9. Packages II - Diagnostics and I/O

MITgcm includes several packages related to input and output during a model integration. The packages described in this chapter are related to the choice of input/output fields and their on-disk format.

9.1. pkg/diagnostics – A Flexible Infrastructure

9.1.1. Introduction

This section of the documentation describes the diagnostics package (pkg/diagnostics) available within MITgcm. A large selection of model diagnostics is available for output. In addition to the diagnostic quantities pre-defined within MITgcm, there exists the option, in any code setup, to define a new diagnostic quantity and include it as part of the diagnostic output with the addition of a single subroutine call in the routine where the field is computed. As a matter of philosophy, no diagnostic is enabled as default, thus each user must specify the exact diagnostic information required for an experiment. This is accomplished by enabling the specific diagnostics of interest from the list of available diagnostics. Additional diagnostic quantities, defined within different MITgcm packages, are available and are listed in the diagnostic list subsection of the manual section associated with each relevant package. Instructions for enabling diagnostic output and defining new diagnostic quantities are found in Section 9.1.4 of this document.

Once a diagnostic is enabled, MITgcm will continually increment an array specifically allocated for that diagnostic whenever the appropriate quantity is computed. A counter is defined which records how many times each diagnostic quantity has been incremented. Several special diagnostics are included in the list of available diagnostics. Quantities referred to as “counter diagnostics” are defined for selected diagnostics which record the frequency at which a diagnostic is incremented separately for each model grid location. Quantities referred to as “user diagnostics” are included to facilitate defining new diagnostics for a particular experiment.

9.1.2. Equations

Not relevant.

9.1.3. Key Subroutines and Parameters

There are several utilities within MITgcm available to users to enable, disable, clear, write and retrieve model diagnostics, and may be called from any routine. The available utilities and the CALL sequences are listed below.

diagnostics_addtolist.F: This routine is the underlying interface routine for defining a new permanent diagnostic in the main model or in a package. The calling sequence is:

O     diagNum,
I     diagName, diagCode, diagUnits, diagTitle, diagMate,
I     myThid )

  diagNum   = diagnostic Id number - Output from routine
  diagName  = name of diagnostic to declare
  diagCode  = parser code for this diagnostic
  diagUnits = field units for this diagnostic
  diagTitle = field description for this diagnostic
  diagMate  = diagnostic mate number
  myThid    = my Thread Id number

diagnostics_fill.F: This is the main user interface routine to the diagnostics package. This routine will increment the specified diagnostic quantity with a field sent through the argument list.

  I             inpFld, diagName,
  I             kLev, nLevs, bibjFlg, bi, bj, myThid )

   inpFld   = Field to increment diagnostics array
   diagName = diagnostic identificator name (8 characters long)
   kLev     = Integer flag for vertical levels:
              > 0 (any integer): WHICH single level to increment in qdiag.
              0,-1 to increment "nLevs" levels in qdiag,
              0 : fill-in in the same order as the input array
              -1: fill-in in reverse order.
   nLevs    = indicates Number of levels of the input field array
              (whether to fill-in all the levels (kLev<1) or just one (kLev>0))
   bibjFlg  = Integer flag to indicate instructions for bi bj loop
            = 0 indicates that the bi-bj loop must be done here
            = 1 indicates that the bi-bj loop is done OUTSIDE
            = 2 indicates that the bi-bj loop is done OUTSIDE
                 AND that we have been sent a local array (with overlap regions)
                 (local array here means that it has no bi-bj dimensions)
            = 3 indicates that the bi-bj loop is done OUTSIDE
                 AND that we have been sent a local array
                 AND that the array has no overlap region (interior only)
              NOTE - bibjFlg can be NEGATIVE to indicate not to increment counter
   bi       = X-direction tile number - used for bibjFlg=1-3
   bj       = Y-direction tile number - used for bibjFlg=1-3
   myThid   =  my thread Id number

diagnostics_scale_fill.F: This is a possible alternative routine to diagnostics_fill.F which performs the same functions and has an additional option to scale the field before filling or raise the field to a power before filling.

  I             inpFld, scaleFact, power, diagName,
  I             kLev, nLevs, bibjFlg, bi, bj, myThid )

where all the arguments are the same as for DIAGNOSTICS_FILL with
the addition of:
   scaleFact   = Scaling factor to apply to the input field product
   power       = Integer power to which to raise the input field (after scaling)

diagnostics_fract_fill.F: This is a specific alternative routine to diagnostics_scale_fill.F for the case of a diagnostics which is associated to a fraction-weight factor (referred to as the diagnostics “counter-mate”). This fraction-weight field is expected to vary during the simulation and is provided as argument to diagnostics_fract_fill.F in order to perform fraction-weighted time-average diagnostics. Note that the fraction-weight field has to correspond to the diagnostics counter-mate which has to be filled independently with a call to diagnostics_fill.F.

  I             inpFld, fractFld, scaleFact, power, diagName,
  I             kLev, nLevs, bibjFlg, bi, bj, myThid )

where all the arguments are the same as for DIAGNOSTICS_SCALE_FILL with
the addition of:
   fractFld    = fraction used for weighted average diagnostics

diagnostics_is_on.F: Function call to inquire whether a diagnostic is active and should be incremented. Useful when there is a computation that must be done locally before a call to diagnostics_fill.F. The call sequence:

   flag = DIAGNOSTICS_IS_ON( diagName, myThid )

   diagName = diagnostic identificator name (8 characters long)
   myThid   = my thread Id number

diagnostics_count.F: This subroutine increments the diagnostics counter only. In general, the diagnostics counter is incremented at the same time as the diagnostics is filled, by calling diagnostics_fill.F. However, there are few cases where the counter is not incremented during the filling (e.g., when the filling is done level per level but level 1 is skipped) and needs to be done explicitly with a call to subroutine diagnostics_count.F. The call sequence is:

  I                        diagName, bi, bj, myThid )

   diagName  = name of diagnostic to increment the counter
   bi        = X-direction tile number, or 0 if called outside bi,bj loops
   bj        = Y-direction tile number, or 0 if called outside bi,bj loops
   myThid    = my thread Id number

The diagnostics are computed at various times and places within MITgcm. Because MITgcm may employ a staggered grid, diagnostics may be computed at grid box centers, corners, or edges, and at the middle or edge in the vertical. Some diagnostics are scalars, while others are components of vectors. An internal array is defined which contains information concerning various grid attributes of each diagnostic. The gdiag array (in common block diagnostics in file DIAGNOSTICS.h) is internally defined as a character*16 variable, and is equivalenced to a character*1 “parse” array in output in order to extract the grid-attribute information. The gdiag array is described in Table 9.1.

Table 9.1 Diagnostic Parsing Array





\(\rightarrow\) S

scalar diagnostic

\(\rightarrow\) U

U-vector component diagnostic

\(\rightarrow\) V

V-vector component diagnostic


\(\rightarrow\) U

C-grid U-point

\(\rightarrow\) V

C-grid V-point

\(\rightarrow\) M

C-grid mass point

\(\rightarrow\) Z

C-grid vorticity (corner) point



used for level-integrated output: cumulate levels

\(\rightarrow\) r

same but cumulate product by model level thickness

\(\rightarrow\) R

same but cumulate product by hFac & level thickness


\(\rightarrow\) P

positive definite diagnostic

\(\rightarrow\) A

Adjoint variable diagnostic


\(\rightarrow\) C

with counter array

\(\rightarrow\) P

post-processed (not filled up) from other diags

\(\rightarrow\) D

disable diagnostic for output


retired, formerly 3-digit mate number


\(\rightarrow\) U

model level + \(\frac{1}{2}\)

\(\rightarrow\) M

model level middle

\(\rightarrow\) L

model level - \(\frac{1}{2}\)


\(\rightarrow\) 0

levels = 0

\(\rightarrow\) 1

levels = 1

\(\rightarrow\) R

levels = Nr

\(\rightarrow\) L

levels = MAX(Nr,NrPhys)

\(\rightarrow\) M

levels = MAX(Nr,NrPhys) - 1

\(\rightarrow\) G

levels = ground_level number

\(\rightarrow\) I

levels = seaice_level number

\(\rightarrow\) X

free levels option (need to be set explicitly)

As an example, consider a diagnostic whose associated gdiag parameter is equal to UUR     MR. From gdiag we can determine that this diagnostic is a U-vector component located at the C-grid U-point, model mid-level (M) with Nr levels (last R).

In this way, each diagnostic in the model has its attributes (i.e., vector or scalar, C-grid location, etc.) defined internally. The output routines use this information in order to determine what type of transformations need to be performed. Any interpolations are done at the time of output rather than during each model step. In this way the user has flexibility in determining the type of output gridded data.

