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Notes on CICE5 in ESM1.6
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| ## CICE5 | ||
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| In ACCESS-ESM1.6, the sea ice component is CICE5 [@hunke2015cice] updated from CICE4 used in ACCESS-ESM1.5. | ||
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| Scientifically the sea ice model is configured the same as ESM1.5 [@Ziehn2020]. The scientific configuration is summarised as follows: | ||
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| - Zero-layer thermodynamics (Semtner 1976) | ||
| - One layer of snow and one layer of ice | ||
| - UM calculates ice surface temperature, and conductive heat flux into the sea-ice | ||
| - Ice transport - Lipscomb (2001) and ridging – Rothrock (1975) | ||
| - Internal Ice Stress follow EVP (Hunke and Dukowicz, 2002) | ||
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| There are significant improvements to diagnostics to support CMIP style diagnostics [@notz_cmip6_2016][@egusphere-2025-3083] natively and error handling. | ||
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| ## Meltwater Runoff | ||
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| Like ESM1.5, the OASIS3-MCT coupler is used and the sea ice model acts as the interface between the atmosphere and ocean models. The only significant change to this interface since ESM1.5 is changes to meltwater from Antarctica and Greenland. As there is no ice sheet model, the volume of meltwater discharge from Antarctica and Greenland is equal to the instantaneous precipitation over each continent. In ESM1.6, this is partially discharged at the coastline of each continent (to represent ice shelf basal melt) and partially spread in open ocean (to represent melt from icebergs). In ESM1.5 all meltwater is at the coastlines. In addition, the latent heat to melt this water is now taken from the ocean. Meltwater runoff is configured in the `input_ice.nml` [namelist](https://github.com/ACCESS-NRI/access-esm1.6-configs/blob/dev-preindustrial%2Bconcentrations/ice/input_ice.nml#L14-L25) with a prescribed pattern from the [ice discharge](https://github.com/ACCESS-NRI/access-esm1.6-configs/blob/13cc7d229b0d4bda193879b8b30cde3441d61bec/config.yaml#L98) input file. | ||
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| ## References | ||
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| \bibliography | ||
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| @Article{egusphere-2025-3083, | ||
| AUTHOR = {Fox-Kemper, B. and DeRepentigny, P. and Treguier, A. M. and Stepanek, C. and O'Rourke, E. and Mackallah, C. and Meucci, A. and Aksenov, Y. and Durack, P. J. and Feldl, N. and Hernaman, V. and Heuz\'e, C. and Iovino, D. and Madan, G. and Marquez, A. L. and Massonnet, F. and Mecking, J. and Samanta, D. and Taylor, P. C. and Tseng, W.-L. and Vancoppenolle, M.}, | ||
| TITLE = {CMIP7 Data Request: Ocean and Sea Ice Priorities and Opportunities}, | ||
| JOURNAL = {EGUsphere}, | ||
| VOLUME = {2025}, | ||
| YEAR = {2025}, | ||
| PAGES = {1--58}, | ||
| URL = {https://egusphere.copernicus.org/preprints/2025/egusphere-2025-3083/}, | ||
| DOI = {10.5194/egusphere-2025-3083} | ||
| } | ||
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| @techreport{hunke2015cice, | ||
| title={CICE: The Los Alamos Sea Ice Model documentation and software user’s manual, version 5.1. Doc}, | ||
| author={Hunke, EC and Lipscomb, WH and Turner, AK and Jeffery, N and Elliott, S}, | ||
| year={2015}, | ||
| institution={LA-CC-06-012} | ||
| } | ||
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| @article{notz_cmip6_2016, | ||
| title = {The {CMIP6} {Sea}-{Ice} {Model} {Intercomparison} {Project} ({SIMIP}): understanding sea ice through climate-model simulations}, | ||
| volume = {9}, | ||
| copyright = {https://creativecommons.org/licenses/by/3.0/}, | ||
| issn = {1991-9603}, | ||
| shorttitle = {The {CMIP6} {Sea}-{Ice} {Model} {Intercomparison} {Project} ({SIMIP})}, | ||
| url = {https://gmd.copernicus.org/articles/9/3427/2016/}, | ||
| doi = {10.5194/gmd-9-3427-2016}, | ||
