Corrigendum to "Impact of CO₂ and climate on the Last Glacial Maximum vegetation: results from the ORCHIDEE/IPSL models" published in Clim. Past, 7, 557–577, 2011

Based upon coupled climate simulations subject to present-day and Last Glacial Maximum conditions, we have investigated the individual impact of including LGM

The climate sensitivity and global mean annual surface air temperature warming of each of the models with simulations in the PlioMIP Experiment 2 ensemble.. Climate sensitivity is

The probability of attending school four our group of interest in this region increased by 6.5 percentage points after the expansion of the Bolsa Família program in 2007 and

The com- bination of cooler SSTs, an enhanced subduction of AABW and the reduction in export production in experiment O-LGM dramatically increased the oxygen content in both the

(a) The simulated cumulative atmosphere–land CO 2 flux ( F e L ) from the Climate + CO 2 simulation in comparison with other terrestrial vegetation model estimates and the

Using four different climate models, we investi- gate sea level pressure variability in the extratropical North Atlantic in the preindustrial climate (1750 AD) and at the Last

Mean Annual Runoff and Continental Temperature as calculated by FOAM when using either the same vegetation type (here mixed deciduous evergreen forest) on all continental grid points

The structure of the remelting zone of the steel C90 steel be- fore conventional tempering consitute cells, dendritic cells, sur- rounded with the cementite, inside of