d2H (LS14FOTI01A): interpretation2_basis: 'Results from both observational and modeling studies suggest that the dominant control on modern interannual Andean ?Dp variability is Rayleigh-type fractionation during rainout along the trajectory of moist air masses across the Amazon Basin up to the Andes (e.g., Rozanski et al., 1993; Hoffmann et al., 2003; Vimeux et al., 2005; Vuille and Werner, 2005). Increased rainout along this trajectory, as well as increased local precipitation in the Andes, results in more depleted ?Dp, consistent with the continentality and amount effects that dominate ?Dp variability throughout most of tropical South America (Vuille et al., 2003).' has been replaced by ''
d2H (LS14FOTI01A): interpretation2_direction: 'positive' has been replaced by ''
d2H (LS14FOTI01A): interpretation2_inferredMaterial: 'soil water' has been replaced by ''
d2H (LS14FOTI01A): interpretation2_rank: '1' has been replaced by ''
d2H (LS14FOTI01A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d2H (LS14FOTI01A): interpretation2_seasonality: 'Dec-Feb' has been replaced by ''
d2H (LS14FOTI01A): interpretation2_seasonalityOriginal: 'SH summer' has been replaced by ''
d2H (LS14FOTI01A): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d2H (LS14FOTI01A): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d2H (LS14FOTI01A): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d2H (LS14FOTI01A): interpretation3_basis: 'Results from both observational and modeling studies suggest that the dominant control on modern interannual Andean ?Dp variability is Rayleigh-type fractionation during rainout along the trajectory of moist air masses across the Amazon Basin up to the Andes (e.g., Rozanski et al., 1993; Hoffmann et al., 2003; Vimeux et al., 2005; Vuille and Werner, 2005). Increased rainout along this trajectory, as well as increased local precipitation in the Andes, results in more depleted ?Dp, consistent with the continentality and amount effects that dominate ?Dp variability throughout most of tropical South America (Vuille et al., 2003).' has been replaced by ''
d2H (LS14FOTI01A): interpretation3_direction: 'negative' has been replaced by ''
d2H (LS14FOTI01A): interpretation3_inferredMaterial: 'soil water' has been replaced by ''
d2H (LS14FOTI01A): interpretation3_rank: '2' has been replaced by ''
d2H (LS14FOTI01A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d2H (LS14FOTI01A): interpretation3_seasonality: 'Dec-Feb' has been replaced by ''
d2H (LS14FOTI01A): interpretation3_seasonalityOriginal: 'SH summer' has been replaced by ''
d2H (LS14FOTI01A): interpretation3_variable: 'deleteMe' has been replaced by ''
d2H (LS14FOTI01A): interpretation3_variableGroup: 'continental effect' has been replaced by ''
d2H (LS14FOTI01A): interpretation4_basis: 'While the isotopic composition of precipitation appears to be the primary control on the structure of the LT ?Dwax record, it is clear that secondary effects also contribute to this signal. Most notably, the much larger range at LT (102h) than at Illimani (58h) over the past 19 kyr suggests the influence of compounding effects on LT ?Dwax, such as decreased regional precipitation, resulting in a more enriched ?Dp, and low local humidity, which would tend to further enrich plant source water by soil water evaporation and/or leaf transpiration. Since such local evapotranspiration feedbacks would be expected to act in step with ?Dp changes, this would serve to amplify the ?Dwax signal and increase its sensitivity to ?Dp variability.' has been replaced by 'Results from both observational and modeling studies suggest that the dominant control on modern interannual Andean ?Dp variability is Rayleigh-type fractionation during rainout along the trajectory of moist air masses across the Amazon Basin up to the Andes (e.g., Rozanski et al., 1993; Hoffmann et al., 2003; Vimeux et al., 2005; Vuille and Werner, 2005). Increased rainout along this trajectory, as well as increased local precipitation in the Andes, results in more depleted ?Dp, consistent with the continentality and amount effects that dominate ?Dp variability throughout most of tropical South America (Vuille et al., 2003).'
