You can download the latest draft of the COSIMA Workshop Program (updated 3rd May). The program includes instructions for uploading your talk, guidelines on how to contribute to our discussion and some preparatory homework for anyone attending the COSIMA Cookbook Tutorial.
Over the last few months, COSIMA folks have been working hard on releasing our ACCESS-OM2 suite of models. The current status is that we have now completed a 500 year spinup for 3 different cases using the JRA55-do (Tsujino et al., 2017, personal communication) forcing dataset. Some preliminary results can be seen in the figures below. We are also spinning up a CORE-NYF comparison case. For a more complete analysis have a look in the COSIMA Cookbook.
Plans in the coming weeks are to finalise spinups of our 0.25° case (ACCESS-OM2-025), and to begin running our flagship 0.1° simulation, ACCESS-OM2-01.
The COSIMA consortium is partly supported by an ARC Linkage Project. This project is now active, following sign-off from all partners in December 2016. The management committee for the project formally met for the first time on Friday 9th December. Following are abbreviated minutes from the meeting which outline our plans for 2017:
To advertise for a Postdoctoral/Research Fellow to coordinate COSIMA projects.
To enhance the vertical resolution of existing MOM5-SIS 0.1° model, with no change in horizontal resolution;
To enhance model bathymetry in coastal regions to take advantage of reduced minimum depth stemming from vertical resolution changes;
To couple MOM5 with CICE at 0.1° using OASIS3-MCT (we have a contract with Nic Hannah from Double Precision to perform this work);
To evaluate, refine, optimise and document the new model configuration.
Furthermore, we have confirmed that the 2017 COSIMA meeting will be in Sydney on May 25-26.
The first meeting of the Consortium for Ocean Sea Ice Modelling in Australia (COSIMA) was held in Hobart on the 26-27 May 2016. There we 38 attendees (20 of whom gave presentations), representing 10 different institutions. A full participant list is included at the end of this report.
The goal of the workshop was to formalise a consortium across universities, BoM, AAD and CSIRO to build global model configurations that will form the basis for high-resolution forecasting, reanalysis, process modelling and ultimately coupled climate modelling. The consortium recently received 4 years of funding from an ARC Linkage Project to build a model configuration which underpins a variety of applications.
Presentations included an update on the current status and near-term plans of the major modelling groups, recent scientific advances using ocean and sea ice models and highlights of technical advances in model development. Some edited highlights are listed below:
Uptake of the MOM5 model for global applications has progressed well in the last 5 years (Bi). It is currently used broadly across climate and ocean-only configurations at both 1° (O’Kane) and 0.25° resolution (Spence, Holmes). Developments at 0.1° are proceeding (Zhang, Langlais, Matear, Chamberlain, Hogg).
Other models with a strong user base in Australia include ROMS (Galton Fenzi) for near-coastal and near-Antarctic applications, MITgcm for regional GFD-style simulations (Nikurashin) and NEMO (Alves) for seasonal prediction.
There is a strong need to consider vertical resolution in future high resolution model developments (Stewart).
The CICE sea ice model, while no longer under active development at LANL, continues to be the ice model of choice (due primarily to its superior ice physics over SIS 1; Heil, Reid, Bennetts). It is likely that it will remain the model of choice with applications using MOM5.
Our MOM-CICE implementations using OASIS3-MCT coupling, but it is not clear that this solution will scale to 0.1° and beyond (Hannah)
MOM6 is rapidly developing, and is beginning to gather users within Australia. It looks viable to use MOM6 for global models in the next year or two (Griffies, Gibson).
MOM6, being a C-grid model, presents some challenges when working with a B-grid ice model such as CICE. For the time being, it seems that the best ice model to use with MOM6 will be SIS2, which is actively being developed at GFDL to incorporate the vertical physics (Griffies).
Computational performance of these models shows that MOM5 is marginally faster than MOM6 (once accounting for vertical resolution differences) and that both models scale well on Raijin. NEMO is faster at small core counts but scales poorly (Ward).
Forced ocean-sea ice models should be transferring to the JRA-55 forcing set when possible (Marsland).
The COSIMA Community
There was significant support for the formation of a community of ocean-sea ice modellers around the COSIMA banner:
Need to create a website to outline COSIMA activities and developments. [We are in the process of acquiring the domain name cosima.org.au, and ANU will fund hosting and a web development team to put together a skeleton site.]
We will formalise a code of ethics for COSIMA users to abide by, based on the DRAKKAR agreement. [Spence]
We aim to register members on the website, and create a mailing list
We will need to formalise the use of technologies to share code configurations, analysis tools and data. It may be possible to have a data project code on NCI to help with this.
We will release flagship configurations that are broadly supported by the community. The goal is to make the naming conventions consistent with the ACCESS community where possible, and to overlap with ACCESS developments where possible.
COSIMA will hold an annual meeting in the last week of May, for two days. Venue will rotate around the partner institutions. The focus of the meeting will be on science applications of ocean models, but will also include a technical component.
We will aim to have more regular communications, including newsletters and video meetings.
We will establish working groups within the community, along with a working group chair. Proposed groups include
Sea Ice Modelling [Heil]
Linkage Project [Hogg]
The major gap in the community was identified to be sea ice modelling and forecasting. We will all look for opportunities to attract visitors and expertise in this space.
One of the workshop goals was to receive advice from the community regarding the ARC Linkage Project designed to support COSIMA development activities. Major items of discussion were:
There was general agreement that the Linkage Project should fund both the development and evaluation of new model configurations. This point implies that we should equally fund the technical and postdoctoral position, despite the partial funding of the program.
In the first year we will look to upgrade current MOM5 implementations, focussing on the vertical grid and the incorporation of CICE.
In subsequent years we will look to adopt a MOM6 configuration.
As configurations develop and have been properly evaluated, they will be distributed to the community.
Suggestions on evaluation include using ESMVal.
(Where available, talk files are linked from the presenter’s name.)
This detailed animation of the movement of the densest and coldest water in the world around Antarctica has been produced using data generated on Australia’s most powerful supercomputer, Raijin.
So much data was used, that it took seven hours to process just one second of the animation.
The visualization has revealed underwater ocean storms generated by eddies, waterfalls of cold dense water that plummet two kilometres off the Antarctic Continental Shelf into the abyss and underwater waves hundreds of metres high.
This latest animation peels back much of the surface layer of the ocean to explore how the cold dense water produced on the Antarctic continental shelf spreads out into every ocean basin in the world.
The movement of this dense water is vital. It is the most oxygenated water in the ocean and its extreme density and coldness drive many of the significant currents in the major ocean basins connected to the Southern Ocean.
The distinctly different densities of water that move around Antarctica also make it important in regards to climate change. Because the most dense water forms near the surface of Antarctica before descending to the ocean floor, any warming that occurs near the surface can be drawn down into the deep ocean.
Importantly, this drives more heat and more carbon into the deep ocean that would otherwise have returned to the atmosphere.