year (MAT4c306207d3): interpretation1_scope: '' has been replaced by 'climate'
year (MAT4c306207d3): interpretation2_scope: '' has been replaced by 'climate'
d18O (Ocean2kHR_020): interpretation2_basis: 'A correlation of seasonal mean rainfall anomalies derived from the NCEP/NCAR reanalysis data set (1948-1995; averaged over 3545E, 20-30S; http://www. cdc.noaa.gov/cdc/data.ncep.reanalysis.derived.html) with coral d18O shows a clear relationship during austral summer (NDJF) significant above the 90% level (Fig. 6). This also holds for a correlation with South African summer rainfall averaged over 25-30E and 15-25S (significant N95%) (Fig. 6). Thus, summer coral d18O is also related to changes in the regional hydrologic (P/E) balance' has been replaced by ''
d18O (Ocean2kHR_020): interpretation2_direction: 'negative' has been replaced by ''
d18O (Ocean2kHR_020): interpretation2_inferredMaterial: 'seawater' has been replaced by ''
d18O (Ocean2kHR_020): interpretation2_integrationTime: '2-Jan' has been replaced by ''
d18O (Ocean2kHR_020): interpretation2_integrationTimeBasis: 'We use the pronounced seasonal cycle in d18O and Sr/Ca to develop the final chronology of the coral core and assigned the highest d18O and Sr/Ca values to august 15 of each year, which is on average the coldest month. [...] The d18O and Sr/Ca time series were interpolated linearly into 6 and 12 equi- distant points for any given year between these anchor points using the Analyseries software,.083 to 0.167 yrs,chronological,months,on a seasonal scale coral d18O  and Sr/Ca at this location primarily reflects SST variability (Fig. 5; Table 1). "' has been replaced by ''
d18O (Ocean2kHR_020): interpretation2_integrationTimeUncertaintyType: 'decrease' has been replaced by ''
d18O (Ocean2kHR_020): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (Ocean2kHR_020): interpretation2_rank: '1' has been replaced by ''
d18O (Ocean2kHR_020): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (Ocean2kHR_020): interpretation2_seasonality: 'subannual' has been replaced by ''
d18O (Ocean2kHR_020): interpretation2_variable: 'temperature' has been replaced by ''
d18O (Ocean2kHR_020): interpretation2_variableGroup: 'Temperature' has been replaced by ''
d18O (Ocean2kHR_020): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (Ocean2kHR_020): interpretation2_variableGroupOriginal: 'T_water' has been replaced by ''
d18O (Ocean2kHR_020): interpretation3_direction: '2' has been replaced by ''
d18O (Ocean2kHR_020): interpretation3_inferredMaterial: 'seawater' has been replaced by ''
d18O (Ocean2kHR_020): interpretation3_integrationTime: '2-Jan' has been replaced by ''
d18O (Ocean2kHR_020): interpretation3_integrationTimeBasis: 'We use the pronounced seasonal cycle in d18O and Sr/Ca to develop the final chronology of the coral core and assigned the highest d18O and Sr/Ca values to august 15 of each year, which is on average the coldest month. [...] The d18O and Sr/Ca time series were interpolated linearly into 6 and 12 equi- distant points for any given year between these anchor points using the Analyseries software|.083 to 0.167 yrs|chronological|months|on a seasonal scale coral d18O  and Sr/Ca at this location primarily reflects SST variability (Fig. 5; Table 1). "' has been replaced by ''
d18O (Ocean2kHR_020): interpretation3_integrationTimeUncertaintyType: 'decrease' has been replaced by ''
d18O (Ocean2kHR_020): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (Ocean2kHR_020): interpretation4_integrationTimeBasis: 'We use the pronounced seasonal cycle in d18O and Sr/Ca to develop the final chronology of the coral core and assigned the highest d18O and Sr/Ca values to august 15 of each year, which is on average the coldest month. [...] The d18O and Sr/Ca time series were interpolated linearly into 6 and 12 equi- distant points for any given year between these anchor points using the Analyseries software|.083 to 0.167 yrs|chronological|months|on a seasonal scale coral d18O  and Sr/Ca at this location primarily reflects SST variability (Fig. 5; Table 1). "' has been replaced by 'We use the pronounced seasonal cycle in d18O and Sr/Ca to develop the final chronology of the coral core and assigned the highest d18O and Sr/Ca values to august 15 of each year, which is on average the coldest month. [...] The d18O and Sr/Ca time series were interpolated linearly into 6 and 12 equi- distant points for any given year between these anchor points using the Analyseries software,.083 to 0.167 yrs,chronological,months,on a seasonal scale coral d18O  and Sr/Ca at this location primarily reflects SST variability (Fig. 5; Table 1). "'
