year (LPD5024de7f): interpretation1_scope: '' has been replaced by 'climate'
year (LPD5024de7f): interpretation2_scope: '' has been replaced by 'climate'
year (LPD5024de7f): interpretation3_scope: '' has been replaced by 'climate'
year (LPDdcf3abca): interpretation1_scope: '' has been replaced by 'climate'
year (LPDdcf3abca): interpretation2_scope: '' has been replaced by 'climate'
year (LPDdcf3abca): interpretation3_scope: '' has been replaced by 'climate'
d18O (Ocean2kHR_140): interpretation2_basis: 'This tracer responds to water temperature through a temperature- dependent fractionation [~ -0.2 permil d18O/degree C (19, 20)], as well as to changes in rainfall, due to the influence of isotopically light (more negative d18O) rainfall on surface ocean composition. Because SST and rainfall are intimately linked in tropical areas of strong convective rainfall such as the western equatorial Pacific, the two factors combine to produce an enhanced climatic signal in coral skeletal d18O.' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_direction: 'negative' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_inferredMaterial: 'seawater' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_integrationTime: '3' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_integrationTimeBasis: 'The chronologies were subsequently developed on the basis of seasonality in skeletal d18O and d13C, supported by examination of annual skeletal density and fluorescent banding.' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_integrationTimeUnits: 'months' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_rank: '1' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (Ocean2kHR_140): interpretation2_seasonality: 'subannual' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_variable: 'temperature' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_variableGroup: 'Temperature' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (Ocean2kHR_140): interpretation2_variableGroupOriginal: 'T_water' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_basis: 'This tracer responds to water temperature through a temperature- dependent fractionation [~ -0.2 permil d18O/degree C (19, 20)], as well as to changes in rainfall, due to the influence of isotopically light (more negative d18O) rainfall on surface ocean composition. Because SST and rainfall are intimately linked in tropical areas of strong convective rainfall such as the western equatorial Pacific, the two factors combine to produce an enhanced climatic signal in coral skeletal d18O.' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_direction: 'positive' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_inferredMaterial: 'seawater' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_integrationTime: '3' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_integrationTimeBasis: 'The chronologies were subsequently developed on the basis of seasonality in skeletal d18O and d13C, supported by examination of annual skeletal density and fluorescent banding.' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_integrationTimeUnits: 'months' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_mathematicalRelation: 'linear' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_rank: '2' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (Ocean2kHR_140): interpretation3_variable: 'seawaterIsotope' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_variableGroupDirection: 'negative' has been replaced by ''
d18O (Ocean2kHR_140): interpretation3_variableGroupOriginal: 'd18O_seawater' has been replaced by ''
d18O (Ocean2kHR_140): interpretation4_basis: '' has been replaced by 'This tracer responds to water temperature through a temperature- dependent fractionation [~ -0.2 permil d18O/degree C (19, 20)], as well as to changes in rainfall, due to the influence of isotopically light (more negative d18O) rainfall on surface ocean composition. Because SST and rainfall are intimately linked in tropical areas of strong convective rainfall such as the western equatorial Pacific, the two factors combine to produce an enhanced climatic signal in coral skeletal d18O.'
d18O (Ocean2kHR_140): interpretation4_direction: '' has been replaced by 'negative'
d18O (Ocean2kHR_140): interpretation4_inferredMaterial: '' has been replaced by 'seawater'
d18O (Ocean2kHR_140): interpretation4_integrationTime: '' has been replaced by '3'
d18O (Ocean2kHR_140): interpretation4_integrationTimeBasis: '' has been replaced by 'The chronologies were subsequently developed on the basis of seasonality in skeletal d18O and d13C, supported by examination of annual skeletal density and fluorescent banding.'