9.1.4. Usage Notes Using available diagnostics

To use the diagnostics package, other than enabling it in packages.conf and turning the useDiagnostics flag in data.pkg to .TRUE., there are two further steps the user must take to enable the diagnostics package for output of quantities that are already defined in MITgcm under an experiment’s configuration of packages. A parameter file data.diagnostics must be supplied in the run directory, and the file DIAGNOSTICS_SIZE.h must be included in the code directory. The steps for defining a new (permanent or experiment-specific temporary) diagnostic quantity will be outlined later.

The namelist in parameter file data.diagnostics will activate a user-defined list of diagnostics quantities to be computed, specify the frequency and type of output, the number of levels, and the name of all the separate output files. A sample data.diagnostics namelist file:

# Diagnostic Package Choices
#  dumpAtLast (logical): always write output at the end of simulation (default=F)
#  diag_mnc   (logical): write to NetCDF files (default=useMNC)
#--for each output-stream:
#  fileName(n) : prefix of the output file name (max 80c long) for outp.stream n
#  frequency(n):< 0 : write snap-shot output every |frequency| seconds
#               > 0 : write time-average output every frequency seconds
#  timePhase(n)     : write at time = timePhase + multiple of |frequency|
#    averagingFreq  : frequency (in s) for periodic averaging interval
#    averagingPhase : phase     (in s) for periodic averaging interval
#    repeatCycle    : number of averaging intervals in 1 cycle
#  levels(:,n) : list of levels to write to file (Notes: declared as REAL)
#                when this entry is missing, select all common levels of this list
#  fields(:,n) : list of selected diagnostics fields (8.c) in outp.stream n
#                (see "available_diagnostics.log" file for the full list of diags)
#  missing_value(n) : missing value for real-type fields in output file "n"
#  fileFlags(n)     : specific code (8c string) for output file "n"
  fields(1:2,1) = 'UVEL    ','VVEL    ',
   levels(1:5,1) = 1.,2.,3.,4.,5.,
   fileName(1) = 'diagout1',
  frequency(1) = 86400.,
  fields(1:2,2) = 'THETA   ','SALT    ',
   fileName(2) = 'diagout2',
  fileFlags(2) = ' P      ',
  levels(1:5,2) = 100000.0, 70000.0, 50000.0, 30000.0, 20000.0,
  frequency(2) = 3600.,


In this example, there are two output files that will be generated for each tile and for each output time. The first set of output files has the prefix diagout1, does time averaging every 86400. seconds, (frequency is 86400.), and will write fields which are multiple-level fields at output levels 1-5. The names of diagnostics quantities are UVEL and VVEL. The second set of output files has the prefix diagout2, does time averaging every 3600. seconds and the names of diagnostics quantities are THETA and SALT. It interpolates vertically to the pressure levels 100000 Pa, …, 20000 Pa.

The fileFlags parameter is explained in Table 9.2. Only the first three characters matter. The first character determines the precision of the output files. The default is to use writeBinaryPrec. The second character determines whether the fields are to be integrated or interpolated vertically or written as is (the default). Interpolation is only available in the atmosphere. The desired pressure levels need to be specified in levels. The third character is used to time average the product of a diagnostic with the appropriate thickness factor, hFacC, hFacW or hFacS. This is mostly useful with a non-linear free surface where the thickness factors vary in time. This will have an effect only for certain diagnostics, as determined by the parsing code (see Table 9.1 and the file available_diagnostics.log for a given setup): parse(3) has to be 'R', parse(5) blank and parse(9:10) 'MR'. Vorticity-point diagnostics cannot be hFac weighted. Note that the appropriate hFac factors are automatically included when integrating vertically (second character 'I'), so the ‘h’ is not needed in this case but could still improve accuracy of a time-averaged vertical integral when using non-linear free surface.

Table 9.2 Diagnostic fileFlags

Character pos





precision: 32 bits


precision: 64 bits

precision: writeBinaryPrec



integrate vertically


interpolate vertically

do not integrate or interpolate



multiply by hFac (if permitted) when filled

The user must assure that enough computer memory is allocated for the diagnostics and the output streams selected for a particular experiment. This is accomplished by modifying the file DIAGNOSTICS_SIZE.h and including it in the experiment code directory. The parameters that should be checked are called numDiags, numLists, numperList, and diagSt_size.

numDiags (and diagSt_size): All MITgcm diagnostic quantities are stored in the single diagnostic array gdiag which is located in the file and has the form:

_RL  qdiag(1-Olx,sNx+Olx,1-Olx,sNx+Olx,numDiags,nSx,nSy)
_RL  qSdiag(0:nStats,0:nRegions,diagSt_size,nSx,nSy)
COMMON / DIAG_STORE_R / qdiag, qSdiag

The first two-dimensions of diagSt_size correspond to the horizontal dimension of a given diagnostic, and the third dimension of diagSt_size is used to identify diagnostic fields and levels combined. In order to minimize the memory requirement of the model for diagnostics, the default MITgcm executable is compiled with room for only one horizontal diagnostic array, or with numDiags set to Nr. In order for the user to enable more than one 3-D diagnostic, the size of the diagnostics common must be expanded to accommodate the desired diagnostics. This can be accomplished by manually changing the parameter numDiags in the file . numDiags should be set greater than or equal to the sum of all the diagnostics activated for output each multiplied by the number of levels defined for that diagnostic quantity. For the above example, there are four multiple level fields, which the available diagnostics list (see below) indicates are defined at the MITgcm vertical resolution, Nr. The value of numDiags in DIAGNOSTICS_SIZE.h would therefore be equal to 4*Nr, or, say 40 if Nr=10.

numLists and numperList: The parameter numLists must be set greater than or equal to the number of separate output streams that the user specifies in the namelist file data.diagnostics. The parameter numperList corresponds to the maximum number of diagnostics requested per output streams. Adjoint variables

The diagnostics package can also be used to print adjoint state variables. Using the diagnostics package as opposed to using the standard ‘adjoint dump’ options allows one to take advantage of all the averaging and post processing routines available to other diagnostics variables.

Currently, the available adjoint state variables are:

109 |ADJetan |  1 |       |SM A    M1|dJ/m            |dJ/dEtaN: Sensitivity to sea surface height anomaly
110 |ADJuvel | 15 |   111 |UURA    MR|dJ/(m/s)        |dJ/dU: Sensitivity to zonal velocity
111 |ADJvvel | 15 |   110 |VVRA    MR|dJ/(m/s)        |dJ/dV: Sensitivity to meridional velocity
112 |ADJwvel | 15 |       |WM A    LR|dJ/(m/s)        |dJ/dW: Sensitivity to vertical velocity
113 |ADJtheta| 15 |       |SMRA    MR|dJ/degC         |dJ/dTheta: Sensitivity to potential temperature
114 |ADJsalt | 15 |       |SMRA    MR|dJ/(g/kg)       |dJ/dSalt: Sensitivity to salinity
115 |ADJtaux |  1 |   116 |UU A    U1|dJ/(N/m^2)      |dJ/dTaux: Senstivity to zonal surface wind stress
116 |ADJtauy |  1 |   115 |VV A    U1|dJ/(N/m^2)      |dJ/dTauy: Sensitivity to merid. surface wind stress
117 |ADJempmr|  1 |       |SM A    U1|dJ/(kg/m^2/s)   |dJ/dEmPmR: Sensitivity to net surface freshwater flux
118 |ADJqnet |  1 |       |SM A    U1|dJ/(W/m^2)      |dJ/dQnet: Sensitivity to net surface heat flux
119 |ADJqsw  |  1 |       |SM A    U1|dJ/(W/m^2)      |dJ/dQsw: Sensitivitiy to net Short-Wave radiation
120 |ADJsst  |  1 |       |SM A    M1|dJ/K            |dJ/dSST: Sensitivity to Sea Surface Temperature
121 |ADJsss  |  1 |       |SM A    M1|dJ/(g/kg)       |dJ/dSSS: Sensitivity to Sea Surface Salinity
122 |ADJbtdrg|  1 |       |SM A    M1|dJ/d()          |dJ/dCd: Sensitivity to bottom drag coefficient
123 |ADJdifkr| 15 |       |SMRA    MR|dJ/d(m^2/s))    |dJ/dKr: Sensitivity to vertical diffusivity
124 |ADJepsix| 15 |   125 |UURA    UR|dJ/(m^2/s)      |dJ/dEddyPsiX: Sensitivity to zonal eddystreamfunction
125 |ADJepsiy| 15 |   124 |VVRA    UR|dJ/(m^2/s)      |dJ/dEddyPsiY: Sensitivity to meridional eddystreamfunction

Additionally the packages gmredi, ptracrs, exf, and seaice have the following available adjoint diagnostics

