d18O (WEB3e43f177): interpretation3_scope: '' has been replaced by 'isotope'
d18O (WEB3e43f177): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addR9wdrLEOIoFkL3y43', with variable name 'yearEnsemble', was added to the dataset

Multi-century humidity reconstructions from the southeastern Tibetan Plateau inferred from tree-ring δ 18 O

Wernicke, J., Hochreuther, P., GrieSSinger, J., Zhu, H., Wang, L. and Braeuning, A.: Multi-century humidity reconstructions from the southeastern Tibetan Plateau inferred from tree-ring δ18O, Global and Planetary Change, 149, 26–35, doi:10.1016/j.gloplacha.2016.12.013, 2017.

tree-ring cellulose mean d18O record representing five Abies georgii trees

Cellulose d18O is strongly influenced by isotopically enriched leaf waters, which is negatively correlated with RH.

d18O (WEB640da8ea): interpretation3_scope: '' has been replaced by 'isotope'
d18O (WEB640da8ea): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addR5zETtHt2W2h3VCfB', with variable name 'yearEnsemble', was added to the dataset

tree-ring cellulose d18O representing primarily Scots pine from multiple sites in SE Sweden

This record represents a regional composite tree-ring d18O record, developed from sub-fossil and living trees from 20 sites in SE Sweden with a spatial range of 57.04-58.59°N and 14.08-16.44°E. The set of coordinates and elevation given for this record correspond to the middle of the total spatial range.

d18O (WEB45a0b5cd): interpretation3_scope: '' has been replaced by 'isotope'
d18O (WEB45a0b5cd): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addRo41od6akyMv7mENQ', with variable name 'yearEnsemble', was added to the dataset

Seasonal variability in Northern Hemisphere atmospheric circulation during the Medieval Climate Anomaly and the Little Ice Age

Edwards, T. W. D., Hammarlund, D., Newton, B. W., Sjolte, J., Linderson, H., Sturm, C., St. Amour, N. A., Bailey, J. N.-L. and Nilsson, A. L.: Seasonal variability in Northern Hemisphere atmospheric circulation during the Medieval Climate Anomaly and the Little Ice Age, Quaternary Science Reviews, 165, 102–110, doi:10.1016/j.quascirev.2017.04.018, 2017.