d18O (Ocean2kHR_140): interpretation4_integrationTimeUnits: '' has been replaced by 'months'
d18O (Ocean2kHR_140): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (Ocean2kHR_140): interpretation4_rank: '' has been replaced by '1'
d18O (Ocean2kHR_140): interpretation4_scope: '' has been replaced by 'isotope'
d18O (Ocean2kHR_140): interpretation4_seasonality: '' has been replaced by 'subannual'
d18O (Ocean2kHR_140): interpretation4_variable: '' has been replaced by 'temperature'
d18O (Ocean2kHR_140): interpretation4_variableGroup: '' has been replaced by 'Temperature'
d18O (Ocean2kHR_140): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (Ocean2kHR_140): interpretation4_variableGroupOriginal: '' has been replaced by 'T_water'
d18O (Ocean2kHR_140): interpretation5_basis: '' has been replaced by 'This tracer responds to water temperature through a temperature- dependent fractionation [~ -0.2 permil d18O/degree C (19, 20)], as well as to changes in rainfall, due to the influence of isotopically light (more negative d18O) rainfall on surface ocean composition. Because SST and rainfall are intimately linked in tropical areas of strong convective rainfall such as the western equatorial Pacific, the two factors combine to produce an enhanced climatic signal in coral skeletal d18O.'
d18O (Ocean2kHR_140): interpretation5_direction: '' has been replaced by 'positive'
d18O (Ocean2kHR_140): interpretation5_inferredMaterial: '' has been replaced by 'seawater'
d18O (Ocean2kHR_140): interpretation5_integrationTime: '' has been replaced by '3'
d18O (Ocean2kHR_140): interpretation5_integrationTimeBasis: '' has been replaced by 'The chronologies were subsequently developed on the basis of seasonality in skeletal d18O and d13C, supported by examination of annual skeletal density and fluorescent banding.'
d18O (Ocean2kHR_140): interpretation5_integrationTimeUnits: '' has been replaced by 'months'
d18O (Ocean2kHR_140): interpretation5_mathematicalRelation: '' has been replaced by 'linear'
d18O (Ocean2kHR_140): interpretation5_rank: '' has been replaced by '2'
d18O (Ocean2kHR_140): interpretation5_scope: '' has been replaced by 'isotope'
d18O (Ocean2kHR_140): interpretation5_variable: '' has been replaced by 'seawaterIsotope'
d18O (Ocean2kHR_140): interpretation5_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (Ocean2kHR_140): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d18O (Ocean2kHR_140): interpretation5_variableGroupOriginal: '' has been replaced by 'd18O_seawater'
d18O (Ocean2kHR_140): interpretation6_scope: '' has been replaced by 'isotope'
d18O (Ocean2kHR_141): interpretation2_basis: 'This tracer responds to water temperature through a temperature- dependent fractionation [~ -0.2 permil d18O/degree C (19, 20)], as well as to changes in rainfall, due to the influence of isotopically light (more negative d18O) rainfall on surface ocean composition. Because SST and rainfall are intimately linked in tropical areas of strong convective rainfall such as the western equatorial Pacific, the two factors combine to produce an enhanced climatic signal in coral skeletal d18O.' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_direction: 'negative' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_inferredMaterial: 'seawater' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_integrationTime: '1 to 3 years' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_integrationTimeBasis: 'The chronologies were subsequently developed on the basis of seasonality in skeletal d18O and d13C, supported by examination of annual skeletal density and fluorescent banding.' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_integrationTimeUnits: 'months' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_rank: '1' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (Ocean2kHR_141): interpretation2_seasonality: 'subannual' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_variable: 'temperature' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_variableGroup: 'Temperature' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (Ocean2kHR_141): interpretation2_variableGroupOriginal: 'T_water' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_basis: 'This tracer responds to water temperature through a temperature- dependent fractionation [~ -0.2 permil d18O/degree C (19, 20)], as well as to changes in rainfall, due to the influence of isotopically light (more negative d18O) rainfall on surface ocean composition. Because SST and rainfall are intimately linked in tropical areas of strong convective rainfall such as the western equatorial Pacific, the two factors combine to produce an enhanced climatic signal in coral skeletal d18O.' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_direction: 'positive' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_inferredMaterial: 'seawater' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_integrationTime: '3' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_integrationTimeBasis: 'The chronologies were subsequently developed on the basis of seasonality in skeletal d18O and d13C, supported by examination of annual skeletal density and fluorescent banding.' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_integrationTimeUnits: 'months' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_mathematicalRelation: 'linear' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_rank: '2' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (Ocean2kHR_141): interpretation3_variable: 'seawaterIsotope' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_variableGroupDirection: 'negative' has been replaced by ''
d18O (Ocean2kHR_141): interpretation3_variableGroupOriginal: 'd18O_seawater' has been replaced by ''
d18O (Ocean2kHR_141): interpretation4_basis: '' has been replaced by 'This tracer responds to water temperature through a temperature- dependent fractionation [~ -0.2 permil d18O/degree C (19, 20)], as well as to changes in rainfall, due to the influence of isotopically light (more negative d18O) rainfall on surface ocean composition. Because SST and rainfall are intimately linked in tropical areas of strong convective rainfall such as the western equatorial Pacific, the two factors combine to produce an enhanced climatic signal in coral skeletal d18O.'
