d18O (CO98QUNC01A): interpretation2_basis: 'Calibration between the instrument (local SST and gridded GISST2) and proxy records was evaluated using two regression techniques: standard ordinary least sqaures and reduced major axis.' has been replaced by ''
d18O (CO98QUNC01A): interpretation2_direction: 'negative' has been replaced by ''
d18O (CO98QUNC01A): interpretation2_fraction: '0.77' has been replaced by ''
d18O (CO98QUNC01A): interpretation2_inferredMaterial: 'seawater' has been replaced by ''
d18O (CO98QUNC01A): interpretation2_integrationTime: '3 months (1657-1952), 12 months (1952-1992)' has been replaced by ''
d18O (CO98QUNC01A): interpretation2_integrationTimeBasis: 'For the upper part of the record (1992-1952) a calendar year was first assigned to each density-band couplet and hence to every 12 samples assuming linear subannual skeletal extension. Second, systematic variations in oxygen isotopic composition were correlated with monthly SST values by using the AnalySeties program [Paillard et al., 1996] to match the peaks and troughs in the two time series. For the lower part of the record (1657-1951), simple band counting was used to extend the chronology back to the beginning of the record, which we estimate to be 1657. Although we have no absolute dates on this coral, Crowley et al. [1997] recently demonstrated that some of the distinctive cool excursions in the mean annual record coincide within 1 year of known volcanic eruptions as determined from the volcano chronology of Sirekin and Siebert [1994] and various ice core records' has been replaced by ''
d18O (CO98QUNC01A): interpretation2_integrationTimeUncertainty: '2-3 months' has been replaced by ''
d18O (CO98QUNC01A): interpretation2_integrationTimeUncertaintyType: 'chronological' has been replaced by ''
d18O (CO98QUNC01A): interpretation2_integrationTimeUnits: 'year' has been replaced by ''
d18O (CO98QUNC01A): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (CO98QUNC01A): interpretation2_rank: '1' has been replaced by ''
d18O (CO98QUNC01A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (CO98QUNC01A): interpretation2_seasonality: 'subannual' has been replaced by ''
d18O (CO98QUNC01A): interpretation2_variable: 'temperature' has been replaced by ''
d18O (CO98QUNC01A): interpretation2_variableGroup: 'Temperature' has been replaced by ''
d18O (CO98QUNC01A): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (CO98QUNC01A): interpretation2_variableGroupOriginal: 'T_water' has been replaced by ''
d18O (CO98QUNC01A): interpretation3_direction: 'positive' has been replaced by ''
d18O (CO98QUNC01A): interpretation3_inferredMaterial: 'seawater' has been replaced by ''
d18O (CO98QUNC01A): interpretation3_integrationTime: '3 months (1657-1952), 12 months (1952-1992)' has been replaced by ''
d18O (CO98QUNC01A): interpretation3_integrationTimeBasis: 'For the upper part of the record (1992-1952) a calendar year was first assigned to each density-band couplet and hence to every 12 samples assuming linear subannual skeletal extension. Second, systematic variations in oxygen isotopic composition were correlated with monthly SST values by using the AnalySeties program [Paillard et al., 1996] to match the peaks and troughs in the two time series. For the lower part of the record (1657-1951), simple band counting was used to extend the chronology back to the beginning of the record, which we estimate to be 1657. Although we have no absolute dates on this coral, Crowley et al. [1997] recently demonstrated that some of the distinctive cool excursions in the mean annual record coincide within 1 year of known volcanic eruptions as determined from the volcano chronology of Sirekin and Siebert [1994] and various ice core records' has been replaced by ''
d18O (CO98QUNC01A): interpretation3_integrationTimeUncertainty: '2-3 months' has been replaced by ''
d18O (CO98QUNC01A): interpretation3_integrationTimeUncertaintyType: 'chronological' has been replaced by ''
d18O (CO98QUNC01A): interpretation3_integrationTimeUnits: 'year' has been replaced by ''
d18O (CO98QUNC01A): interpretation3_mathematicalRelation: 'linear' has been replaced by ''
d18O (CO98QUNC01A): interpretation3_rank: '2' has been replaced by ''
d18O (CO98QUNC01A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (CO98QUNC01A): interpretation3_variable: 'seawaterIsotope' has been replaced by ''
d18O (CO98QUNC01A): interpretation3_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (CO98QUNC01A): interpretation3_variableGroupDirection: 'negative' has been replaced by ''
d18O (CO98QUNC01A): interpretation3_variableGroupOriginal: 'd18O_seawater' has been replaced by ''
d18O (CO98QUNC01A): interpretation4_basis: '' has been replaced by 'Calibration between the instrument (local SST and gridded GISST2) and proxy records was evaluated using two regression techniques: standard ordinary least sqaures and reduced major axis.'
