C. Cerege,

W. Acevedo, Dyn, vol.46, pp.1909-1920, 2016.

E. Boucher, biogeosciences, vol.11, pp.2014-3245, 2014.

K. Briffa and T. Melvin, Dendroclimatology, vol.5, pp.1-30, 2011.

. Briffa-kr, J clim, vol.5, pp.735-753, 1992.

, Tellus A, vol.58, pp.227-235, 2006.

L. Christiansen-b and . Fc, rev Geophys, vol.55, pp.40-96, 2016.

. Cook-er and L. A. Kairiukstis, Methods of dendrochronology. Applications in the environmental sciences, p.393, 1990.

. D'arrigo-r, Glob Planet change, vol.60, pp.289-305, 2008.

F. Hc, J Appl Meteorol, vol.10, pp.845-864, 1971.

J. Guiot, PLoS One, vol.5, p.9972, 2010.

M. K. Hughes, , vol.18, pp.87-89, 2010.

D. Mccarroll and N. J. Loader, Quat Sci rev, vol.23, pp.771-801, 2004.

A. Moberg, Nature, vol.433, pp.613-617, 2005.

M. Saurer, Tellus Ser b, vol.49, pp.80-92, 1997.

T. Se, Dyn, vol.44, pp.791-806, 2014.

, obtained from the inversion of the multiproxy biophysical model MAIDENiso (boucher et al. 2014), i.e. the MAIDEN model with an isotope simulation module. red curves are obtained when the inversion is forced by cO 2 fixed at preindustrial levels (280 ppmv) and black curves are obtained from increasing values of cO 2 from 280 ppmv in 1850, Summer temperature and precipitation reconstructions at, vol.2, 2014.