d2H (LS14KOSA01A): interpretation2_basis: 'In East Africa, stable isotopes in modern precipitation have been shown to reflect large-scale atmospheric circulation processes (Vuille et al., 2005), and the ?18O of precipitation (and by inference, the ?D of precipitation) on Mt. Kenya has been shown to be a good indicator of moisture balance (Barker et al., 2001). Leaf wax ?D reflects ?Dprecip, after a series of offsets due to soil water evaporation, fractionation of leaf water relative to xylem water, and biosynthesis (Sachse et al., 2012).' has been replaced by ''
d2H (LS14KOSA01A): interpretation2_direction: 'positive' has been replaced by ''
d2H (LS14KOSA01A): interpretation2_inferredMaterial: 'soil water' has been replaced by ''
d2H (LS14KOSA01A): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d2H (LS14KOSA01A): interpretation2_rank: '1' has been replaced by ''
d2H (LS14KOSA01A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d2H (LS14KOSA01A): interpretation2_seasonality: 'Annual' has been replaced by ''
d2H (LS14KOSA01A): interpretation2_seasonalityOriginal: 'Annual' has been replaced by ''
d2H (LS14KOSA01A): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d2H (LS14KOSA01A): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d2H (LS14KOSA01A): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d2H (LS14KOSA01A): interpretation3_basis: 'Air temperature has 2 influences: "air temperature is important for the elevation of the zone of maximum rainfall (ZMR) on Mt. Kenya" and for soil/lake evaporation. "Recent drying may have also been locally enhanced by a recent rise in temperature (via an upward shift in the ZMR and/or increased evaporation of soil water)."' has been replaced by ''
d2H (LS14KOSA01A): interpretation3_direction: 'positive' has been replaced by ''
d2H (LS14KOSA01A): interpretation3_inferredMaterial: 'soil water' has been replaced by ''
d2H (LS14KOSA01A): interpretation3_rank: '2' has been replaced by ''
d2H (LS14KOSA01A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d2H (LS14KOSA01A): interpretation3_seasonality: 'Annual' has been replaced by ''
d2H (LS14KOSA01A): interpretation3_seasonalityOriginal: 'Annual' has been replaced by ''
d2H (LS14KOSA01A): interpretation3_variable: 'temperature' has been replaced by ''
d2H (LS14KOSA01A): interpretation3_variableGroup: 'Temperature' has been replaced by ''
d2H (LS14KOSA01A): interpretation3_variableGroupDirection: 'negative' has been replaced by ''
d2H (LS14KOSA01A): interpretation3_variableGroupOriginal: 'T_air' has been replaced by ''
d2H (LS14KOSA01A): interpretation4_basis: '' has been replaced by 'In East Africa, stable isotopes in modern precipitation have been shown to reflect large-scale atmospheric circulation processes (Vuille et al., 2005), and the ?18O of precipitation (and by inference, the ?D of precipitation) on Mt. Kenya has been shown to be a good indicator of moisture balance (Barker et al., 2001). Leaf wax ?D reflects ?Dprecip, after a series of offsets due to soil water evaporation, fractionation of leaf water relative to xylem water, and biosynthesis (Sachse et al., 2012).'
d2H (LS14KOSA01A): interpretation4_direction: '' has been replaced by 'positive'
d2H (LS14KOSA01A): interpretation4_inferredMaterial: '' has been replaced by 'soil water'
d2H (LS14KOSA01A): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d2H (LS14KOSA01A): interpretation4_rank: '' has been replaced by '1'
d2H (LS14KOSA01A): interpretation4_scope: '' has been replaced by 'isotope'
d2H (LS14KOSA01A): interpretation4_seasonality: '' has been replaced by 'Annual'
d2H (LS14KOSA01A): interpretation4_seasonalityOriginal: '' has been replaced by 'Annual'
d2H (LS14KOSA01A): interpretation4_variable: '' has been replaced by 'precipitationIsotope'
d2H (LS14KOSA01A): interpretation4_variableGroup: '' has been replaced by 'P_isotope'
d2H (LS14KOSA01A): interpretation4_variableGroupDirection: '' has been replaced by 'positive'
d2H (LS14KOSA01A): interpretation5_basis: '' has been replaced by 'Air temperature has 2 influences: "air temperature is important for the elevation of the zone of maximum rainfall (ZMR) on Mt. Kenya" and for soil/lake evaporation. "Recent drying may have also been locally enhanced by a recent rise in temperature (via an upward shift in the ZMR and/or increased evaporation of soil water)."'
d2H (LS14KOSA01A): interpretation5_direction: '' has been replaced by 'positive'
d2H (LS14KOSA01A): interpretation5_inferredMaterial: '' has been replaced by 'soil water'
d2H (LS14KOSA01A): interpretation5_rank: '' has been replaced by '2'
d2H (LS14KOSA01A): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS14KOSA01A): interpretation5_seasonality: '' has been replaced by 'Annual'
d2H (LS14KOSA01A): interpretation5_seasonalityOriginal: '' has been replaced by 'Annual'
d2H (LS14KOSA01A): interpretation5_variable: '' has been replaced by 'temperature'
d2H (LS14KOSA01A): interpretation5_variableGroup: '' has been replaced by 'Temperature'
d2H (LS14KOSA01A): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d2H (LS14KOSA01A): interpretation5_variableGroupOriginal: '' has been replaced by 'T_air'
d2H (LS14KOSA01A): interpretation6_scope: '' has been replaced by 'isotope'
year (MAT11712e4d07): interpretation1_scope: '' has been replaced by 'climate'
year (MAT11712e4d07): interpretation2_scope: '' has been replaced by 'climate'
year (MAT11712e4d07): interpretation3_scope: '' has been replaced by 'climate'
depth (MATb0c73ae5e6): interpretation1_scope: '' has been replaced by 'climate'
depth (MATb0c73ae5e6): interpretation2_scope: '' has been replaced by 'climate'
depth (MATb0c73ae5e6): interpretation3_scope: '' has been replaced by 'climate'