225 |ADJkapgm| 15 |       |SMRA    MR|dJ/d[m^2/s]     |dJ/dKgm: Sensitivity to GM Intensity
226 |ADJkapre| 15 |       |SMRA    MR|dJ/d[m^2/s]     |dJ/dKredi: Sensitivity to Redi Coefficient
227 |TRAC01  | 15 |       |SMR     MR|mol C/m         |Dissolved Inorganic Carbon concentration
241 |ADJptr01| 15 |       |SMRA    MR|dJ/mol C/m      |sensitivity to Dissolved Inorganic Carbon concentration
221 |ADJustrs|  1 |   222 |UU A    U1|dJ/(N/m^2)      |dJ/dustress: Senstivity to zonal surface wind stress
222 |ADJvstrs|  1 |   221 |VV A    U1|dJ/(N/m^2)      |dJ/dvstrs: Sensitivity to merid. surface wind stress
223 |ADJhflux|  1 |       |SM A    U1|dJ/(W/m^2)      |dJ/dhflux: Sensitivity to upward heat flux
224 |ADJsflux|  1 |       |SM A    U1|dJ/(m/s)        |dJ/dhflux: Sensitivity to upward fresh water flux
225 |ADJatemp|  1 |       |SM A    U1|dJ/K            |dJ/datemp: Sensitivity to atmos. surface temperature
226 |ADJpreci|  1 |       |SM A    U1|dJ/(m/s)        |dJ/daqh: Sensitivity to precipitation
227 |ADJroff |  1 |       |SM A    U1|dJ/(m/s)        |dJ/daqh: Sensitivity to river runoff
228 |ADJswdn |  1 |       |SM A    U1|dJ/(W/m^2)      |dJ/dswdown: Sensitivity to downward SW radiation
229 |ADJlwdn |  1 |       |SM A    U1|dJ/(W/m^2)      |dJ/dlwdown: Sensitivity to downward LW radiation
230 |ADJuwind|  1 |       |UM A    U1|dJ/d(m/s)       |dJ/duwind: Senstivity to zonal 10-m wind speed
231 |ADJvwind|  1 |       |VM A    U1|dJ/d(m/s)       |dJ/dvwind: Senstivity to meridional 10-m wind speed
232 |ADJclsst|  1 |       |SM A    U1|dJ/K            |dJ/dclimsst: Sensitivity to restoring SST
233 |ADJclsss|  1 |       |SM A    U1|dJ/(g/kg)       |dJ/dclimsss: Sensitivity to restoring SSS
332 |ADJarea |  1 |       |SM A    M1|dJ/(m^2/m^2)    |dJ/darea: Sensitivity to seaice fractional ice-cover
333 |ADJheff |  1 |       |SM A    M1|dJ/dm           |dJ/dheff: Sensitvity to seaice ice thickness
334 |ADJhsnow|  1 |       |SM A    M1|dJ/dm           |dJ/dhsnow: Sensitivity to seaice snow thickness
335 |ADJuice |  1 |   336 |UU A    M1|dJ/(m/s)        |dJ/duice: sensitivity to zonal ice velocity
336 |ADJvice |  1 |   335 |VV A    M1|dJ/(m/s)        |dJ/dvice: sensitivity to meridional ice velocity Some notes to the user
  1. This feature is currently untested with OpenAD.

  2. This feature does not work with the divided adjoint.

  3. The sensitivity to sea surface height ADJetan is technically one time step ahead of other adjoint diagnostics printed at the same time step number. To be concrete, if ADJetan is written via the diagnostics package at every iteration, n, then each field will technically correspond to the written iteration number, n+1. This is simply due to a techincality about when this variable is printed in relation to the adjoint pressure solve.

  4. The diagStats options are not available for these variables.

  5. Adjoint variables are recognized by checking the 10 character variable diagCode. To add a new adjoint variable, set the 4th position of diagCode to A (notice this is the case for the list of available adjoint variables). Using pkg/diagnostics for adjoint variables
  1. Make sure the following flag is defined in either AUTODIFF_OPTIONS.h or ECCO_CPPOPTIONS.h if that is being used.

  1. Be sure to increase numlists and numDiags appropriately in DIAGNOSTICS_SIZE.h. Safe values are e.g. 10-20 and 500-1000 respectively.

  2. Specify desired variables in data.diagnostics as any other variable, as in the following example or as in this data.diagnostics. Note however, adjoint and forward diagnostic variables cannot be in the same list. That is, a single fields(:,:) list cannot contain both adjoint and forward variables.

# ---
  fields(1:5,1) = 'ADJtheta','ADJsalt ',
                     'ADJuvel ','ADJvvel ','ADJwvel '
  filename(1) = 'diags/adjState_3d_snaps',
  fields(1:5,2) = 'ADJtheta','ADJsalt ',
                     'ADJuvel ','ADJvvel ','ADJwvel '
  filename(2) = 'diags/adjState_3d_avg',
  frequency(2)= 86400.0,

Note: the diagnostics package automatically provides a phase shift of \(frequency/2\), so specify timePhase = 0 to match output from adjDumpFreq. Adding new diagnostics to the code

In order to define and include as part of the diagnostic output any field that is desired for a particular experiment, two steps must be taken. The first is to enable the “User Diagnostic” in data.diagnostics. This is accomplished by adding one of the “User Diagnostic” field names (see available diagnostics):UDIAG1 through UDIAG10, for multi-level fields, or SDIAG1 through SDIAG10 for single level fields) to the data.diagnostics namelist in one of the output streams. The second step is to add a call to diagnostics_fill.F from the subroutine in which the quantity desired for diagnostic output is computed.

In order to add a new diagnostic to the permanent set of diagnostics that the main model or any package contains as part of its diagnostics menu, the subroutine diagnostics_addtolist.F should be called during the initialization phase of the main model or package. For the main model, the call should be made from subroutine diagnostics_main_init.F, and for a package, the call should probably be made from from inside the particular package’s init_fixed routine. A typical code sequence to set the input arguments to diagnostics_addtolist.F would look like:

 diagName  = 'RHOAnoma'
 diagTitle = 'Density Anomaly (=Rho-rhoConst)'
 diagUnits = 'kg/m^3          '
 diagCode  = 'SMR     MR      '
I          diagName, diagCode, diagUnits, diagTitle, 0, myThid )

If the new diagnostic quantity is associated with either a vector pair or a diagnostic counter, the diagMate argument must be provided with the proper index corresponding to the “mate”. The output argument from diagnostics_addtolist.F that is called diagNum here contains a running total of the number of diagnostics defined in the code up to any point during the run. The sequence number for the next two diagnostics defined (the two components of the vector pair, for instance) will be diagNum+1 and diagNum+2. The definition of the first component of the vector pair must fill the “mate” segment of the diagCode as diagnostic number diagNum+2. Since the subroutine increments diagNum, the definition of the second component of the vector fills the “mate” part of diagCode with diagNum. A code sequence for this case would look like:

 diagName  = 'UVEL    '
 diagTitle = 'Zonal Component of Velocity (m/s)'
 diagUnits = 'm/s             '
 diagCode  = 'UUR     MR      '
 diagMate  = diagNum + 2
I   diagName, diagCode, diagUnits, diagTitle, diagMate, myThid )

 diagName  = 'VVEL    '
 diagTitle = 'Meridional Component of Velocity (m/s)'
 diagUnits = 'm/s             '
 diagCode  = 'VVR     MR      '
 diagMate  = diagNum
I   diagName, diagCode, diagUnits, diagTitle, diagMate, myThid ) MITgcm kernel available diagnostics list:

<-Name->|<- code ->|<--  Units   -->|<- Tile (max=80c)
SDIAG1  |SM      L1|user-defined    |User-Defined   Surface   Diagnostic  #1
SDIAG2  |SM      L1|user-defined    |User-Defined   Surface   Diagnostic  #2
SDIAG3  |SM      L1|user-defined    |User-Defined   Surface   Diagnostic  #3
SDIAG4  |SM      L1|user-defined    |User-Defined   Surface   Diagnostic  #4
SDIAG5  |SM      L1|user-defined    |User-Defined   Surface   Diagnostic  #5
SDIAG6  |SM      L1|user-defined    |User-Defined   Surface   Diagnostic  #6
SDIAG7  |SU      L1|user-defined    |User-Defined U.pt Surface Diagnostic #7
SDIAG8  |SV      L1|user-defined    |User-Defined V.pt Surface Diagnostic #8
SDIAG9  |UU      L1|user-defined    |User-Defined U.vector Surface Diag.  #9
SDIAG10 |VV      L1|user-defined    |User-Defined V.vector Surface Diag. #10
UDIAG1  |SM      MR|user-defined    |User-Defined Model-Level Diagnostic  #1
UDIAG2  |SM      MR|user-defined    |User-Defined Model-Level Diagnostic  #2
UDIAG3  |SMR     MR|user-defined    |User-Defined Model-Level Diagnostic  #3
UDIAG4  |SMR     MR|user-defined    |User-Defined Model-Level Diagnostic  #4
UDIAG5  |SU      MR|user-defined    |User-Defined U.pt Model-Level Diag.  #5
UDIAG6  |SV      MR|user-defined    |User-Defined V.pt Model-Level Diag.  #6
UDIAG7  |UUR     MR|user-defined    |User-Defined U.vector Model-Lev Diag.#7
UDIAG8  |VVR     MR|user-defined    |User-Defined V.vector Model-Lev Diag.#8
UDIAG9  |SM      ML|user-defined    |User-Defined Phys-Level  Diagnostic  #9
UDIAG10 |SM      ML|user-defined    |User-Defined Phys-Level  Diagnostic #10
SDIAGC  |SM  C   L1|user-defined    |User-Defined Counted Surface Diagnostic
SDIAGCC |SM      L1|count           |User-Defined Surface Diagnostic Counter
ETAN    |SM      M1|m               |Surface Height Anomaly
ETANSQ  |SM P    M1|m^2             |Square of Surface Height Anomaly
DETADT2 |SM      M1|m^2/s^2         |Square of Surface Height Anomaly Tendency
THETA   |SMR     MR|degC            |Potential Temperature
SALT    |SMR     MR|g/kg            |Salinity
RELHUM  |SMR     MR|percent         |Relative Humidity
SALTanom|SMR     MR|g/kg            |Salt anomaly (=SALT-35; g/kg)
UVEL    |UUR     MR|m/s             |Zonal Component of Velocity (m/s)
VVEL    |VVR     MR|m/s             |Meridional Component of Velocity (m/s)
WVEL    |WM      LR|m/s             |Vertical Component of Velocity (r_units/s)
THETASQ |SMRP    MR|degC^2          |Square of Potential Temperature
SALTSQ  |SMRP    MR|(g/kg)^2        |Square of Salinity
SALTSQan|SMRP    MR|(g/kg)^2        |Square of Salt anomaly (=(SALT-35)^2 (g^2/kg^2)
UVELSQ  |UURP    MR|m^2/s^2         |Square of Zonal Comp of Velocity (m^2/s^2)
VVELSQ  |VVRP    MR|m^2/s^2         |Square of Meridional Comp of Velocity (m^2/s^2)
WVELSQ  |WM P    LR|m^2/s^2         |Square of Vertical Comp of Velocity
UE_VEL_C|UMR     MR|m/s             |Eastward Velocity (m/s) (cell center)
VN_VEL_C|VMR     MR|m/s             |Northward Velocity (m/s) (cell center)
UV_VEL_C|UMR     MR|m^2/s^2         |Product of horizontal Comp of velocity (cell center)
UV_VEL_Z|UZR     MR|m^2/s^2         |Meridional Transport of Zonal Momentum (m^2/s^2)
WU_VEL  |WU      LR|m.m/s^2         |Vertical Transport of Zonal Momentum
WV_VEL  |WV      LR|m.m/s^2         |Vertical Transport of Meridional Momentum
UVELMASS|UUr     MR|m/s             |Zonal Mass-Weighted Comp of Velocity (m/s)
VVELMASS|VVr     MR|m/s             |Meridional Mass-Weighted Comp of Velocity (m/s)
WVELMASS|WM      LR|m/s             |Vertical Mass-Weighted Comp of Velocity
PhiVEL  |SMR P   MR|m^2/s           |Horizontal Velocity Potential (m^2/s)
PsiVEL  |SZ  P   MR|m.m^2/s         |Horizontal Velocity Stream-Function
UTHMASS |UUr     MR|degC.m/s        |Zonal Mass-Weight Transp of Pot Temp
VTHMASS |VVr     MR|degC.m/s        |Meridional Mass-Weight Transp of Pot Temp
WTHMASS |WM      LR|degC.m/s        |Vertical Mass-Weight Transp of Pot Temp (K.m/s)
USLTMASS|UUr     MR|g/kg.m/s        |Zonal Mass-Weight Transp of Salinity
VSLTMASS|VVr     MR|g/kg.m/s        |Meridional Mass-Weight Transp of Salinity
WSLTMASS|WM      LR|g/kg.m/s        |Vertical Mass-Weight Transp of Salinity
UVELTH  |UUR     MR|degC.m/s        |Zonal Transport of Pot Temp
VVELTH  |VVR     MR|degC.m/s        |Meridional Transport of Pot Temp
WVELTH  |WM      LR|degC.m/s        |Vertical Transport of Pot Temp
UVELSLT |UUR     MR|g/kg.m/s        |Zonal Transport of Salinity
VVELSLT |VVR     MR|g/kg.m/s        |Meridional Transport of Salinity
WVELSLT |WM      LR|g/kg.m/s        |Vertical Transport of Salinity
UVELPHI |UUr     MR|m^3/s^3         |Zonal Mass-Weight Transp of Pressure Pot.(p/rho) Anomaly
VVELPHI |VVr     MR|m^3/s^3         |Merid. Mass-Weight Transp of Pressure Pot.(p/rho) Anomaly
RHOAnoma|SMR     MR|kg/m^3          |Density Anomaly (=Rho-rhoConst)
RHOANOSQ|SMRP    MR|kg^2/m^6        |Square of Density Anomaly (=(Rho-rhoConst)^2)
URHOMASS|UUr     MR|kg/m^2/s        |Zonal Transport of Density
VRHOMASS|VVr     MR|kg/m^2/s        |Meridional Transport of Density
WRHOMASS|WM      LR|kg/m^2/s        |Vertical Transport of Density
WdRHO_P |WM      LR|kg/m^2/s        |Vertical velocity times delta^k(Rho)_at-const-P
WdRHOdP |WM      LR|kg/m^2/s        |Vertical velocity times delta^k(Rho)_at-const-T,S
PHIHYD  |SMR     MR|m^2/s^2         |Hydrostatic Pressure Pot.(p/rho) Anomaly
PHIHYDSQ|SMRP    MR|m^4/s^4         |Square of Hyd. Pressure Pot.(p/rho) Anomaly
PHIBOT  |SM      M1|m^2/s^2         |Bottom Pressure Pot.(p/rho) Anomaly
PHIBOTSQ|SM P    M1|m^4/s^4         |Square of Bottom Pressure Pot.(p/rho) Anomaly
PHI_SURF|SM      M1|m^2/s^2         |Surface Dynamical Pressure Pot.(p/rho)
PHIHYDcR|SMR     MR|m^2/s^2         |Hydrostatic Pressure Pot.(p/rho) Anomaly @ const r
PHI_NH  |SMR     MR|m^2/s^2         |Non-Hydrostatic Pressure Pot.(p/rho)
MXLDEPTH|SM      M1|m               |Mixed-Layer Depth (>0)
DRHODR  |SM      LR|kg/m^4          |Stratification: d.Sigma/dr (kg/m3/r_unit)
CONVADJ |SMR     LR|fraction        |Convective Adjustment Index [0-1]
oceTAUX |UU      U1|N/m^2           |zonal surface wind stress, >0 increases uVel
oceTAUY |VV      U1|N/m^2           |meridional surf. wind stress, >0 increases vVel
atmPload|SM      U1|Pa              |Atmospheric pressure loading anomaly (vs surf_pRef)
sIceLoad|SM      U1|kg/m^2          |sea-ice loading (in Mass of ice+snow / area unit)
oceFWflx|SM      U1|kg/m^2/s        |net surface Fresh-Water flux into the ocean (+=down), >0 decreases salinity
oceSflux|SM      U1|g/m^2/s         |net surface Salt flux into the ocean (+=down), >0 increases salinity
oceQnet |SM      U1|W/m^2           |net surface heat flux into the ocean (+=down), >0 increases theta
oceQsw  |SM      U1|W/m^2           |net Short-Wave radiation (+=down), >0 increases theta
oceFreez|SM      U1|W/m^2           |heating from freezing of sea-water (allowFreezing=T)
TRELAX  |SM      U1|W/m^2           |surface temperature relaxation, >0 increases theta
SRELAX  |SM      U1|g/m^2/s         |surface salinity relaxation, >0 increases salt
surForcT|SM      U1|W/m^2           |model surface forcing for Temperature, >0 increases theta
surForcS|SM      U1|g/m^2/s         |model surface forcing for Salinity, >0 increases salinity
TFLUX   |SM      U1|W/m^2           |total heat flux (match heat-content variations), >0 increases theta
SFLUX   |SM      U1|g/m^2/s         |total salt flux (match salt-content variations), >0 increases salt
RCENTER |SM      MR|m               |Cell-Center Height
RSURF   |SM      M1|m               |Surface Height
hFactorC|SMr     MR|1               |Center cell-thickness fraction [-]
hFactorW|SUr     MR|1               |Western-Edge cell-thickness fraction [-]
hFactorS|SVr     MR|1               |Southern-Edge cell-thickness fraction [-]
TOTUTEND|UUR     MR|m/s/day         |Tendency of Zonal Component of Velocity
TOTVTEND|VVR     MR|m/s/day         |Tendency of Meridional Component of Velocity
TOTTTEND|SMR     MR|degC/day        |Tendency of Potential Temperature
TOTSTEND|SMR     MR|g/kg/day        |Tendency of Salinity
<-Name->|<- code ->|<--  Units   -->|<- Tile (max=80c)
MoistCor|SM      MR|W/m^2           |Heating correction due to moist thermodynamics
HeatDiss|SM      MR|W/m^2           |Heating from frictional dissipation
gT_Forc |SMR     MR|degC/s          |Potential Temp. forcing tendency
gS_Forc |SMR     MR|g/kg/s          |Salinity forcing tendency
AB_gT   |SMR     MR|degC/s          |Potential Temp. tendency from Adams-Bashforth
AB_gS   |SMR     MR|g/kg/s          |Salinity tendency from Adams-Bashforth
gTinAB  |SMR     MR|degC/s          |Potential Temp. tendency going in Adams-Bashforth
gSinAB  |SMR     MR|g/kg/s          |Salinity tendency going in Adams-Bashforth
AB_gU   |UUR     MR|m/s^2           |U momentum tendency from Adams-Bashforth
