year (MATad36c816e2): interpretation1_scope: '' has been replaced by 'climate'
year (MATad36c816e2): interpretation2_scope: '' has been replaced by 'climate'
d18O (TR07RECA01): interpretation2_basis: 'Correlations with 18O of precipitation (GNIP data) showed that source water signals are preserved in d18O tree rings. A possible explanation for the common decadal-to century scale trends, not directly related to mean monthly air temperature or precipitation amount, is variations in moisture source determined by the dominant atmospheric circulation pattern. The NAO index, determinates diminant wind pattern and temperature, and precipitation systems over Europe and influences d18O precipitation in Switzerland.' has been replaced by ''
d18O (TR07RECA01): interpretation2_direction: 'positive' has been replaced by ''
d18O (TR07RECA01): interpretation2_inferredMaterial: 'precipitation' has been replaced by ''
d18O (TR07RECA01): interpretation2_integrationTime: '1' has been replaced by ''
d18O (TR07RECA01): interpretation2_integrationTimeUnits: 'years' has been replaced by ''
d18O (TR07RECA01): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d18O (TR07RECA01): interpretation2_rank: '1' has been replaced by ''
d18O (TR07RECA01): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (TR07RECA01): interpretation2_seasonality: 'May-Jun' has been replaced by ''
d18O (TR07RECA01): interpretation2_seasonalityOriginal: 'P_amount (May, June), T_air (June, July, August,September)' has been replaced by ''
d18O (TR07RECA01): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d18O (TR07RECA01): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d18O (TR07RECA01): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d18O (TR07RECA01): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (TR07RECA01): interpretation3_variableGroupOriginal: 'P_E' has been replaced by ''
d18O (TR07RECA01): interpretation4_basis: '' has been replaced by 'Correlations with 18O of precipitation (GNIP data) showed that source water signals are preserved in d18O tree rings. A possible explanation for the common decadal-to century scale trends, not directly related to mean monthly air temperature or precipitation amount, is variations in moisture source determined by the dominant atmospheric circulation pattern. The NAO index, determinates diminant wind pattern and temperature, and precipitation systems over Europe and influences d18O precipitation in Switzerland.'
d18O (TR07RECA01): interpretation4_direction: '' has been replaced by 'positive'
d18O (TR07RECA01): interpretation4_inferredMaterial: '' has been replaced by 'precipitation'
d18O (TR07RECA01): interpretation4_integrationTime: '' has been replaced by '1'
d18O (TR07RECA01): interpretation4_integrationTimeUnits: '' has been replaced by 'years'
d18O (TR07RECA01): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d18O (TR07RECA01): interpretation4_rank: '' has been replaced by '1'
d18O (TR07RECA01): interpretation4_scope: '' has been replaced by 'isotope'
d18O (TR07RECA01): interpretation4_seasonality: '' has been replaced by 'May-Jun'
d18O (TR07RECA01): interpretation4_seasonalityOriginal: '' has been replaced by 'P_amount (May, June), T_air (June, July, August,September)'
d18O (TR07RECA01): interpretation4_variable: '' has been replaced by 'precipitationIsotope'
d18O (TR07RECA01): interpretation4_variableGroup: '' has been replaced by 'P_isotope'
d18O (TR07RECA01): interpretation4_variableGroupDirection: '' has been replaced by 'positive'
d18O (TR07RECA01): interpretation5_scope: '' has been replaced by 'isotope'
d18O (TR07RECA01): interpretation5_variableGroupOriginal: '' has been replaced by 'P_E'
d18O (TR07RECA01): interpretation6_scope: '' has been replaced by 'isotope'