d18O (LS02BEPY): interpretation2_basis: 'There are two principal sources of d18Oin to Pyramid Lake: Sierran snowmelt and Lake Tahoe overflow.Evaporation from Lake Tahoe has resulted in a d18O value (5.6m) much larger than that of snowmelt (14.6m). Thus, during droughts when Lake Fig. 19. Plot of TOC, d13C and d18O data from PLB98-2 (solid lines) and the top of PLC97-1 (dashed lines) indicating overlap of cores. 670 L. Benson et al. / Quaternary Science Reviews 21 (2002) 659?682 Tahoe ceases spilling, the d18O value of Truckee River discharge decreases from B11m to B14.6m. Th e input of 14.6m water to Pyramid lake causes its d18O value to first increase as its volume decreases; however, its steady-state value (1.6m) is much smaller than when the lake receives spill from Lake Tahoe.' has been replaced by ''
d18O (LS02BEPY): interpretation2_direction: 'negative' has been replaced by ''
d18O (LS02BEPY): interpretation2_inferredMaterial: 'lake water' has been replaced by ''
d18O (LS02BEPY): interpretation2_integrationTimeUnits: 'years' has been replaced by ''
d18O (LS02BEPY): interpretation2_rank: '1' has been replaced by ''
d18O (LS02BEPY): interpretation2_scope: 'isotope' has been replaced by 'climate'
d18O (LS02BEPY): interpretation2_variable: 'effectivePrecipitation' has been replaced by ''
d18O (LS02BEPY): interpretation2_variableGroup: 'EffectiveMoisture' has been replaced by ''
d18O (LS02BEPY): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d18O (LS02BEPY): interpretation2_variableGroupOriginal: 'P_E' has been replaced by ''
d18O (LS02BEPY): interpretation3_scope: 'isotope' has been replaced by 'climate'
d18O (LS02BEPY): interpretation4_rank: '' has been replaced by '1'
d18O (LS02BEPY): interpretation4_basis: '' has been replaced by 'There are two principal sources of d18Oin to Pyramid Lake: Sierran snowmelt and Lake Tahoe overflow.Evaporation from Lake Tahoe has resulted in a d18O value (5.6m) much larger than that of snowmelt (14.6m). Thus, during droughts when Lake Fig. 19. Plot of TOC, d13C and d18O data from PLB98-2 (solid lines) and the top of PLC97-1 (dashed lines) indicating overlap of cores. 670 L. Benson et al. / Quaternary Science Reviews 21 (2002) 659?682 Tahoe ceases spilling, the d18O value of Truckee River discharge decreases from B11m to B14.6m. Th e input of 14.6m water to Pyramid lake causes its d18O value to first increase as its volume decreases; however, its steady-state value (1.6m) is much smaller than when the lake receives spill from Lake Tahoe.'
d18O (LS02BEPY): interpretation4_direction: '' has been replaced by 'negative'
d18O (LS02BEPY): interpretation4_inferredMaterial: '' has been replaced by 'lake water'
d18O (LS02BEPY): interpretation4_integrationTimeUnits: '' has been replaced by 'years'
d18O (LS02BEPY): interpretation4_variable: '' has been replaced by 'effectivePrecipitation'
d18O (LS02BEPY): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d18O (LS02BEPY): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d18O (LS02BEPY): interpretation4_variableGroupOriginal: '' has been replaced by 'P_E'
d18O (LS02BEPY): interpretation5_scope: '' has been replaced by 'isotope'
d18O (LS02BEPY): interpretation6_scope: '' has been replaced by 'isotope'
year (MATe843de3f7d): interpretation1_scope: '' has been replaced by 'climate'
year (MATe843de3f7d): interpretation2_scope: '' has been replaced by 'climate'
depth (MATff68a2142b): interpretation1_scope: '' has been replaced by 'climate'
depth (MATff68a2142b): interpretation2_scope: '' has been replaced by 'climate'