d18O (Ocean2kHR_141): interpretation4_direction: '' has been replaced by 'negative'
d18O (Ocean2kHR_141): interpretation4_inferredMaterial: '' has been replaced by 'seawater'
d18O (Ocean2kHR_141): interpretation4_integrationTime: '' has been replaced by '1 to 3 years'
d18O (Ocean2kHR_141): interpretation4_integrationTimeBasis: '' has been replaced by 'The chronologies were subsequently developed on the basis of seasonality in skeletal d18O and d13C, supported by examination of annual skeletal density and fluorescent banding.'
d18O (Ocean2kHR_141): interpretation4_integrationTimeUnits: '' has been replaced by 'months'
d18O (Ocean2kHR_141): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (Ocean2kHR_141): interpretation4_rank: '' has been replaced by '1'
d18O (Ocean2kHR_141): interpretation4_scope: '' has been replaced by 'isotope'
d18O (Ocean2kHR_141): interpretation4_seasonality: '' has been replaced by 'subannual'
d18O (Ocean2kHR_141): interpretation4_variable: '' has been replaced by 'temperature'
d18O (Ocean2kHR_141): interpretation4_variableGroup: '' has been replaced by 'Temperature'
d18O (Ocean2kHR_141): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (Ocean2kHR_141): interpretation4_variableGroupOriginal: '' has been replaced by 'T_water'
d18O (Ocean2kHR_141): interpretation5_basis: '' has been replaced by 'This tracer responds to water temperature through a temperature- dependent fractionation [~ -0.2 permil d18O/degree C (19, 20)], as well as to changes in rainfall, due to the influence of isotopically light (more negative d18O) rainfall on surface ocean composition. Because SST and rainfall are intimately linked in tropical areas of strong convective rainfall such as the western equatorial Pacific, the two factors combine to produce an enhanced climatic signal in coral skeletal d18O.'
d18O (Ocean2kHR_141): interpretation5_direction: '' has been replaced by 'positive'
d18O (Ocean2kHR_141): interpretation5_inferredMaterial: '' has been replaced by 'seawater'
d18O (Ocean2kHR_141): interpretation5_integrationTime: '' has been replaced by '3'
d18O (Ocean2kHR_141): interpretation5_integrationTimeBasis: '' has been replaced by 'The chronologies were subsequently developed on the basis of seasonality in skeletal d18O and d13C, supported by examination of annual skeletal density and fluorescent banding.'
d18O (Ocean2kHR_141): interpretation5_integrationTimeUnits: '' has been replaced by 'months'
d18O (Ocean2kHR_141): interpretation5_mathematicalRelation: '' has been replaced by 'linear'
d18O (Ocean2kHR_141): interpretation5_rank: '' has been replaced by '2'
d18O (Ocean2kHR_141): interpretation5_scope: '' has been replaced by 'isotope'
d18O (Ocean2kHR_141): interpretation5_variable: '' has been replaced by 'seawaterIsotope'
d18O (Ocean2kHR_141): interpretation5_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (Ocean2kHR_141): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d18O (Ocean2kHR_141): interpretation5_variableGroupOriginal: '' has been replaced by 'd18O_seawater'
d18O (Ocean2kHR_141): interpretation6_scope: '' has been replaced by 'isotope'