d2H (LS11TICH01A): interpretation2_basis: 'Vegetation and humidity effects are negligble, "Thus, we assume in this study that dDwax represents mean annual dDP." ... "Instrumental measurements of the isotopic composition of East African precipitation are correlated with 850 hPa zonal wind speeds in the central Indian Ocean (5 Ne5 S, 60 Ee90 E), with stronger zonal wind speed resulting in more depleted precipitation (Vuille et al., 2005). Isotope-enabled modeling experiments confirm that shifts in zonal wind speed in the Indian Ocean e such as those that might occur during an IOZM event or during a strong Indian summer monsoon e result in isotopically-depleted rainfall throughout East Africa (Vuille et al., 2005)."' has been replaced by ''
d2H (LS11TICH01A): interpretation2_direction: 'positive' has been replaced by ''
d2H (LS11TICH01A): interpretation2_inferredMaterial: 'soil water' has been replaced by ''
d2H (LS11TICH01A): interpretation2_rank: '1' has been replaced by ''
d2H (LS11TICH01A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d2H (LS11TICH01A): interpretation2_seasonality: 'Annual' has been replaced by ''
d2H (LS11TICH01A): interpretation2_seasonalityOriginal: 'Annual' has been replaced by ''
d2H (LS11TICH01A): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d2H (LS11TICH01A): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d2H (LS11TICH01A): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d2H (LS11TICH01A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d2H (LS11TICH01A): interpretation4_rank: '' has been replaced by '1'
d2H (LS11TICH01A): interpretation4_basis: '' has been replaced by 'Vegetation and humidity effects are negligble, "Thus, we assume in this study that dDwax represents mean annual dDP." ... "Instrumental measurements of the isotopic composition of East African precipitation are correlated with 850 hPa zonal wind speeds in the central Indian Ocean (5 Ne5 S, 60 Ee90 E), with stronger zonal wind speed resulting in more depleted precipitation (Vuille et al., 2005). Isotope-enabled modeling experiments confirm that shifts in zonal wind speed in the Indian Ocean e such as those that might occur during an IOZM event or during a strong Indian summer monsoon e result in isotopically-depleted rainfall throughout East Africa (Vuille et al., 2005)."'
d2H (LS11TICH01A): interpretation4_direction: '' has been replaced by 'positive'
d2H (LS11TICH01A): interpretation4_inferredMaterial: '' has been replaced by 'soil water'
d2H (LS11TICH01A): interpretation4_seasonality: '' has been replaced by 'Annual'
d2H (LS11TICH01A): interpretation4_seasonalityOriginal: '' has been replaced by 'Annual'
d2H (LS11TICH01A): interpretation4_variable: '' has been replaced by 'precipitationIsotope'
d2H (LS11TICH01A): interpretation4_variableGroup: '' has been replaced by 'P_isotope'
d2H (LS11TICH01A): interpretation4_variableGroupDirection: '' has been replaced by 'positive'
d2H (LS11TICH01A): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS11TICH01A): interpretation6_scope: '' has been replaced by 'isotope'
year (MAT4d02d57c05): interpretation1_scope: '' has been replaced by 'climate'
year (MAT4d02d57c05): interpretation2_scope: '' has been replaced by 'climate'
depth (MAT707747961b): interpretation1_scope: '' has been replaced by 'climate'
depth (MAT707747961b): interpretation2_scope: '' has been replaced by 'climate'