Hi all,
Apologies if this was obvious to everyone, but I just realised that the ht
variable in ACCESS-OM2-01 is different to the actual bottom st_ocean
cell where data is not NaN (for instance, temperature). See below for the difference between the two, which can be up to 40m in places in my region of the Ross Sea.
I know people define isobaths using the ht
variable, but wouldn’t it be better to do so using the coarser bottom st_ocean
cell where data is actually available for analysis? Masking would also yield slightly different results if we use bounds defined by ht
vs. the actual data depth. Same applies for hu
…
.