AB_gV   |VVR     MR|m/s^2           |V momentum tendency from Adams-Bashforth
AB_gW   |WM      LR|m/s^2           |W momentum tendency from Adams-Bashforth
TAUXEDDY|UU      LR|N/m^2           |Zonal Eddy Stress
TAUYEDDY|VV      LR|N/m^2           |Meridional Eddy Stress
U_EulerM|UUR     MR|m/s             |Zonal Eulerian-Mean Velocity (m/s)
V_EulerM|VVR     MR|m/s             |Meridional Eulerian-Mean Velocity (m/s)
ADVr_TH |WM      LR|degC.m^3/s      |Vertical   Advective Flux of Pot.Temperature
ADVx_TH |UU      MR|degC.m^3/s      |Zonal      Advective Flux of Pot.Temperature
ADVy_TH |VV      MR|degC.m^3/s      |Meridional Advective Flux of Pot.Temperature
DFrE_TH |WM      LR|degC.m^3/s      |Vertical Diffusive Flux of Pot.Temperature (Explicit part)
DFxE_TH |UU      MR|degC.m^3/s      |Zonal      Diffusive Flux of Pot.Temperature
DFyE_TH |VV      MR|degC.m^3/s      |Meridional Diffusive Flux of Pot.Temperature
DFrI_TH |WM      LR|degC.m^3/s      |Vertical Diffusive Flux of Pot.Temperature (Implicit part)
SM_x_TH |UM      MR|degC            |Pot.Temp.   1rst Order Moment Sx
SM_y_TH |VM      MR|degC            |Pot.Temp.   1rst Order Moment Sy
SM_z_TH |SM      MR|degC            |Pot.Temp.   1rst Order Moment Sz
SMxx_TH |UM      MR|degC            |Pot.Temp.   2nd Order Moment Sxx
SMyy_TH |VM      MR|degC            |Pot.Temp.   2nd Order Moment Syy
SMzz_TH |SM      MR|degC            |Pot.Temp.   2nd Order Moment Szz
SMxy_TH |SM      MR|degC            |Pot.Temp.   2nd Order Moment Sxy
SMxz_TH |UM      MR|degC            |Pot.Temp.   2nd Order Moment Sxz
SMyz_TH |VM      MR|degC            |Pot.Temp.   2nd Order Moment Syz
SM_v_TH |SM P    MR|(degC)^2        |Pot.Temp.   sub-grid variance
ADVr_SLT|WM      LR|g/kg.m^3/s      |Vertical   Advective Flux of Salinity
ADVx_SLT|UU      MR|g/kg.m^3/s      |Zonal      Advective Flux of Salinity
ADVy_SLT|VV      MR|g/kg.m^3/s      |Meridional Advective Flux of Salinity
DFrE_SLT|WM      LR|g/kg.m^3/s      |Vertical Diffusive Flux of Salinity    (Explicit part)
DFxE_SLT|UU      MR|g/kg.m^3/s      |Zonal      Diffusive Flux of Salinity
DFyE_SLT|VV      MR|g/kg.m^3/s      |Meridional Diffusive Flux of Salinity
DFrI_SLT|WM      LR|g/kg.m^3/s      |Vertical Diffusive Flux of Salinity    (Implicit part)
SALTFILL|SM      MR|g/kg.m^3/s      |Filling of Negative Values of Salinity
SM_x_SLT|UM      MR|g/kg            |Salinity    1rst Order Moment Sx
SM_y_SLT|VM      MR|g/kg            |Salinity    1rst Order Moment Sy
SM_z_SLT|SM      MR|g/kg            |Salinity    1rst Order Moment Sz
SMxx_SLT|UM      MR|g/kg            |Salinity    2nd Order Moment Sxx
SMyy_SLT|VM      MR|g/kg            |Salinity    2nd Order Moment Syy
SMzz_SLT|SM      MR|g/kg            |Salinity    2nd Order Moment Szz
SMxy_SLT|SM      MR|g/kg            |Salinity    2nd Order Moment Sxy
SMxz_SLT|UM      MR|g/kg            |Salinity    2nd Order Moment Sxz
SMyz_SLT|VM      MR|g/kg            |Salinity    2nd Order Moment Syz
SM_v_SLT|SM P    MR|(g/kg)^2        |Salinity    sub-grid variance
VISCAHZ |SZ      MR|m^2/s           |Harmonic Visc Coefficient (m2/s) (Zeta Pt)
VISCA4Z |SZ      MR|m^4/s           |Biharmonic Visc Coefficient (m4/s) (Zeta Pt)
VISCAHD |SM      MR|m^2/s           |Harmonic Viscosity Coefficient (m2/s) (Div Pt)
VISCA4D |SM      MR|m^4/s           |Biharmonic Viscosity Coefficient (m4/s) (Div Pt)
VISCAHW |WM      LR|m^2/s           |Harmonic Viscosity Coefficient (m2/s) (W Pt)
VISCA4W |WM      LR|m^4/s           |Biharmonic Viscosity Coefficient (m4/s) (W Pt)
VAHZMAX |SZ      MR|m^2/s           |CFL-MAX Harm Visc Coefficient (m2/s) (Zeta Pt)
VA4ZMAX |SZ      MR|m^4/s           |CFL-MAX Biharm Visc Coefficient (m4/s) (Zeta Pt)
VAHDMAX |SM      MR|m^2/s           |CFL-MAX Harm Visc Coefficient (m2/s) (Div Pt)
VA4DMAX |SM      MR|m^4/s           |CFL-MAX Biharm Visc Coefficient (m4/s) (Div Pt)
VAHZMIN |SZ      MR|m^2/s           |RE-MIN Harm Visc Coefficient (m2/s) (Zeta Pt)
VA4ZMIN |SZ      MR|m^4/s           |RE-MIN Biharm Visc Coefficient (m4/s) (Zeta Pt)
VAHDMIN |SM      MR|m^2/s           |RE-MIN Harm Visc Coefficient (m2/s) (Div Pt)
VA4DMIN |SM      MR|m^4/s           |RE-MIN Biharm Visc Coefficient (m4/s) (Div Pt)
VAHZLTH |SZ      MR|m^2/s           |Leith Harm Visc Coefficient (m2/s) (Zeta Pt)
VA4ZLTH |SZ      MR|m^4/s           |Leith Biharm Visc Coefficient (m4/s) (Zeta Pt)
VAHDLTH |SM      MR|m^2/s           |Leith Harm Visc Coefficient (m2/s) (Div Pt)
VA4DLTH |SM      MR|m^4/s           |Leith Biharm Visc Coefficient (m4/s) (Div Pt)
VAHZLTHD|SZ      MR|m^2/s           |LeithD Harm Visc Coefficient (m2/s) (Zeta Pt)
VA4ZLTHD|SZ      MR|m^4/s           |LeithD Biharm Visc Coefficient (m4/s) (Zeta Pt)
VAHDLTHD|SM      MR|m^2/s           |LeithD Harm Visc Coefficient (m2/s) (Div Pt)
VA4DLTHD|SM      MR|m^4/s           |LeithD Biharm Visc Coefficient (m4/s) (Div Pt)
VAHZLTHQ|SZ      MR|m^2/s           |LeithQG Harm Visc Coefficient (m2/s) (Zeta Pt)
VAHDLTHQ|SM      MR|m^2/s           |LeithQG Harm Visc Coefficient (m2/s) (Div Pt)
VAHZSMAG|SZ      MR|m^2/s           |Smagorinsky Harm Visc Coefficient (m2/s) (Zeta Pt)
VA4ZSMAG|SZ      MR|m^4/s           |Smagorinsky Biharm Visc Coeff. (m4/s) (Zeta Pt)
VAHDSMAG|SM      MR|m^2/s           |Smagorinsky Harm Visc Coefficient (m2/s) (Div Pt)
VA4DSMAG|SM      MR|m^4/s           |Smagorinsky Biharm Visc Coeff. (m4/s) (Div Pt)
momKE   |SMR     MR|m^2/s^2         |Kinetic Energy (in momentum Eq.)
momHDiv |SMR     MR|s^-1            |Horizontal Divergence (in momentum Eq.)
momVort3|SZR     MR|s^-1            |3rd component (vertical) of Vorticity
Strain  |SZR     MR|s^-1            |Horizontal Strain of Horizontal Velocities
Tension |SMR     MR|s^-1            |Horizontal Tension of Horizontal Velocities
Stretch |SM      MR|s^-1            |Vortex stretching from QG Leith dynamic viscosity
USidDrag|UUR     MR|m/s^2           |U momentum tendency from Side Drag
VSidDrag|VVR     MR|m/s^2           |V momentum tendency from Side Drag
Um_Diss |UUR     MR|m/s^2           |U momentum tendency from Dissipation (Explicit part)
Vm_Diss |VVR     MR|m/s^2           |V momentum tendency from Dissipation (Explicit part)
Um_ImplD|UUR     MR|m/s^2           |U momentum tendency from Dissipation (Implicit part)
Vm_ImplD|VVR     MR|m/s^2           |V momentum tendency from Dissipation (Implicit part)
Um_Advec|UUR     MR|m/s^2           |U momentum tendency from Advection terms
Vm_Advec|VVR     MR|m/s^2           |V momentum tendency from Advection terms
Um_Cori |UUR     MR|m/s^2           |U momentum tendency from Coriolis term
Vm_Cori |VVR     MR|m/s^2           |V momentum tendency from Coriolis term
Um_dPhiX|UUR     MR|m/s^2           |U momentum tendency from Pressure/Potential grad
Vm_dPhiY|VVR     MR|m/s^2           |V momentum tendency from Pressure/Potential grad
Um_Ext  |UUR     MR|m/s^2           |U momentum tendency from external forcing
Vm_Ext  |VVR     MR|m/s^2           |V momentum tendency from external forcing
Um_AdvZ3|UUR     MR|m/s^2           |U momentum tendency from Vorticity Advection
Vm_AdvZ3|VVR     MR|m/s^2           |V momentum tendency from Vorticity Advection
Um_AdvRe|UUR     MR|m/s^2           |U momentum tendency from vertical Advection (Explicit part)
Vm_AdvRe|VVR     MR|m/s^2           |V momentum tendency from vertical Advection (Explicit part)
Wm_Diss |WMr     LR|m/s^2           |W momentum tendency from Dissipation
Wm_Advec|WMr     LR|m/s^2           |W momentum tendency from Advection terms
WSidDrag|WMr     LR|m/s^2           |Vertical momentum tendency from Side Drag
botTauX |UU      U1|N/m^2           |zonal bottom stress, >0 increases uVel
botTauY |VV      U1|N/m^2           |meridional bottom stress, >0 increases vVel
ADVx_Um |UM      MR|m^4/s^2         |Zonal      Advective Flux of U momentum
ADVy_Um |VZ      MR|m^4/s^2         |Meridional Advective Flux of U momentum
ADVrE_Um|WU      LR|m^4/s^2         |Vertical   Advective Flux of U momentum (Explicit part)
ADVx_Vm |UZ      MR|m^4/s^2         |Zonal      Advective Flux of V momentum
ADVy_Vm |VM      MR|m^4/s^2         |Meridional Advective Flux of V momentum
ADVrE_Vm|WV      LR|m^4/s^2         |Vertical   Advective Flux of V momentum (Explicit part)
VISCx_Um|UM      MR|m^4/s^2         |Zonal      Viscous Flux of U momentum
VISCy_Um|VZ      MR|m^4/s^2         |Meridional Viscous Flux of U momentum
VISrE_Um|WU      LR|m^4/s^2         |Vertical   Viscous Flux of U momentum (Explicit part)
VISrI_Um|WU      LR|m^4/s^2         |Vertical   Viscous Flux of U momentum (Implicit part)
VISCx_Vm|UZ      MR|m^4/s^2         |Zonal      Viscous Flux of V momentum
VISCy_Vm|VM      MR|m^4/s^2         |Meridional Viscous Flux of V momentum
VISrE_Vm|WV      LR|m^4/s^2         |Vertical   Viscous Flux of V momentum (Explicit part)
VISrI_Vm|WV      LR|m^4/s^2         |Vertical   Viscous Flux of V momentum (Implicit part)