d18O (CO98QUNC01A): interpretation4_direction: '' has been replaced by 'negative'
d18O (CO98QUNC01A): interpretation4_fraction: '' has been replaced by '0.77'
d18O (CO98QUNC01A): interpretation4_inferredMaterial: '' has been replaced by 'seawater'
d18O (CO98QUNC01A): interpretation4_integrationTime: '' has been replaced by '3 months (1657-1952), 12 months (1952-1992)'
d18O (CO98QUNC01A): interpretation4_integrationTimeBasis: '' has been replaced by 'For the upper part of the record (1992-1952) a calendar year was first assigned to each density-band couplet and hence to every 12 samples assuming linear subannual skeletal extension. Second, systematic variations in oxygen isotopic composition were correlated with monthly SST values by using the AnalySeties program [Paillard et al., 1996] to match the peaks and troughs in the two time series. For the lower part of the record (1657-1951), simple band counting was used to extend the chronology back to the beginning of the record, which we estimate to be 1657. Although we have no absolute dates on this coral, Crowley et al. [1997] recently demonstrated that some of the distinctive cool excursions in the mean annual record coincide within 1 year of known volcanic eruptions as determined from the volcano chronology of Sirekin and Siebert [1994] and various ice core records'
d18O (CO98QUNC01A): interpretation4_integrationTimeUncertainty: '' has been replaced by '2-3 months'
d18O (CO98QUNC01A): interpretation4_integrationTimeUncertaintyType: '' has been replaced by 'chronological'
d18O (CO98QUNC01A): interpretation4_integrationTimeUnits: '' has been replaced by 'year'
d18O (CO98QUNC01A): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (CO98QUNC01A): interpretation4_rank: '' has been replaced by '1'
d18O (CO98QUNC01A): interpretation4_scope: '' has been replaced by 'isotope'
d18O (CO98QUNC01A): interpretation4_seasonality: '' has been replaced by 'subannual'
d18O (CO98QUNC01A): interpretation4_variable: '' has been replaced by 'temperature'
d18O (CO98QUNC01A): interpretation4_variableGroup: '' has been replaced by 'Temperature'
d18O (CO98QUNC01A): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (CO98QUNC01A): interpretation4_variableGroupOriginal: '' has been replaced by 'T_water'
d18O (CO98QUNC01A): interpretation5_direction: '' has been replaced by 'positive'
d18O (CO98QUNC01A): interpretation5_inferredMaterial: '' has been replaced by 'seawater'
d18O (CO98QUNC01A): interpretation5_integrationTime: '' has been replaced by '3 months (1657-1952), 12 months (1952-1992)'
d18O (CO98QUNC01A): interpretation5_integrationTimeBasis: '' has been replaced by 'For the upper part of the record (1992-1952) a calendar year was first assigned to each density-band couplet and hence to every 12 samples assuming linear subannual skeletal extension. Second, systematic variations in oxygen isotopic composition were correlated with monthly SST values by using the AnalySeties program [Paillard et al., 1996] to match the peaks and troughs in the two time series. For the lower part of the record (1657-1951), simple band counting was used to extend the chronology back to the beginning of the record, which we estimate to be 1657. Although we have no absolute dates on this coral, Crowley et al. [1997] recently demonstrated that some of the distinctive cool excursions in the mean annual record coincide within 1 year of known volcanic eruptions as determined from the volcano chronology of Sirekin and Siebert [1994] and various ice core records'
d18O (CO98QUNC01A): interpretation5_integrationTimeUncertainty: '' has been replaced by '2-3 months'
d18O (CO98QUNC01A): interpretation5_integrationTimeUncertaintyType: '' has been replaced by 'chronological'
d18O (CO98QUNC01A): interpretation5_integrationTimeUnits: '' has been replaced by 'year'
d18O (CO98QUNC01A): interpretation5_mathematicalRelation: '' has been replaced by 'linear'
d18O (CO98QUNC01A): interpretation5_rank: '' has been replaced by '2'
d18O (CO98QUNC01A): interpretation5_scope: '' has been replaced by 'isotope'
d18O (CO98QUNC01A): interpretation5_variable: '' has been replaced by 'seawaterIsotope'
d18O (CO98QUNC01A): interpretation5_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (CO98QUNC01A): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d18O (CO98QUNC01A): interpretation5_variableGroupOriginal: '' has been replaced by 'd18O_seawater'
d18O (CO98QUNC01A): interpretation6_scope: '' has been replaced by 'isotope'
depth (MAT7827f007c4): interpretation1_scope: '' has been replaced by 'climate'
depth (MAT7827f007c4): interpretation2_scope: '' has been replaced by 'climate'
depth (MAT7827f007c4): interpretation3_scope: '' has been replaced by 'climate'
year (MATf724531f7f): interpretation1_scope: '' has been replaced by 'climate'
year (MATf724531f7f): interpretation2_scope: '' has been replaced by 'climate'
year (MATf724531f7f): interpretation3_scope: '' has been replaced by 'climate'