d2H (LS14FOTI01A): interpretation4_rank: '3' has been replaced by '1'
d2H (LS14FOTI01A): interpretation4_variable: 'evaporation' has been replaced by 'precipitationIsotope'
d2H (LS14FOTI01A): interpretation4_variableGroup: 'EffectiveMoisture' has been replaced by 'P_isotope'
d2H (LS14FOTI01A): interpretation4_variableGroupDirection: 'negative' has been replaced by 'positive'
d2H (LS14FOTI01A): interpretation4_variableGroupOriginal: 'soil water evapotranspiration' has been replaced by ''
d2H (LS14FOTI01A): interpretation4_seasonality: '' has been replaced by 'Dec-Feb'
d2H (LS14FOTI01A): interpretation4_seasonalityOriginal: '' has been replaced by 'SH summer'
d2H (LS14FOTI01A): interpretation5_basis: '' has been replaced by 'Results from both observational and modeling studies suggest that the dominant control on modern interannual Andean ?Dp variability is Rayleigh-type fractionation during rainout along the trajectory of moist air masses across the Amazon Basin up to the Andes (e.g., Rozanski et al., 1993; Hoffmann et al., 2003; Vimeux et al., 2005; Vuille and Werner, 2005). Increased rainout along this trajectory, as well as increased local precipitation in the Andes, results in more depleted ?Dp, consistent with the continentality and amount effects that dominate ?Dp variability throughout most of tropical South America (Vuille et al., 2003).'
d2H (LS14FOTI01A): interpretation5_direction: '' has been replaced by 'negative'
d2H (LS14FOTI01A): interpretation5_inferredMaterial: '' has been replaced by 'soil water'
d2H (LS14FOTI01A): interpretation5_rank: '' has been replaced by '2'
d2H (LS14FOTI01A): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS14FOTI01A): interpretation5_seasonality: '' has been replaced by 'Dec-Feb'
d2H (LS14FOTI01A): interpretation5_seasonalityOriginal: '' has been replaced by 'SH summer'
d2H (LS14FOTI01A): interpretation5_variable: '' has been replaced by 'deleteMe'
d2H (LS14FOTI01A): interpretation5_variableGroup: '' has been replaced by 'continental effect'
d2H (LS14FOTI01A): interpretation6_basis: '' has been replaced by 'While the isotopic composition of precipitation appears to be the primary control on the structure of the LT ?Dwax record, it is clear that secondary effects also contribute to this signal. Most notably, the much larger range at LT (102h) than at Illimani (58h) over the past 19 kyr suggests the influence of compounding effects on LT ?Dwax, such as decreased regional precipitation, resulting in a more enriched ?Dp, and low local humidity, which would tend to further enrich plant source water by soil water evaporation and/or leaf transpiration. Since such local evapotranspiration feedbacks would be expected to act in step with ?Dp changes, this would serve to amplify the ?Dwax signal and increase its sensitivity to ?Dp variability.'
