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revision 1.606 by jmc, Fri Feb 10 00:33:31 2006 UTC revision 1.616 by heimbach, Thu Mar 2 02:56:54 2006 UTC
# Line 4  $Name$ Line 4  $Name$
4      Notes on tags used in MITgcmUV      Notes on tags used in MITgcmUV
5      ==============================      ==============================
6    
7    o Adding runtime parameter to exf/, ctrl/, to remove on-the-fly global mean
8      and trend from exf forcing and ctrl control adjustments
9    o fix variable aliasing in gad_calc_rhs that cannot be handled by TAF
10      (since checkpoint57x_post)
11    o change the default rotation period to 86164.s = the Earth rotation
12    o 1rst implementation of Implicit IGW using the 3-D solver (use3Dsolver=T)
13      and based on a reference stratification. Tested within hs94.cs-32x32x5.
14    o seaice advection: add code for choosing between the default (2nd order
15      central differences) and multiDim advection schemes provided by
16      pkg/generic_advdiff
17    o seaice:
18      - removed all references to SEAICE_GRID.h fields from
19        dynsolver, advect, diffus, lsr, without changing the results of lab_sea
20        (cubed-sphere configuration will change a little)
21      - grid computations in seaice_init are obsolete now.
22      - cleaned up code a little so that is easier to read (hopefully).
23      - added new (better?) discretizations of default advection and diffusion
24        (turn on with SEAICEuseFluxForm)
25      - replace 1 in 3d global fields by kSurface in growth.F
26      
27    checkpoint58a_post
28    o seaice:
29      - bug fix in advect.F
30    o shelfice:
31      - separate shelfice load anomaly from pload (breaks with time
32        dependent forcing), => introduce constant field shelficeLoadAnomaly.
33        Its default is 0., but it may be computed more cleverly from (unknown)
34        t- and s-profiles (tRef, sRef) and actual EOS. For now this has to be
35        done offline. A good approximation of the pressure load anomaly is
36        necessary to avoid large initial adjustment processes underneath
37        deep-reaching shelfice.
38      - small fix in ISOMIP shelfice_thermodynamics
39      - add more sophisticated thermodynamics of Hellmer (1989), this is
40        now the default
41      - give a few constants more intuitive names
42    o add code to balance EmPmP and Qnet at the end of do_ocean_physics. Useful
43      if bulk formulae are used in long integration (especially EmPmR). Turn
44      on with balanceEmPmR = .true. or balanceQnet = .true. in data, PARM01
45      if balancePrintMean, the imbalance that is substracted is printed to
46      STDOUT.
47  o fix bug (typo) in obcs_apply_eta.F  o fix bug (typo) in obcs_apply_eta.F
48  o add a new package shelfice which enables us to model the circulation  o add a new package shelfice which enables us to model the circulation
49    underneath shelf-ice with draughts of hundreds of meters.    underneath shelf-ice with draughts of hundreds of meters.
# Line 14  o add a new package shelfice which enabl Line 54  o add a new package shelfice which enabl
54            + can we use topoFile, Ro_surf and existing code in ini_depth.F            + can we use topoFile, Ro_surf and existing code in ini_depth.F
55              instead of new field R_shelfIce and new code in ini_depth.F              instead of new field R_shelfIce and new code in ini_depth.F
56              and ini_mask_etc.F?              and ini_mask_etc.F?
57              + adjust vertical mixing schemes?
58  o seaice pkg:  o seaice pkg:
59   - add a cpp-flag to include a simple formula for a salinity dependent   - add a cpp-flag to include a simple formula for a salinity dependent
60     freezing point of sea water at the surface     freezing point of sea water at the surface

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