Abstract Resolving discrepancies in long-term Holocene temperature trends between climate models and proxy records is essential to improve future climate projections. However. uncertainties in paleoclimate reconstructions limit their ability to constrain models. This study compares ice core-derived oxygen isotope records with isotope-enabled climate simulations to evaluate model perfo... https://parisnaturalfoodes.shop/product-category/all-natural-waxed-paper/