"The predictive power of ice sheet models and the regional sensitivity of ice loss to basal sliding parameterisations: A case study of Pine Island and Thwaites Glaciers, West Antarctica" - Interactive discussionhttps://tc.copernicus.org/preprints/tc-2022-109/2022-09-05T14:55:33+02:00Copernicus Publicationshttps://tc.copernicus.org/preprints/tc-2022-109/tc-2022-109-AC2.pdfAC2: 'Response to reviewers', Jowan Barnes, 05 Sep 2022AC2: 'Response to reviewers', Jowan Barnes, 05 Sep 2022Jowan Barnes2022-09-05T14:55:32+02:002022-09-05T14:55:32+02:00https://tc.copernicus.org/preprints/tc-2022-109/tc-2022-109-AC1.pdfAC1: 'Response to reviewers', Jowan Barnes, 05 Sep 2022AC1: 'Response to reviewers', Jowan Barnes, 05 Sep 2022Jowan Barnes2022-09-05T14:54:38+02:002022-09-05T14:54:38+02:00https://tc.copernicus.org/preprints/tc-2022-109/tc-2022-109-RC2.pdfRC2: 'Comment on tc-2022-109', Douglas Brinkerhoff, 13 Jul 2022RC2: 'Comment on tc-2022-109', Douglas Brinkerhoff, 13 Jul 2022Douglas Brinkerhoff2022-07-13T17:44:22+02:002022-07-13T17:44:22+02:00https://tc.copernicus.org/preprints/tc-2022-109/tc-2022-109-RC1.pdfRC1: 'Comment on tc-2022-109', Anonymous Referee #1, 13 Jul 2022RC1: 'Comment on tc-2022-109', Anonymous Referee #1, 13 Jul 2022Anonymous Referee #12022-07-13T15:37:13+02:002022-07-13T15:37:13+02:00