The meaning of the “code” column is explained in Table 9.1. The last character of the code, in particular, determines the number of vertical levels in the diagnostic (of the commonly used codes, “1” represents a 2-D diagnostic, “R” and “L” are multi-level diagnostics). MITgcm packages: available diagnostics lists

For a list of the diagnostic fields available in the different MITgcm packages, follow the link to the available diagnostics listing in the manual section describing the package:

9.2. Fortran Native I/O: pkg/mdsio and pkg/rw

9.2.1. pkg/mdsio Introduction

pkg/mdsio contains a group of Fortran routines intended as a general interface for reading and writing direct-access (“binary”) Fortran files. pkg/mdsio routines are used by pkg/rw. Using pkg/mdsio

pkg/mdsio is geared toward the reading and writing of floating point (Fortran REAL*4 or REAL*8) arrays. It assumes that the in-memory layout of all arrays follows the per-tile MITgcm convention

C     Example of a "2D" array
      _RL anArray(1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy)

C     Example of a "3D" array
      _RL anArray(1-OLx:sNx+OLx,1-OLy:sNy+OLy,1:Nr,nSx,nSy)

where the first two dimensions are spatial or “horizontal” indicies that include a “halo” or exchange region (please see Section 6 and Section 8.2.5 which describe domain decomposition), and the remaining indicies (Nr, nSx, and nSx) are often present but may or may not be necessary for a specific variable..

In order to write output, pkg/mdsio is called with a function such as:

CALL MDSWRITEFIELD(fn,prec,lgf,typ,Nr,arr,irec,myIter,myThid)



is a CHARACTER string containing a file “base” name which will then be used to create file names that contain tile and/or model iteration indicies


is an integer that contains one of two globally defined values (precFloat64 or precFloat32)


is a LOGICAL that typically contains the globally defined globalFile option which specifies the creation of globally (spatially) concatenated files


is a CHARACTER string that specifies the type of the variable being written (’RL’ or ’RS’)


is an integer that specifies the number of vertical levels within the variable being written


is the variable (array) to be written


is the starting record within the output file that will contain the array


are integers containing, respectively, the current model iteration count and the unique thread ID for the current context of execution

As one can see from the above (generic) example, enough information is made available (through both the argument list and through common blocks) for pkg/mdsio to perform the following tasks:

  1. open either a per-tile file such as:


    or a “global” file such as


  2. byte-swap (as necessary) the input array and write its contents (minus any halo information) to the binary file – or to the correct location within the binary file if the globalfile option is used, and

  3. create an ASCII–text metadata file (same name as the binary but with a .meta extension) describing the binary file contents (often, for later use with the MATLAB rdmds() utility).

Reading output with pkg/mdsio is very similar to writing it. A typical function call is

CALL MDSREADFIELD(fn,prec,typ,Nr,arr,irec,myThid)

where variables are exactly the same as the MDSWRITEFIELD example provided above. It is important to note that the lgf argument is missing from the MDSREADFIELD function. By default, pkg/mdsio will first try to read from an appropriately named global file and, failing that, will try to read from a per-tile file. Important considerations

When using pkg/mdsio, one should be aware of the following package features and limitations:

  • Byte-swapping: For the most part, byte-swapping is gracefully handled. All files intended for reading/writing by pkg/mdsio should contain big-endian (sometimes called “network byte order”) data. By handling byte-swapping within the model, MITgcm output is more easily ported between different machines, architectures, compilers, etc. Byteswapping can be turned on/off at compile time within pkg/mdsio using the _BYTESWAPIO CPP macro which is usually set within a genmake2 options file or optfile (see Section Additionally, some compilers may have byte-swap options that are speedier or more convenient to use.

  • Data types: Data types are currently limited to single– or double–precision floating point values. These values can be converted, on-the-fly, from one to the other so that any combination of either single– or double–precision variables can be read from or written to files containing either single– or double–precision data.

