d18O (LS06TIST): interpretation2_basis: 'However, two lines of evidence indicate that at Steel Lake, evaporative 18O enrichment related to aridity was the dominant control. First, the d18O values of water samples from the epilimnion and hypolimnion of Steel Lake were 8.7 and 10.7%, respectively, in July 2001 (Figure 1d). The elevated d18O value of the epilimnetic water resulted from evaporative 18O enrichment, suggesting that Steel  Lake is sensitive to evaporation;In particular, the most severe historic drought events in north-central Minnesota, the 1988 drought [Trenberth et al., 1988] and 1930s Dust Bowl [Worster, 1979], are recorded by the heaviest d18O values at Steel Lake' has been replaced by ''
d18O (LS06TIST): interpretation2_direction: 'negative' has been replaced by ''
d18O (LS06TIST): interpretation2_inferredMaterial: 'lake water' has been replaced by ''
d18O (LS06TIST): interpretation2_integrationTime: '5' has been replaced by ''
d18O (LS06TIST): interpretation2_integrationTimeBasis: 'varve counts' has been replaced by ''
d18O (LS06TIST): interpretation2_integrationTimeUncertaintyType: 'sampling resoluton' has been replaced by ''
d18O (LS06TIST): interpretation2_integrationTimeUnits: 'years' has been replaced by ''
d18O (LS06TIST): interpretation2_rank: '1' has been replaced by ''
d18O (LS06TIST): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (LS06TIST): interpretation2_variable: 'effectivePrecipitation' has been replaced by ''
d18O (LS06TIST): interpretation2_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (LS06TIST): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (LS06TIST): interpretation2_variableGroupOriginal: 'P_E' has been replaced by ''
d18O (LS06TIST): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (LS06TIST): interpretation4_rank: '' has been replaced by '1'
d18O (LS06TIST): interpretation4_basis: '' has been replaced by 'However, two lines of evidence indicate that at Steel Lake, evaporative 18O enrichment related to aridity was the dominant control. First, the d18O values of water samples from the epilimnion and hypolimnion of Steel Lake were 8.7 and 10.7%, respectively, in July 2001 (Figure 1d). The elevated d18O value of the epilimnetic water resulted from evaporative 18O enrichment, suggesting that Steel  Lake is sensitive to evaporation;In particular, the most severe historic drought events in north-central Minnesota, the 1988 drought [Trenberth et al., 1988] and 1930s Dust Bowl [Worster, 1979], are recorded by the heaviest d18O values at Steel Lake'
d18O (LS06TIST): interpretation4_direction: '' has been replaced by 'negative'
d18O (LS06TIST): interpretation4_inferredMaterial: '' has been replaced by 'lake water'
d18O (LS06TIST): interpretation4_integrationTime: '' has been replaced by '5'
d18O (LS06TIST): interpretation4_integrationTimeBasis: '' has been replaced by 'varve counts'
d18O (LS06TIST): interpretation4_integrationTimeUncertaintyType: '' has been replaced by 'sampling resoluton'
d18O (LS06TIST): interpretation4_integrationTimeUnits: '' has been replaced by 'years'
d18O (LS06TIST): interpretation4_variable: '' has been replaced by 'effectivePrecipitation'
d18O (LS06TIST): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (LS06TIST): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (LS06TIST): interpretation4_variableGroupOriginal: '' has been replaced by 'P_E'
d18O (LS06TIST): interpretation5_scope: '' has been replaced by 'isotope'
d18O (LS06TIST): interpretation6_scope: '' has been replaced by 'isotope'
year (MATf47550ae7d): interpretation1_scope: '' has been replaced by 'climate'
year (MATf47550ae7d): interpretation2_scope: '' has been replaced by 'climate'
depth (MATf6335d8d19): interpretation1_scope: '' has been replaced by 'climate'
depth (MATf6335d8d19): interpretation2_scope: '' has been replaced by 'climate'