Calculating MLD off-line is straight forward and relatively inexpensive, but it does require you to download all the 3z levels of T and S. This is how we do it:
foreach f ( ${R}_${year}${mon}??12_M0000_t3z.nc )
setenv A `echo $f | sed -e "s/_
t3z.nc//g"`
#
if (-f ${A}_
t3z.nc && \
-f ${A}_
s3z.nc && \
-f ${A}_
u3z.nc && \
-f ${A}_
v3z.nc ) then
if (! -f ${A}_
bot.nc) then
setenv CDF_INST "COAPS/FSU"
setenv CDF_PUBLIC "yes"
setenv CDF_HIST "espc_bottom"
setenv CDF_TAU 0
setenv CDF001 ${A}_
bot.nc /bin/rm -f $CDF001
${HT}/archive/src/espc_bottom <<E-o-D
${TT}/depth_${R}_${T}.nc
${A}_
t3z.nc${A}_
s3z.nc${A}_
u3z.nc${A}_
v3z.nc 0 'itest ' = grid point where detailed diagnostics are desired
0 'jtest ' = grid point where detailed diagnostics are desired
031 'iexpt ' = experiment number x10
0.3 'tmljmq' = equiv. temp. jump across mixed-layer (degC, 0 no I/O)
E-o-D
date
# created ${A}_
bot.nc
This is also calculating the velocity 2-D fields.
The Navy is unlikely to add MLD to its output unless one of its operational customers asks for it.
The following is from Joe Metzger on the next version:
We have plans to do a VTR for ESPC-D v2.1 by 1st or 2nd
quarter of FY26. It will use HYCOM v2.3.01 and include a) rivers as a
mass flux, b) a new rivers database developed by Cheryl Ann, c) include
parameterized Stokes drift mixing (since we still only have one-way
coupling to WW3), d) include SWOT altimeter assimilation utilizing
adaptive scales that are defined by the resolution of the observations,
i.e., take advantage of the finer space scales resolved by the
wide-swath altimeter, e) include landfast sea ice in both hemispheres,
and e) sea ice thickness assimilation. I’ve probably forgotten something
but that is the main list of improvements on the ocean/sea ice side.
This is a substantial upgrade that should produce a measurable improvement.
A Validation Testing Report that demonstrates improvements over existing capabilities is the last step before entering OPTEST (i.e. before it runs every day in the operational queues), but the amount of time a product stays in OPTEST before becoming fully operational varies a lot. We might be able to distribute the OPTEST in parallel with ESPC-D v2. FY26Q2 ends March 31st, so at best this might be available a year from now.
The strange eddies were an NCODA issue that has been fixed.
It is taking a while to spin down, but attached are two pictures. One
is just after we started applying the correction and the other is after
it’s been implemented a while. The checkerboard pattern is slightly
visible in the more recent plot, but for less egregious.
Let me know if you think this is still an issue.
Alan.