Significant Correlation with maximum June July Aaugust air temperature (r=0.54; p<0.001)

d18O (TR15NACA00): interpretation3_scope: '' has been replaced by 'isotope'
d18O (TR15NACA00): interpretation4_scope: '' has been replaced by 'isotope'

Column 'addRBCE45LR1X8m3GvQo', with variable name 'yearEnsemble', was added to the dataset

Naulier, M., Savard, M. M., Begin, C., Gennaretti, F., Arseneault, D., Marion, J., Nicault, A. and Begin, Y.: A millennial summer temperature reconstruction for northeastern Canada using oxygen isotopes in subfossil trees, Climate of the Past, 11(9), 1153–1164, doi:10.5194/cp-11-1153-2015, 2015.

TP: added elevations; OCh-S: replaced soil water to soil, precipitation water; Changed Pub_1 DOI

Significant Correlation with summer months of the England Wales Precipiation series (r = -0.58, n = 161, p < 0.001)

Each of the individual I´18O series has a significant negative correlation (p < 0.001) with the summer (Junea€“August) EWP

d18O (TR15YOLL00): interpretation3_scope: '' has been replaced by 'isotope'
d18O (TR15YOLL00): interpretation4_scope: '' has been replaced by 'isotope'

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

Young, G.H.F., Loader, N.j., McCarroll, D., Bale, R.J., Demmler, J.C., Miles, D., Nayling, N.T., Rinne, K. T., Robertson, I., Watts, C., Whitney, M.

Young, G. H. F., Loader, N. J., McCarroll, D., Bale, R. J., Demmler, J. C., Miles, D., Nayling, N. T., Rinne, K. T., Robertson, I., Watts, C. and Whitney, M.: Oxygen stable isotope ratios from British oak tree-rings provide a strong and consistent record of past changes in summer rainfall, Climate Dynamics, 45(11-12), 3609–3622, doi:10.1007/s00382-015-2559-4, 2015.

TP: added elevations; OCh_S: replaced soil water to soil, precipitation water

Significant Correlation with summer months of the England Wales Precipiation series (r= -0.39, n = 163, p<0.001)

Each of the individual I´18O series has a significant negative correlation (p < 0.001) with the summer (Junea€“August) P_E