[MITgcm-devel] depressed Eta and sIceLoad
Martin Losch
mlosch at awi-bremerhaven.de
Mon Oct 23 04:26:09 EDT 2006
Hi Jean-Michel,
unfortunately I cannot say when, but at sometime the sIceLoad fields
started to cause problems in the height field Eta. With useSeaice
= .true., useRealFreshWaterFlux=.true., exactConserv=.true., and
LINEAR free surface (#undef NONLIN_FRSURF) I get local depressions of
ETA underneath seaice along the coast of -40m and more in 100years.
They go away, when I set useRealFreshWaterFlux = .false. I need to
mention, that I have a global EmPmR imbalance of approximately 10cm
per year, so that my mean Eta is approximately -11m after 100years,
but that wasn't a problem earlier. I attach a figure which shows Eta
and surface velocities averaged over the years 91 to 100 of a 100
year integration. What I find strange is that the strong depression
in Eta does not have any corresponding signal in the surface
velocities. T/S do not have any striking anomalies in these regions
around Antartica, either, that could compensate Eta-gradients of more
10m per 100km. The model does not explode, the mean effective ice
thickness is way below 2m in the areas of Eta-depression.
Do you have any idea what's going on?
Martin
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