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published-comment-tracker.pdf

Level used in SROCC), as he sees it as a first step towards comprising the forcing uncertainty in Change sea-level estimates. The limitations should be more fully discussed. In addition the authors seem to favour the no-delay numbers, if these limitations are p;oestimates for deConto&Pollard 2016

published-comment-tracker-local-2.2km.pdf

/10.1007/s00382-017- 3885-5 Scientific/technical issue 90 1.3 Motivation for new 2.2km projections 14 1-8 You might want to mention the intercomparison of the two European-scale simulations available (i.e. Berthou et al. 2018: Pan-European climate at convection-permitting scale: a model

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