d2H (LS14FOTI01A): interpretation6_direction: '' has been replaced by 'positive'
d2H (LS14FOTI01A): interpretation6_inferredMaterial: '' has been replaced by 'soil water'
d2H (LS14FOTI01A): interpretation6_rank: '' has been replaced by '3'
d2H (LS14FOTI01A): interpretation6_scope: '' has been replaced by 'isotope'
d2H (LS14FOTI01A): interpretation6_variable: '' has been replaced by 'evaporation'
d2H (LS14FOTI01A): interpretation6_variableGroup: '' has been replaced by 'EffectiveMoisture'
d2H (LS14FOTI01A): interpretation6_variableGroupDirection: '' has been replaced by 'negative'
d2H (LS14FOTI01A): interpretation6_variableGroupOriginal: '' has been replaced by 'soil water evapotranspiration'
d2H (LS14FOTI01B): interpretation2_basis: 'Results from both observational and modeling studies suggest that the dominant control on modern interannual Andean ?Dp variability is Rayleigh-type fractionation during rainout along the trajectory of moist air masses across the Amazon Basin up to the Andes (e.g., Rozanski et al., 1993; Hoffmann et al., 2003; Vimeux et al., 2005; Vuille and Werner, 2005). Increased rainout along this trajectory, as well as increased local precipitation in the Andes, results in more depleted ?Dp, consistent with the continentality and amount effects that dominate ?Dp variability throughout most of tropical South America (Vuille et al., 2003).' has been replaced by ''
d2H (LS14FOTI01B): interpretation2_direction: 'positive' has been replaced by ''
d2H (LS14FOTI01B): interpretation2_inferredMaterial: 'soil water' has been replaced by ''
d2H (LS14FOTI01B): interpretation2_rank: '1' has been replaced by ''
d2H (LS14FOTI01B): interpretation2_scope: 'isotope' has been replaced by 'climate'
d2H (LS14FOTI01B): interpretation2_seasonality: 'Dec-Feb' has been replaced by ''
d2H (LS14FOTI01B): interpretation2_seasonalityOriginal: 'SH summer' has been replaced by ''
d2H (LS14FOTI01B): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d2H (LS14FOTI01B): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d2H (LS14FOTI01B): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d2H (LS14FOTI01B): interpretation3_basis: 'Results from both observational and modeling studies suggest that the dominant control on modern interannual Andean ?Dp variability is Rayleigh-type fractionation during rainout along the trajectory of moist air masses across the Amazon Basin up to the Andes (e.g., Rozanski et al., 1993; Hoffmann et al., 2003; Vimeux et al., 2005; Vuille and Werner, 2005). Increased rainout along this trajectory, as well as increased local precipitation in the Andes, results in more depleted ?Dp, consistent with the continentality and amount effects that dominate ?Dp variability throughout most of tropical South America (Vuille et al., 2003).' has been replaced by ''
d2H (LS14FOTI01B): interpretation3_direction: 'negative' has been replaced by ''
d2H (LS14FOTI01B): interpretation3_rank: '2' has been replaced by ''
d2H (LS14FOTI01B): interpretation3_scope: 'isotope' has been replaced by 'climate'
d2H (LS14FOTI01B): interpretation3_seasonality: 'Dec-Feb' has been replaced by ''
d2H (LS14FOTI01B): interpretation3_seasonalityOriginal: 'SH summer' has been replaced by ''
d2H (LS14FOTI01B): interpretation3_variable: 'deleteMe' has been replaced by ''
d2H (LS14FOTI01B): interpretation3_variableGroup: 'continental effect' has been replaced by ''
d2H (LS14FOTI01B): interpretation4_basis: 'While the isotopic composition of precipitation appears to be the primary control on the structure of the LT ?Dwax record, it is clear that secondary effects also contribute to this signal. Most notably, the much larger range at LT (102h) than at Illimani (58h) over the past 19 kyr suggests the influence of compounding effects on LT ?Dwax, such as decreased regional precipitation, resulting in a more enriched ?Dp, and low local humidity, which would tend to further enrich plant source water by soil water evaporation and/or leaf transpiration. Since such local evapotranspiration feedbacks would be expected to act in step with ?Dp changes, this would serve to amplify the ?Dwax signal and increase its sensitivity to ?Dp variability.' has been replaced by 'Results from both observational and modeling studies suggest that the dominant control on modern interannual Andean ?Dp variability is Rayleigh-type fractionation during rainout along the trajectory of moist air masses across the Amazon Basin up to the Andes (e.g., Rozanski et al., 1993; Hoffmann et al., 2003; Vimeux et al., 2005; Vuille and Werner, 2005). Increased rainout along this trajectory, as well as increased local precipitation in the Andes, results in more depleted ?Dp, consistent with the continentality and amount effects that dominate ?Dp variability throughout most of tropical South America (Vuille et al., 2003).'
