d18O (IC06VID301A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (IC06VID301A): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addRXtE56lWDl1URFffK', with variable name 'yearEnsemble', was added to the dataset

Vinther, B. M., Clausen, H. B., Johnsen, S. J., Rasmussen, S. O., Andersen, K. K., Buchardt, S. L., Dahl-Jensen, D., Seierstad, I. K., Siggaard-Andersen, M.-L., Steffensen, J. P., Svensson, A., Olsen, J. and Heinemeier, J.: A synchronized dating of three Greenland ice cores throughout the Holocene, Journal of Geophysical Research, 111(D13), doi:10.1029/2005jd006921, 2006.

d18O (IC06VIGR01A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (IC06VIGR01A): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addRTsIdFyaFvtX8uJlA', with variable name 'yearEnsemble', was added to the dataset

d18O (IC06VING01A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (IC06VING01A): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addRebwMQiyfxhEo6UKX', with variable name 'yearEnsemble', was added to the dataset

Our previous studies[10,19] have revealed that annual mean I´ 18O in the Malan ice core mainly reflects the summer temperature (high annual mean  I´ 18O value implies warm summer while low annual mean I´ 18O value means  cold summer), and its variation can ex-press the variations of summer temperatures in the large part of the northern Tibetan Plateau.

Tian, L., V. Masson-Delmotte, M. Stievenard, T. Yao and J. Jouzel.2001. Tibetan Plateau summer monsoon northward extent revealed by measurements of water stable isotopes.J. Geophys. Res., 106(D22), 28,081?28,088.

d18O (IC06WAML01A): interpretation3_scope: '' has been replaced by 'isotope'
d18O (IC06WAML01A): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addRtOFu8OFaRl7jljNg', with variable name 'yearEnsemble', was added to the dataset

Wang, N., Yao, T., Pu, J., Zhang, Y. and Sun, W.: Climatic and environmental changes over the last millennium recorded in the Malan ice core from the northern Tibetan Plateau, Science in China Series D: Earth Sciences, 49(10), 1079–1089, doi:10.1007/s11430-006-1079-9, 2006.