, higher temperatures (usually associated with lower precipitation levels) also lead to d18O enrichment of soil water; acting together, these factors cause d18O enrichment of source water.
Grid of 15.0 deg N and 22.5 deg N and 100 deg E and 105 deg E
http://badc.nerc.ac.uk/data/cru and Dai et al. [2004]
Column 'TR12SAMU-chron-NA1', with variable name 'yearEnsemble', was added to the dataset
Updated lipdverse database entry with a changed file.
year (MAT1f7cb77c97): paleoData_isPrimary: '' has been replaced by 'TRUE'
year (MAT1f7cb77c97): paleoData_primaryAgeColumn: '' has been replaced by 'TRUE'
d18O (TR12SAMU00): paleoData_isPrimary: '' has been replaced by 'FALSE'
d18O (TR12SAMU00): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'
d18O (TR12SAMU01): paleoData_isPrimary: '' has been replaced by 'FALSE'
d18O (TR12SAMU01): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'
d18O (TR12SAMU02): paleoData_isPrimary: '' has been replaced by 'FALSE'
d18O (TR12SAMU02): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'
d18O (TR12SAMU03): paleoData_isPrimary: '' has been replaced by 'FALSE'
d18O (TR12SAMU03): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'
d18O (TR12SAMU04): paleoData_isPrimary: '' has been replaced by 'FALSE'
d18O (TR12SAMU04): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'
d18O (TR12SAMU05): paleoData_isPrimary: '' has been replaced by 'FALSE'
d18O (TR12SAMU05): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'
d18O (TR12SAMU06): paleoData_isPrimary: '' has been replaced by 'FALSE'
d18O (TR12SAMU06): paleoData_primaryAgeColumn: '' has been replaced by 'FALSE'
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'
d18O (TR12SAMU00): interpretation1_seasonality: 'May to October' has been replaced by 'May-Oct'
d18O (TR12SAMU00): interpretation1_variable: 'PDSI' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU00): interpretation2_seasonality: 'MJJASO' has been replaced by 'May-Oct'
d18O (TR12SAMU00): interpretation2_variable: 'P_E' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU01): interpretation1_seasonality: 'May, June, July, August, September, October' has been replaced by 'May-Oct'
d18O (TR12SAMU01): interpretation1_variable: 'PDSI' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU01): interpretation2_seasonality: 'MJJASO' has been replaced by 'May-Oct'
d18O (TR12SAMU01): interpretation2_variable: 'P_E' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU02): interpretation1_seasonality: 'May, June, July, August, September, October' has been replaced by 'May-Oct'
d18O (TR12SAMU02): interpretation1_variable: 'PDSI' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU02): interpretation2_seasonality: 'MJJASO' has been replaced by 'May-Oct'
d18O (TR12SAMU02): interpretation2_variable: 'P_E' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU03): interpretation1_seasonality: 'May, June, July, August, September, October' has been replaced by 'May-Oct'
d18O (TR12SAMU03): interpretation1_variable: 'PDSI' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU03): interpretation2_seasonality: 'MJJASO' has been replaced by 'May-Oct'
d18O (TR12SAMU03): interpretation2_variable: 'P_E' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU04): interpretation1_seasonality: 'May, June, July, August, September, October' has been replaced by 'May-Oct'
d18O (TR12SAMU04): interpretation1_variable: 'PDSI' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU04): interpretation2_seasonality: 'MJJASO' has been replaced by 'May-Oct'
d18O (TR12SAMU04): interpretation2_variable: 'P_E' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU05): interpretation1_seasonality: 'May, June, July, August, September, October' has been replaced by 'May-Oct'
d18O (TR12SAMU05): interpretation1_variable: 'PDSI' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU05): interpretation2_seasonality: 'MJJASO' has been replaced by 'May-Oct'
d18O (TR12SAMU05): interpretation2_variable: 'P_E' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU06): interpretation1_seasonality: 'May, June, July, August, September, October' has been replaced by 'May-Oct'
d18O (TR12SAMU06): interpretation1_variable: 'PDSI' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU06): interpretation2_seasonality: 'MJJASO' has been replaced by 'May-Oct'
d18O (TR12SAMU06): interpretation2_variable: 'P_E' has been replaced by 'effectivePrecipitation'
d18O (TR12SAMU06): interpretation3_seasonality: 'MJJASO' has been replaced by 'May-Oct'
d18O (TR12SAMU06): interpretation3_variable: 'P' has been replaced by 'precipitation'
d18O (TR12SAMU06): interpretation4_seasonality: 'MJJASO' has been replaced by 'May-Oct'
d18O (TR12SAMU06): interpretation4_variable: 'T_air' has been replaced by 'temperature'
Changes made as part of LiPDverse vocabulary standardization process
year (MAT1f7cb77c97): paleoData_units: 'AD' has been replaced by 'yr AD'
year (MAT1f7cb77c97): paleoData_longName: '' has been replaced by 'AD'
d18O (TR12SAMU00): paleoData_units: 'zscore' has been replaced by 'z score'
d18O (TR12SAMU00): paleoData_longName: '' has been replaced by 'AD'
d18O (TR12SAMU01): paleoData_longName: '' has been replaced by 'AD'
d18O (TR12SAMU02): paleoData_longName: '' has been replaced by 'AD'
d18O (TR12SAMU03): paleoData_longName: '' has been replaced by 'AD'
d18O (TR12SAMU04): paleoData_longName: '' has been replaced by 'AD'
d18O (TR12SAMU05): paleoData_longName: '' has been replaced by 'AD'
d18O (TR12SAMU06): paleoData_longName: '' has been replaced by 'AD'
Sano, M., Xu, C. and Nakatsuka, T.: A 300-year Vietnam hydroclimate and ENSO variability record reconstructed from tree ringδ18O, Journal of Geophysical Research: Atmospheres, 117(D12), n/a–n/a, doi:10.1029/2012jd017749, 2012.