d2H (LS14FOTI01B): interpretation4_inferredMaterial: '' has been replaced by 'soil water'
d2H (LS14FOTI01B): interpretation4_rank: '3' has been replaced by '1'
d2H (LS14FOTI01B): interpretation4_variable: 'evaporation' has been replaced by 'precipitationIsotope'
d2H (LS14FOTI01B): interpretation4_variableGroup: 'EffectiveMoisture' has been replaced by 'P_isotope'
d2H (LS14FOTI01B): interpretation4_variableGroupDirection: 'negative' has been replaced by 'positive'
d2H (LS14FOTI01B): interpretation4_variableGroupOriginal: 'soil water evapotranspiration' has been replaced by ''
d2H (LS14FOTI01B): interpretation4_seasonality: '' has been replaced by 'Dec-Feb'
d2H (LS14FOTI01B): interpretation4_seasonalityOriginal: '' has been replaced by 'SH summer'
d2H (LS14FOTI01B): interpretation5_basis: '' has been replaced by 'Results from both observational and modeling studies suggest that the dominant control on modern interannual Andean ?Dp variability is Rayleigh-type fractionation during rainout along the trajectory of moist air masses across the Amazon Basin up to the Andes (e.g., Rozanski et al., 1993; Hoffmann et al., 2003; Vimeux et al., 2005; Vuille and Werner, 2005). Increased rainout along this trajectory, as well as increased local precipitation in the Andes, results in more depleted ?Dp, consistent with the continentality and amount effects that dominate ?Dp variability throughout most of tropical South America (Vuille et al., 2003).'
d2H (LS14FOTI01B): interpretation5_direction: '' has been replaced by 'negative'
d2H (LS14FOTI01B): interpretation5_rank: '' has been replaced by '2'
d2H (LS14FOTI01B): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS14FOTI01B): interpretation5_seasonality: '' has been replaced by 'Dec-Feb'
d2H (LS14FOTI01B): interpretation5_seasonalityOriginal: '' has been replaced by 'SH summer'
d2H (LS14FOTI01B): interpretation5_variable: '' has been replaced by 'deleteMe'
d2H (LS14FOTI01B): interpretation5_variableGroup: '' has been replaced by 'continental effect'
d2H (LS14FOTI01B): interpretation6_basis: '' has been replaced by 'While the isotopic composition of precipitation appears to be the primary control on the structure of the LT ?Dwax record, it is clear that secondary effects also contribute to this signal. Most notably, the much larger range at LT (102h) than at Illimani (58h) over the past 19 kyr suggests the influence of compounding effects on LT ?Dwax, such as decreased regional precipitation, resulting in a more enriched ?Dp, and low local humidity, which would tend to further enrich plant source water by soil water evaporation and/or leaf transpiration. Since such local evapotranspiration feedbacks would be expected to act in step with ?Dp changes, this would serve to amplify the ?Dwax signal and increase its sensitivity to ?Dp variability.'
d2H (LS14FOTI01B): interpretation6_direction: '' has been replaced by 'positive'
d2H (LS14FOTI01B): interpretation6_rank: '' has been replaced by '3'
d2H (LS14FOTI01B): interpretation6_scope: '' has been replaced by 'isotope'
d2H (LS14FOTI01B): interpretation6_variable: '' has been replaced by 'evaporation'
d2H (LS14FOTI01B): interpretation6_variableGroup: '' has been replaced by 'EffectiveMoisture'
d2H (LS14FOTI01B): interpretation6_variableGroupDirection: '' has been replaced by 'negative'
d2H (LS14FOTI01B): interpretation6_variableGroupOriginal: '' has been replaced by 'soil water evapotranspiration'
year (MAT24a1c7baff): interpretation1_scope: '' has been replaced by 'climate'
year (MAT24a1c7baff): interpretation2_scope: '' has been replaced by 'climate'
year (MAT24a1c7baff): interpretation3_scope: '' has been replaced by 'climate'
year (MAT24a1c7baff): interpretation4_scope: '' has been replaced by 'climate'
depth (MATa2cbe1b687): interpretation1_scope: '' has been replaced by 'climate'
depth (MATa2cbe1b687): interpretation2_scope: '' has been replaced by 'climate'
depth (MATa2cbe1b687): interpretation3_scope: '' has been replaced by 'climate'
depth (MATa2cbe1b687): interpretation4_scope: '' has been replaced by 'climate'