d18O (Ocean2kHR_020): interpretation4_mathematicalRelation: 'Sr/Ca avaiable for select intervals' has been replaced by 'linear'
d18O (Ocean2kHR_020): interpretation4_variableGroup: 'JZ, NJA' has been replaced by 'Temperature'
d18O (Ocean2kHR_020): interpretation4_basis: '' has been replaced by 'A correlation of seasonal mean rainfall anomalies derived from the NCEP/NCAR reanalysis data set (1948-1995; averaged over 3545E, 20-30S; http://www. cdc.noaa.gov/cdc/data.ncep.reanalysis.derived.html) with coral d18O shows a clear relationship during austral summer (NDJF) significant above the 90% level (Fig. 6). This also holds for a correlation with South African summer rainfall averaged over 25-30E and 15-25S (significant N95%) (Fig. 6). Thus, summer coral d18O is also related to changes in the regional hydrologic (P/E) balance'
d18O (Ocean2kHR_020): interpretation4_direction: '' has been replaced by 'negative'
d18O (Ocean2kHR_020): interpretation4_rank: '' has been replaced by '1'
d18O (Ocean2kHR_020): interpretation4_seasonality: '' has been replaced by 'subannual'
d18O (Ocean2kHR_020): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (Ocean2kHR_020): interpretation4_variableGroupOriginal: '' has been replaced by 'T_water'
d18O (Ocean2kHR_020): interpretation5_direction: '' has been replaced by '2'
d18O (Ocean2kHR_020): interpretation5_inferredMaterial: '' has been replaced by 'seawater'
d18O (Ocean2kHR_020): interpretation5_integrationTime: '' has been replaced by '2-Jan'
d18O (Ocean2kHR_020): interpretation5_integrationTimeBasis: '' has been replaced by 'We use the pronounced seasonal cycle in d18O and Sr/Ca to develop the final chronology of the coral core and assigned the highest d18O and Sr/Ca values to august 15 of each year, which is on average the coldest month. [...] The d18O and Sr/Ca time series were interpolated linearly into 6 and 12 equi- distant points for any given year between these anchor points using the Analyseries software|.083 to 0.167 yrs|chronological|months|on a seasonal scale coral d18O  and Sr/Ca at this location primarily reflects SST variability (Fig. 5; Table 1). "'
d18O (Ocean2kHR_020): interpretation5_integrationTimeUncertaintyType: '' has been replaced by 'decrease'
d18O (Ocean2kHR_020): interpretation5_scope: '' has been replaced by 'isotope'
d18O (Ocean2kHR_020): interpretation6_inferredMaterial: '' has been replaced by 'seawater'
d18O (Ocean2kHR_020): interpretation6_integrationTime: '' has been replaced by '2-Jan'
d18O (Ocean2kHR_020): interpretation6_integrationTimeBasis: '' has been replaced by 'We use the pronounced seasonal cycle in d18O and Sr/Ca to develop the final chronology of the coral core and assigned the highest d18O and Sr/Ca values to august 15 of each year, which is on average the coldest month. [...] The d18O and Sr/Ca time series were interpolated linearly into 6 and 12 equi- distant points for any given year between these anchor points using the Analyseries software|.083 to 0.167 yrs|chronological|months|on a seasonal scale coral d18O  and Sr/Ca at this location primarily reflects SST variability (Fig. 5; Table 1). "'
d18O (Ocean2kHR_020): interpretation6_integrationTimeUncertaintyType: '' has been replaced by 'decrease'
d18O (Ocean2kHR_020): interpretation6_mathematicalRelation: '' has been replaced by 'Sr/Ca avaiable for select intervals'
d18O (Ocean2kHR_020): interpretation6_scope: '' has been replaced by 'isotope'
d18O (Ocean2kHR_020): interpretation6_variable: '' has been replaced by 'temperature'
d18O (Ocean2kHR_020): interpretation6_variableGroup: '' has been replaced by 'JZ, NJA'