  • Array sizes: Array sizes are limited; pkg/mdsio is very much geared towards the reading/writing of per-tile (that is, domain-decomposed and halo-ed) arrays. Data that cannot be made to “fit” within these assumed sizes can be challenging to read or write with pkg/mdsio.

  • Tiling: Tiling or domain decomposition is automatically handled by pkg/mdsio for logically rectangular grid topologies (e.g., lat-lon grids) and “standard” cubed sphere topologies. More complicated topologies will probably not be supported. pkg/mdsio can, without any coding changes, read and write to/from files that were run on the same global grid but with different tiling (grid decomposition) schemes. For example, pkg/mdsio can use and/or create identical input/output files for a “C32” cube when the model is run with either 6, 12, or 24 tiles (corresponding to 1, 2 or 4 tiles per cubed sphere face). This is one of the primary advantages that the pkg/mdsio package has over pkg/mnc.

  • Single-CPU I/O: This option can be specified with the flag useSingleCpuIO = .TRUE. in the PARM01 namelist within the main data file. Single–CPU I/O mode is appropriate for computers (e.g., some SGI systems) where it can either speed overall I/O or solve problems where the operating system or file systems cannot correctly handle multiple threads or MPI processes simultaneously writing to the same file.

  • Meta-data: Meta-data is written by MITgcm on a per-file basis using a second file with a .meta extension as described above. MITgcm itself does not read the *.meta files, they are there primarly for convenience during post-processing. One should be careful not to delete the meta-data files when using MATLAB post-processing scripts such as rdmds() since it relies upon them.

  • Numerous files: If one is not careful (e.g., dumping many variables every time step over a long integration), pkg/mdsio will write copious amounts of files. The creation of both a binary (*.data) and ASCII text meta-data (*.meta) file for each output type step exacerbates the issue. Some operating systems do not gracefully handle large numbers (e.g., many thousands to millions) of files within one directory. So care should be taken to split output into smaller groups using subdirectories.

  • Overwriting output: Overwriting of output is the default behavior for pkg/mdsio. If a model tries to write to a file name that already exists, the older file will be deleted. For this reason, MITgcm users should be careful to move output that they wish to keep into, for instance, subdirectories before performing subsequent runs that may over–lap in time or otherwise produce files with identical names (e.g., Monte-Carlo simulations).

  • No “halo” information: “Halo” information is neither written nor read by pkg/mdsio. Along the horizontal dimensions, all variables are written in an sNx–by–sNy fashion. So, although variables (arrays) may be defined at different locations on Arakawa grids [U (right/left horizontal edges), V (top/bottom horizontal edges), M (mass or cell center), or Z (vorticity or cell corner) points], they are all written using only interior (1:sNx and 1:sNy) values. For quantities defined at U, V, and M points, writing 1:sNx and 1:sNy for every tile is sufficient to ensure that all values are written globally for some grids (e.g., cubed sphere, re-entrant channels, and doubly-periodic rectangular regions). For Z points, failing to write values at the sNx+1 and sNy+1 locations means that, for some tile topologies, not all values are written. For instance, with a cubed sphere topology at least two corner values are “lost” (fail to be written for any tile) if the sNx+1 and sNy+1 values are ignored. If this is an issue, we recommend switching to pkg/mnc, which writes the sNx+1 and sNy+1 grid values for the U, V, and Z locations. Also, pkg/mnc is capable of reading and/or writing entire halo regions and more complicated array shapes which can be helpful when debugging – features that do not exist within pkg/mdsio.

CPP Flag Name





if defined, stops the model from overwriting its own files



I/O will include tile halos in the files

9.2.2. pkg/rw basic binary I/O utilities

pkg/rw provides a very rudimentary binary I/O capability for quickly writing single record direct-access Fortran binary files. It is primarily used for writing diagnostic output. Introduction

pkg/rw is an interface to the more general pkg/mdsio package. pkg/rw can be used to write or read direct-access Fortran binary files for 2-D XY and 3-D XYZ arrays. The arrays are assumed to have been declared according to the standard MITgcm 2-D or 3-D floating point array type:

C     Example of declaring a standard two dimensional "long"
C     floating point type array (the _RL macro is usually
C     mapped to 64-bit floats in most configurations)
      _RL anArray(1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy)

Each call to a pkg/rw read or write routine will read (or write) to the first record of a file. To write direct access Fortran files with multiple records use the higher-level routines in pkg/mdsio rather than pkg/rw routines. To write self-describing files that contain embedded information describing the variables being written and the spatial and temporal locations of those variables use the pkg/mnc instead (see Section 9.3) which produces netCDF format output.

CPP Flag Name





use READ_MFLDS in “safe” mode (set/check/unset for each file to read); involves more thread synchronization which could slow down multi-threaded run



disable writing of small-overlap size array (to reduce memory size since those S/R do a local copy to 3-D full-size overlap array)

9.3. NetCDF I/O: pkg/mnc

Package pkg/mnc is a set of convenience routines written to expedite the process of creating, appending, and reading netCDF files. NetCDF is an increasingly popular self-describing file format intended primarily for scientific data sets. An extensive collection of netCDF documentation, including a user’s guide, tutorial, FAQ, support archive and other information can be obtained from UCAR’s web site http://www.unidata.ucar.edu/software/netcdf.

Since it is a “wrapper” for netCDF, pkg/mnc depends upon the Fortran-77 interface included with the standard NetCDF v3.x library which is often called libnetcdf.a. Please contact your local systems administrators or email mitgcm-support@mitgcm.org for help building and installing netCDF for your particular platform.

Every effort has been made to allow pkg/mnc and pkg/mdsio (see Section 9.2) to peacefully co-exist. In may cases, the model can read one format and write to the other. This side-by-side functionality can be used to, for instance, help convert pickup files or other data sets between the two formats.

9.3.1. Using pkg/mnc pkg/mnc configuration:

As with all MITgcm packages, pkg/mnc can be turned on or off at compile time using the packages.conf file or the genmake2 -enable=mnc or -disable=mnc switches.

While pkg/mnc is likely to work “as is”, there are a few compile–time constants that may need to be increased for simulations that employ large numbers of tiles within each process. Note that the important quantity is the maximum number of tiles per process. Since MPI configurations tend to distribute large numbers of tiles over relatively large numbers of MPI processes, these constants will rarely need to be increased.

If pkg/mnc runs out of space within its “lookup” tables during a simulation, then it will provide an error message along with a recommendation of which parameter to increase. The parameters are all located within MNC_COMMON.h and the ones that may need to be increased are:






IDs for various low-level entities



IDs (mostly for object sizes)



IDs for the “wrapper” layer

In those rare cases where pkg/mnc “out-of-memory” error messages are encountered, it is a good idea to increase the too-small parameter by a factor of 2–10 in order to avoid wasting time on an iterative compile–test sequence. pkg/mnc Inputs:

Like most MITgcm packages, all of pkg/mnc can be turned on/off at runtime using a single flag in data.pkg:








overall MNC ON/OFF switch

One important MNC–related flag is present in the main data namelist file in the PARM03 section:








use all available output “types”

which specifies that turning on pkg/mnc for a particular type of output should not simultaneously turn off the default output method as it normally does. Usually, this option is only used for debugging purposes since it is inefficient to write output types using both pkg/mnc and pkg/mdsio or ASCII output. This option can also be helpful when transitioning from pkg/mdsio to pkg/mnc since the output can be readily compared.

For run-time configuration, most of the pkg/mnc–related model parameters are contained within a Fortran namelist file called data.mnc. The available parameters currently include:








create a directory for output




output directory name




embed date in the outdir name








use MNC to write pickup files




use MNC to read pickup file




use a directory (path) for input



‘ ’

input directory (or path) name




write snapshot output w/MNC




write pkg/monitor output w/MNC




write pkg/timeave output w/MNC




write pkg/autodiff output w/MNC




max allowable file size (<2GB)




frequency of new file creation (seconds)




read grid quantities using MNC




list pre-defined “types” (debug)

Unlike the older pkg/mdsio method, pkg/mnc has the ability to create or use existing output directories. If either mnc_outdir_date or mnc_outdir_num is .TRUE., then pkg/mnc will try to create directories on a per process basis for its output. This means that a single directory will be created for a non-MPI run and multiple directories (one per MPI process) will be created for an MPI run. This approach was chosen since it works safely on both shared global file systems (such as NFS and AFS) and on local (per-compute-node) file systems. And if both mnc_outdir_date and mnc_outdir_num are .FALSE., then the pkg/mnc package will assume that the directory specified in mnc_outdir_str already exists and will use it. This allows the user to create and specify directories outside of the model.

For input, pkg/mnc can use a single global input directory. This is a just convenience that allows pkg/mnc to gather all of its input files from a path other than the current working directory. As with pkg/mdsio, the default is to use the current working directory.

