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sea ice changes #10
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Thicker sea ice on shelf when easterlies weaken, and less ice on shelf when they strengthen. A little counterintuitive give that stronger easterlies should move more ice towards land (onshore Ekman with easterly winds). |
Yes, this isn't what I would have expected. Also the DSW formation increases in the increased easterlies perturbation, which means there should be more sea ice production in the up case. However, this is consistent (even down to the spatial pattern) with the SST change (see figure here). So maybe we need to figure out what's driving the SST change? Perhaps there's increased convection in the up case, which brings up more heat from below? |
Excellent! This is a very nice result - and reassuring to see / confirm that the fast time-scale Ekman response is there (sanity check that the wind anomaly sign was applied correctly haha) - then eventually overwhelmed by upwelling / mixing from below. Highly analogous to the John Marshall et al. argument around a two-time scale mid-latitude response in SST: i.e. the initial surface SWW-driven cooling eventually being overwhelmed by CDW upwelling. |
Maybe looking at the sea ice movement helps. I expect the ice to be more divergent near the coast in the UP case, leading to higher sea ice production rates, deeper mixed layers and thinner sea ice. |
Ok, that makes sense that there's more ice production in the UP case, even though the ice is thinner. I would guess the thickness is just following the SST response (warming in the UP case). I think we need to get to the bottom of why the SST warms in the UP case. |
Maybe where there's more ice, it's moving south and the reverse (definitely in Ross and east Weddell)? Hard to tell what's going on in East Antarctica and West Antarctica though. Maybe a longer average would help? |
Thanks, @PaulSpence , that was quick! Looking at the Ross Sea, this makes sense to me. Hard to tell what's going on with the narrower shelf regions. We might have to zoom in as for the surface momentum stress plots). |
impressive symmetry between UP and DOWN. |
Also while preparing for my seminar I made this sea ice thickness and velocity figure (very similar to Paul's previous ones, but averaged over last 5 years, and I masked the velocities where the sea ice concentration was low at the northern edge). Do you think this is good for Figure 7? I guess it would look better if we could plot transports not velocities, but I don't think we have the right diagnostics to do that properly. |
Hi Adele,
Thanks for looking into the sea ice. I am working on it as well. Trying to
regrid the data a bit to smooth the arrows.
P
…On Mon, Nov 22, 2021 at 10:55 AM Adele Morrison ***@***.***> wrote:
Also while preparing for my seminar I made this sea ice thickness and
velocity figure (very similar to Paul's previous ones, but averaged over
last 5 years, and I masked the velocities where the sea ice concentration
was low at the northern edge).
Do you think this is good for Figure 7?
[image: sea_ice_thickness_velocity]
<https://user-images.githubusercontent.com/8506963/142784059-099764ee-9412-41e0-a857-1223db0ebae4.png>
I guess it would look better if we could plot transports not velocities,
but I don't think we have the right diagnostics to do that properly.
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Yes, it would be nice if the velocities were smoother. I tried and failed at improving it using linear interpolation. |
evaluate how the sea ice responds ... link to changes in watermass transformation
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