Experimental design for the Marine Ice Sheet–Ocean Model Intercomparison Project – phase 2 (MISOMIP2)

De Rydt, Jan; Jourdain, Nicolas C.; Nakayama, Yoshihiro; van Caspel, Mathias; Timmermann, Ralph; Mathiot, Pierre; Asay-Davis, Xylar S.; Seroussi, Hélène; Dutrieux, Pierre; Galton-Fenzi, Ben; Holland, David; Reese, Ronja

doi:10.5194/gmd-17-7105-2024

Title: Experimental design for the Marine Ice Sheet–Ocean Model Intercomparison Project – phase 2 (MISOMIP2)

Journal Article · 24 September 2024 · Geoscientific Model Development (Online)

DOI: https://doi.org/10.5194/gmd-17-7105-2024 · OSTI ID:2472572

^[1];

^[2]; Nakayama, Yoshihiro ^[3]; van Caspel, Mathias ^[4]; Timmermann, Ralph ^[4]; Mathiot, Pierre ^[2];

^[5];

^[6];

^[7];

^[8]; Holland, David ^[9];

^[1]

Northumbria University, Newcastle (United Kingdom)
Univ. of Grenoble Alpes, Grenoble (France)
Hokkaido Univ., Sapporo (Japan)
Alfred Wegener Inst. for Polar and Marine Research, Bremerhaven (Germany)
Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)
Dartmouth College, Hanover, NH (United States)
British Antarctic Survey, Cambridge (United Kingdom)
Univ. of Tasmania, Hobart, TAS (Australia)
New York Univ. (NYU), NY (United States)

The Marine Ice Sheet–Ocean Model Intercomparison Project – phase 2 (MISOMIP2) is a natural progression of previous and ongoing model intercomparison exercises that have focused on the simulation of ice-sheet and ocean processes in Antarctica. The previous exercises motivate the move towards realistic configurations, as well as more diverse model parameters and resolutions. The main objective of MISOMIP2 is to investigate the performance of existing ocean and coupled ice-sheet–ocean models in a range of Antarctic environments through comparisons to observational data. We will assess the status of ice-sheet–ocean modelling as a community and identify common characteristics of models that are best able to capture observed features. As models are highly tuned based on present-day data, we will also compare their sensitivity to prescribed abrupt atmospheric perturbations leading to either very warm or slightly warmer ocean conditions compared to the present day. The approach of MISOMIP2 is to welcome contributions of models as they are, including global and regional configurations, but we request standardized variables and common grids for the outputs. We target the analysis at two specific regions, the Amundsen Sea and the Weddell Sea, since they describe two different ocean environments and have been relatively well observed compared to other areas of Antarctica. An observational “MIPkit” synthesizing existing ocean and ice-sheet observations for a common period is provided to evaluate ocean and ice-sheet models in these two regions.

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Research Organization:: Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)

Sponsoring Organization:: USDOE Office of Science (SC), Biological and Environmental Research (BER); USDOE Office of Science (SC), Advanced Scientific Computing Research (ASCR). Scientific Discovery through Advanced Computing (SciDAC); Research Councils UK; European Research Council (ERC); Agence Nationale de la Recherche

Grant/Contract Number:: 89233218CNA000001

OSTI ID:: 2472572

Report Number(s):: LA-UR--23-32175

Journal Information:: Geoscientific Model Development (Online), Journal Name: Geoscientific Model Development (Online) Journal Issue: 18 Vol. 17; ISSN 1991-9603

Publisher:: Copernicus Publications, EGUCopyright Statement

Country of Publication:: United States

Language:: English

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