Hi everyone,
After the Cryo WG meeting today I had a few questions rattling around in my mind - things like:
- Will ACCESS-OM3 have sub shelf cavities?
- If so, will it have thermodynamics (e.g. melt)?
- Could it even have dynamics?
We (Hobart Cryo people) talked a bit about these things after the meeting together. I had naively assumed OM3 wouldn’t have a cavity, so I was mentally planning for fast ice in the model configuration using the ice sheet model, which would have been super expensive.
But we grabbed @PSpence as he walked past our meeting room. He said…
- OM3 will have sub ice shelf cavities (this is part of MOM6 code)
- It will have thermodynamics (e.g., sub shelf melt) and even dynamics (e.g. grounding line retreat) - but without the fully coupled ice sheet model expense
- Cavities will be implemented in both the pan-Ant configuration (1/20th to 1/40th deg) as well as the global model (1/10th I guess?). But not in the regional configuration of OM3 (which has to be north of the ice edge anyway).
Anyway I guess the purpose of this post is to draw attention to this capability within the cryo group.
(@anton @Chen_Zhao @pat_wongpan were in the room and @dpath2o you might be interested too. Paola Papapetros was there too but I can’t find her @)
@PSpence please correct anything I’ve messed up!
Cheers, Alex.