d18O (IC00STTY01A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (IC00STTY01A): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addRyprgVijGpFcxVgDf', with variable name 'yearEnsemble', was added to the dataset

Steig, E. J., Morse, D. L., Waddington, E. D., Stuiver, M., Grootes, P. M., Mayewski, P. A., Twickler, M. S. and Whitlow, S. I.: Wisconsinan and holocene climate history from an ice core at taylor dome, western ross embayment, antarctica, Geografiska Annaler: Series A, Physical Geography, 82(2-3), 213–235, doi:10.1111/j.0435-3676.2000.00122.x, 2000.

Finnigan Mat Delta Plus mass spectrometers

age model based on beta activity and counting of annual layers (seasonal variations of stable isotopes)

correlation to meteorological data, ("...these data provide qualitative support for the hypothesis that temperature, not the amount effect, is the dominant process controlling d18O over the Tibetan Plateau.")

Yao, T., Thompson, L. G., Mosley-Thompson, E., Zhihong, Y., Xingping, Z., and Lin, P.-N.: 1996,Climatological Significance of I´18O in North Tibetan Ice Cores, J. Geophys. Res. 101, 29531a€“29537

isotope interpretation 1 field has an error (move to isotope interpretation 2?) - BK --> TO:corrected

Yao, T., Thompson, L. G., Mosley-Thompson, E., Zhihong, Y., Xingping, Z., and Lin, P.-N.: 1996,Climatological Significance of ?18O in North Tibetan Ice Cores, J. Geophys. Res. 101, 29531?29537

d18O (IC00THDS03A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (IC00THDS03A): interpretation4_scope: '' has been replaced by 'isotope'
d18O (IC00THDS03B): interpretation3_scope: '' has been replaced by 'isotope'
d18O (IC00THDS03B): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addR6Vq2PMnnAqNBc3uF', with variable name 'yearEnsemble', was added to the dataset
Column 'addRbw75wYErTjHuisqI', with variable name 'yearEnsemble', was added to the dataset

Thompson, L. G.: A High-Resolution Millennial Record of the South Asian Monsoon from Himalayan Ice Cores, Science, 289(5486), 1916–1919, doi:10.1126/science.289.5486.1916, 2000.