ACCESS-OM2 v1.0: a global ocean–sea ice model at three resolutions
-
Published:2020-02-05
Issue:2
Volume:13
Page:401-442
-
ISSN:1991-9603
-
Container-title:Geoscientific Model Development
-
language:en
-
Short-container-title:Geosci. Model Dev.
Author:
Kiss Andrew E., Hogg Andrew McC.ORCID, Hannah Nicholas, Boeira Dias FabioORCID, Brassington Gary B., Chamberlain Matthew A., Chapman ChristopherORCID, Dobrohotoff Peter, Domingues Catia M., Duran Earl R., England Matthew H., Fiedler Russell, Griffies Stephen M.ORCID, Heerdegen AidanORCID, Heil PetraORCID, Holmes Ryan M.ORCID, Klocker AndreasORCID, Marsland Simon J.ORCID, Morrison Adele K., Munroe James, Nikurashin Maxim, Oke Peter R., Pilo Gabriela S., Richet Océane, Savita Abhishek, Spence Paul, Stewart Kial D., Ward Marshall L.ORCID, Wu FanghuaORCID, Zhang Xihan
Abstract
Abstract. We introduce ACCESS-OM2, a new version of the ocean–sea ice model of the Australian Community Climate and Earth System Simulator.
ACCESS-OM2 is driven by a prescribed atmosphere (JRA55-do) but has been designed to form the ocean–sea ice component of the fully coupled (atmosphere–land–ocean–sea ice) ACCESS-CM2 model.
Importantly, the model is available at three different horizontal resolutions: a coarse resolution (nominally 1∘ horizontal grid spacing), an eddy-permitting resolution (nominally 0.25∘), and an eddy-rich resolution (0.1∘ with 75 vertical levels); the eddy-rich model is designed to be incorporated into the Bluelink operational ocean prediction and reanalysis system.
The different resolutions have been developed simultaneously, both to allow for testing at lower resolutions and to permit comparison across resolutions.
In this paper, the model is introduced and the individual components are documented.
The model performance is evaluated across the three different resolutions, highlighting the relative advantages and disadvantages of running ocean–sea ice models at higher resolution.
We find that higher resolution is an advantage in resolving flow through small straits, the structure of western boundary currents, and the abyssal overturning cell but that there is scope for improvements in sub-grid-scale parameterizations at the highest resolution.
Funder
Australian Research Council
Publisher
Copernicus GmbH
Reference162 articles.
1. Adcroft, A. and Campin, J.-M.: Rescaled height coordinates for accurate
representation of free-surface flows in ocean circulation models, Ocean
Modell., 7, 269–284, 2004. a 2. Adcroft, A., Hill, C., and Marshall, J.: Representation of topography by shaved
cells in a height coordinate ocean model, Mon. Weather Rev., 125,
2293–2315, 1997. a, b 3. Annamalai, H., Liu, P., and Xie, S. P.: Southwest Indian Ocean SST
variability: Its local effect and remote influence on Asian monsoons,
J. Climate, 18, 4150–4167, https://doi.org/10.1175/JCLI3533.1, 2005. a 4. Ansorge, I. J., Froneman, P. W., and Durgadoo, J. V.: The Marine Ecosystem of
the Sub-Antarctic, Prince Edward Islands, in: Marine Ecosystems, edited by:
Cruzado, A., chap. 3, IntechOpen, Rijeka, https://doi.org/10.5772/36676, 2012. a 5. Bamber, J., van den Broeke, M., Ettema, J., Lenaerts, J., and Rignot, E.:
Recent large increases in freshwater fluxes from Greenland into the North
Atlantic, Geophys. Res. Lett., 39, L19501,
https://doi.org/10.1029/2012gl052552, 2012. a
Cited by
117 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|