d18O (LS04YUWA): interpretation2_basis: 'The TIC d18O derived from downcore sediments effectively parallels the anthropogenic lake-level lowering (Figure 2). The anthropogenically induced drought is recorded in downcore sediments as a 6% increase in TIC d18O. During the El Nin?o years of 1982?83 and 1997?98, Walker Lake (like Pyramid Lake) received well above average moisture. The lake volume increased by 28% from its September 1981 value and the d18OL decreased 3.6% during the 1982?83 event [Benson et al., 1991]. This climate-induced wet event was well recorded in downcore sediments as a 3% decrease in TIC d18O (Figures 2b and 2c)' has been replaced by ''
d18O (LS04YUWA): interpretation2_direction: 'negative' has been replaced by ''
d18O (LS04YUWA): interpretation2_inferredMaterial: 'lake water' has been replaced by ''
d18O (LS04YUWA): interpretation2_integrationTime: '3' has been replaced by ''
d18O (LS04YUWA): interpretation2_integrationTimeUncertaintyType: 'chronology;' has been replaced by ''
d18O (LS04YUWA): interpretation2_integrationTimeUnits: 'years' has been replaced by ''
d18O (LS04YUWA): interpretation2_rank: '1' has been replaced by ''
d18O (LS04YUWA): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (LS04YUWA): interpretation2_variable: 'effectivePrecipitation' has been replaced by ''
d18O (LS04YUWA): interpretation2_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (LS04YUWA): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (LS04YUWA): interpretation2_variableGroupOriginal: 'P_E' has been replaced by ''
d18O (LS04YUWA): interpretation3_direction: 'negative' has been replaced by ''
d18O (LS04YUWA): interpretation3_rank: '2' has been replaced by ''
d18O (LS04YUWA): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (LS04YUWA): interpretation3_variable: 'temperature' has been replaced by ''
d18O (LS04YUWA): interpretation3_variableGroup: 'Temperature' has been replaced by ''
d18O (LS04YUWA): interpretation3_variableGroupDirection: 'negative' has been replaced by ''
d18O (LS04YUWA): interpretation3_variableGroupOriginal: 'T_water' has been replaced by ''
d18O (LS04YUWA): interpretation4_rank: '' has been replaced by '1'
d18O (LS04YUWA): interpretation4_basis: '' has been replaced by 'The TIC d18O derived from downcore sediments effectively parallels the anthropogenic lake-level lowering (Figure 2). The anthropogenically induced drought is recorded in downcore sediments as a 6% increase in TIC d18O. During the El Nin?o years of 1982?83 and 1997?98, Walker Lake (like Pyramid Lake) received well above average moisture. The lake volume increased by 28% from its September 1981 value and the d18OL decreased 3.6% during the 1982?83 event [Benson et al., 1991]. This climate-induced wet event was well recorded in downcore sediments as a 3% decrease in TIC d18O (Figures 2b and 2c)'
d18O (LS04YUWA): interpretation4_direction: '' has been replaced by 'negative'
d18O (LS04YUWA): interpretation4_inferredMaterial: '' has been replaced by 'lake water'
d18O (LS04YUWA): interpretation4_integrationTime: '' has been replaced by '3'
d18O (LS04YUWA): interpretation4_integrationTimeUncertaintyType: '' has been replaced by 'chronology;'
d18O (LS04YUWA): interpretation4_integrationTimeUnits: '' has been replaced by 'years'
d18O (LS04YUWA): interpretation4_variable: '' has been replaced by 'effectivePrecipitation'
d18O (LS04YUWA): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (LS04YUWA): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (LS04YUWA): interpretation4_variableGroupOriginal: '' has been replaced by 'P_E'
d18O (LS04YUWA): interpretation5_direction: '' has been replaced by 'negative'
d18O (LS04YUWA): interpretation5_rank: '' has been replaced by '2'
d18O (LS04YUWA): interpretation5_scope: '' has been replaced by 'isotope'
d18O (LS04YUWA): interpretation5_variable: '' has been replaced by 'temperature'
d18O (LS04YUWA): interpretation5_variableGroup: '' has been replaced by 'Temperature'
d18O (LS04YUWA): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d18O (LS04YUWA): interpretation5_variableGroupOriginal: '' has been replaced by 'T_water'
d18O (LS04YUWA): interpretation6_scope: '' has been replaced by 'isotope'
CaCO3 (WEBa4c9285c): interpretation1_scope: 'isotope' has been replaced by 'climate'
CaCO3 (WEBa4c9285c): interpretation2_scope: 'isotope' has been replaced by 'climate'
CaCO3 (WEBa4c9285c): interpretation3_scope: 'isotope' has been replaced by 'climate'
CaCO3 (WEBa4c9285c): interpretation4_scope: '' has been replaced by 'isotope'
CaCO3 (WEBa4c9285c): interpretation5_scope: '' has been replaced by 'isotope'
CaCO3 (WEBa4c9285c): interpretation6_scope: '' has been replaced by 'isotope'
TIC (WEBbfa46c07): interpretation1_scope: 'isotope' has been replaced by 'climate'
TIC (WEBbfa46c07): interpretation2_scope: 'isotope' has been replaced by 'climate'
TIC (WEBbfa46c07): interpretation3_scope: 'isotope' has been replaced by 'climate'
TIC (WEBbfa46c07): interpretation4_scope: '' has been replaced by 'isotope'
TIC (WEBbfa46c07): interpretation5_scope: '' has been replaced by 'isotope'
TIC (WEBbfa46c07): interpretation6_scope: '' has been replaced by 'isotope'
d13C (WEBedf590e2): interpretation1_scope: 'isotope' has been replaced by 'climate'
d13C (WEBedf590e2): interpretation2_scope: 'isotope' has been replaced by 'climate'
d13C (WEBedf590e2): interpretation3_scope: 'isotope' has been replaced by 'climate'
d13C (WEBedf590e2): interpretation4_scope: '' has been replaced by 'isotope'
d13C (WEBedf590e2): interpretation5_scope: '' has been replaced by 'isotope'
d13C (WEBedf590e2): interpretation6_scope: '' has been replaced by 'isotope'