| abstract = {Abstract. A better understanding of the role of sea ice for the changing climate of our planet is the central aim of the diagnostic Coupled Model Intercomparison Project 6 (CMIP6)-endorsed Sea-Ice Model Intercomparison Project (SIMIP). To reach this aim, SIMIP requests sea-ice-related variables from climate-model simulations that allow for a better understanding and, ultimately, improvement of biases and errors in sea-ice simulations with large-scale climate models. This then allows us to better understand to what degree CMIP6 model simulations relate to reality, thus improving our confidence in answering sea-ice-related questions based on these simulations. Furthermore, the SIMIP protocol provides a standard for sea-ice model output that will streamline and hence simplify the analysis of the simulated sea-ice evolution in research projects independent of CMIP. To reach its aims, SIMIP provides a structured list of model output that allows for an examination of the three main budgets that govern the evolution of sea ice, namely the heat budget, the momentum budget, and the mass budget. In this contribution, we explain the aims of SIMIP in more detail and outline how its design allows us to answer some of the most pressing questions that sea ice still poses to the international climate-research community.}, | ||
| language = {en}, | ||
| number = {9}, | ||
| urldate = {2024-04-30}, | ||
| journal = {Geoscientific Model Development}, | ||
| author = {Notz, Dirk and Jahn, Alexandra and Holland, Marika and Hunke, Elizabeth and Massonnet, François and Stroeve, Julienne and Tremblay, Bruno and Vancoppenolle, Martin}, | ||
| month = sep, | ||
| year = {2016}, | ||
| pages = {3427--3446}, | ||
| file = {Notz et al. - 2016 - The CMIP6 Sea-Ice Model Intercomparison Project (S.pdf:/Users/ajs/Zotero/storage/8RIWRH4M/Notz et al. - 2016 - The CMIP6 Sea-Ice Model Intercomparison Project (S.pdf:application/pdf}, | ||
| } | ||
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| @ARTICLE{Ziehn2020, | ||
| title = "The {Australian Earth System Model}: {ACCESS-ESM1.5}", | ||
| author = "Ziehn, Tilo and Chamberlain, Matthew A and Law, Rachel M and | ||
| Lenton, Andrew and Bodman, Roger W and Dix, Martin and Stevens, | ||
| Lauren and Wang, Ying-Ping and Srbinovsky, Jhan", | ||
| abstract = "The Australian Community Climate and Earth System Simulator | ||
| (ACCESS) has been extended to include land and ocean carbon cycle | ||
| components to form an Earth System Model (ESM). The current | ||
| version, ACCESS-ESM1.5, has been mainly developed to enable | ||
| Australia to participate in the Coupled Model Intercomparison | ||
| Project Phase 6 (CMIP6) with an ESM version. Here we describe the | ||
| model components and changes to the previous version, | ||
| ACCESS-ESM1. We use the 500-year pre-industrial control run to | ||
| highlight the stability of the physical climate and the carbon | ||
| cycle. The long spin-up, negligible drift in temperature and | ||
| small pre-industrial net carbon fluxes (0.02 and 0.08 PgC year−1 | ||
| for land and ocean respectively) highlight the suitability of | ||
| ACCESS-ESM1.5 to explore modes of variability in the climate | ||
| system and coupling to the carbon cycle. The physical climate and | ||
| carbon cycle for the present day have been evaluated using the | ||
| CMIP6 historical simulation by comparing against observations and | ||
| ACCESS-ESM1. Although there is generally little change in the | ||
| climate simulation from the earlier model, many aspects of the | ||
| carbon simulation are improved. An assessment of the climate | ||
| response to CO2 forcing indicates that ACCESS-ESM1.5 has an | ||
| equilibrium climate sensitivity of 3.87°C.", | ||
| journal = "Journal of Southern Hemisphere Earth Systems Science", | ||
| volume = 70, | ||
| number = 1, | ||
| pages = "193--214", | ||
| year = 2020, | ||
| keywords = "Keywords: ACCESS, biogeochemistry, CABLE, carbon cycle, climate | ||
| modelling, CMIP6, earth system modelling", | ||
| DOI = {10.1071/ES19035} | ||
| } |
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