The flags snapshot_mnc, monitor_mnc, timeave_mnc, and autodiff_mnc allow the user to turn on pkg/mnc for particular “types” of output. If a type is selected, then pkg/mnc will be used for all output that matches that type. This applies to output from the main model and from all of the optional MITgcm packages. Mostly, the names used here correspond to the names used for the output frequencies in the main data namelist file.

The mnc_max_fsize parameter is a convenience added to help users work around common file size limitations. On many computer systems, either the operating system, the file system(s), and/or the netCDF libraries are unable to handle files greater than two or four gigabytes in size. pkg/mnc is able to work within this limitation by creating new files which grow along the netCDF “unlimited” (usually, time) dimension. The default value for this parameter is just slightly less than 2GB which is safe on virtually all operating systems. Essentially, this feature is a way to intelligently and automatically split files output along the unlimited dimension. On systems that support large file sizes, these splits can be readily concatenated (that is, un-done) using tools such as the NetCDF Operators (with ncrcat) which is available at http://nco.sourceforge.net.

Another way users can force the splitting of pkg/mnc files along the time dimension is the mnc_filefreq option. With it, files that contain variables with a temporal dimension can be split at regular intervals based solely upon the model time (specified in seconds). For some problems, this can be much more convenient than splitting based upon file size.

Additional pkg/mnc–related parameters may be contained within each package. Please see the individual packages for descriptions of their use of pkg/mnc. pkg/mnc output:

Depending upon the flags used, pkg/mnc will produce zero or more directories containing one or more netCDF files as output. These files are either mostly or entirely compliant with the netCDF “CF” convention (v1.0) and any conformance issues will be fixed over time. The patterns used for file names are:

  • «BASENAME».«tileNum».nc

  • «BASENAME».«nIter».«faceNum».nc

  • «BASENAME».«nIter».«tileNum».nc

and examples are:

  • grid.t001.nc, grid.t002.nc

  • input.0000072000.f001.nc

  • state.0000000000.t001.nc, surfDiag.0000036000.t001.nc

where «BASENAME» is the name selected to represent a set of variables written together, «nIter» is the current iteration number as specified in the main data namelist input file and written in a zero-filled 10-digit format, «tileNum» is a three-or-more-digit zero-filled and t–prefixed tile number, «faceNum» is a three-or-more-digit zero-filled and f–prefixed face number, and .nc is the file suffix specified by the current netCDF “CF” conventions.

Some example «BASENAME» values are:


contains the variables that describe the various grid constants related to locations, lengths, areas, etc.


contains the variables output at the dumpFreq time frequency

pickup.ckptA, pickup.ckptB

are the “rolling” checkpoint files


contains the time-averaged quantities from the main model

All pkg/mnc output is currently done in a “file-per-tile” fashion since most NetCDF v3.x implementations cannot write safely within MPI or multi-threaded environments. This tiling is done in a global fashion and the tile numbers are appended to the base names as described above. Some scripts to manipulate pkg/mnc output are available at utils/matlab which includes a spatial “assembly” script mnc_assembly.m.

More general manipulations can be performed on netCDF files with the NetCDF Operators (“NCO”) at http://nco.sourceforge.net or with the Climate Data Operators (“CDO”) at https://code.mpimet.mpg.de/projects/cdo.

Unlike the older pkg/mdsio routines, pkg/mnc reads and writes variables on different “grids” depending upon their location in the Arakawa C–grid. The following table provides examples:


C–grid location

# in X

# in Y









U velocity




V velocity








and the intent is two–fold:

  1. For some grid topologies it is impossible to output all quantities using only sNx,sNy arrays for every tile. Two examples of this failure are the missing corners problem for vorticity values on the cubed sphere and the velocity edge values for some open–boundary domains.

  2. Writing quantities located on velocity or vorticity points with the above scheme introduces a very small data redundancy. However, any slight inconvenience is easily offset by the ease with which one can, on every individual tile, interpolate these values to mass points without having to perform an “exchange” (or “halo-filling”) operation to collect the values from neighboring tiles. This makes the most common post–processing operations much easier to implement.

9.3.2. pkg/mnc Troubleshooting Build troubleshooting:

In order to build MITgcm with pkg/mnc enabled, the NetCDF v3.x Fortran-77 (not Fortran-90) library must be available. This library is composed of a single header file (called netcdf.inc) and a single library file (usually called libnetcdf.a) and it must be built with the same compiler with compatible compiler options as the one used to build MITgcm (in other words, while one does not have to build libnetcdf.a with the same exact set of compiler options as MITgcm, one must avoid using some specific different compiler options which are incompatible, i.e., causing a compile-time or run-time error).

For more details concerning the netCDF build and install process, please visit the Getting and Building NetCDF guide which includes an extensive list of known–good netCDF configurations for various platforms. Runtime troubleshooting:

Please be aware of the following:

  • As a safety feature, the pkg/mnc does not, by default, allow pre-existing files to be appended to or overwritten. This is in contrast to the older pkg/mdsio which will, without any warning, overwrite existing files. If MITgcm aborts with an error message about the inability to open or write to a netCDF file, please check first whether you are attempting to overwrite files from a previous run.

  • The constraints placed upon the “unlimited” (or “record”) dimension inherent with NetCDF v3.x make it very inefficient to put variables written at potentially different intervals within the same file. For this reason, pkg/mnc output is split into groups of files which attempt to reflect the nature of their content.

  • On many systems, netCDF has practical file size limits on the order of 2–4GB (the maximium memory addressable with 32bit pointers or pointer differences) due to a lack of operating system, compiler, and/or library support. The latest revisions of NetCDF v3.x have large file support and, on some operating systems, file sizes are only limited by available disk space.

  • There is an 80 character limit to the total length of all file names. This limit includes the directory (or path) since paths and file names are internally appended. Generally, file names will not exceed the limit and paths can usually be shortened using, for example, soft links.

  • pkg/mnc does not (yet) provide a mechanism for reading information from a single “global” file as can be done with pkg/mdsio. This is in progress.

9.3.3. pkg/mnc Internals

pkg/mnc is a two-level convenience library (or “wrapper”) for most of the netCDF Fortran API. Its purpose is to streamline the user interface to netCDF by maintaining internal relations (look-up tables) keyed with strings (or names) and entities such as netCDF files, variables, and attributes.

The two levels of pkg/mnc are:

Upper level

The upper level contains information about two kinds of associations:

grid type

is lookup table indexed with a grid type name. Each grid type name is associated with a number of dimensions, the dimension sizes (one of which may be unlimited), and starting and ending index arrays. The intent is to store all the necessary size and shape information for the Fortran arrays containing MITgcm–style “tile” variables (i.e., a central region surrounded by a variably-sized “halo” or exchange region as shown in Figure 6.5 and Figure 6.6).

variable type

is a lookup table indexed by a variable type name. For each name, the table contains a reference to a grid type for the variable and the names and values of various attributes.

Within the upper level, these associations are not permanently tied to any particular netCDF file. This allows the information to be re-used over multiple file reads and writes.

Lower level

In the lower (or internal) level, associations are stored for netCDF files and many of the entities that they contain including dimensions, variables, and global attributes. All associations are on a per-file basis. Thus, each entity is tied to a unique netCDF file and will be created or destroyed when files are, respectively, opened or closed. pkg/mnc grid–tTypes and variable–types:

As a convenience for users, pkg/mnc includes numerous routines to aid in the writing of data to netCDF format. Probably the biggest convenience is the use of pre-defined “grid types” and “variable types”. These “types” are simply look-up tables that store dimensions, indicies, attributes, and other information that can all be retrieved using a single character string.

The “grid types” are a way of mapping variables within MITgcm to netCDF arrays. Within MITgcm, most spatial variables are defined using 2–D or 3–D arrays with “overlap” regions (see Figure 6.5, a possible vertical index, and Figure 6.6) and tile indicies such as the following “U” velocity:

_RL  uVel (1-OLx:sNx+OLx,1-OLy:sNy+OLy,Nr,nSx,nSy)

as defined in DYNVARS.h.

The grid type is a character string that encodes the presence and types associated with the four possible dimensions. The character string follows the format:


(note the double underscore between «H2» and «V», and «V» and «T») where the terms «H0», «H1», «H2», «V», «T» can be almost any combination of the following:




H0: location

H1: dimensions

H2: halo

V: location

T: level













A example list of all pre-defined combinations is contained in the file pkg/mnc/pre-defined_grids.txt.

The variable type is an association between a variable type name and the following items:



grid type

defines the in-memory arrangement

bi,bj dimensions

tiling indices, if present

and is used by the mnc_cw__[R|W] subroutines for reading and writing variables. Using pkg/mnc: examples

Writing variables to netCDF files can be accomplished in as few as two function calls. The first function call defines a variable type, associates it with a name (character string), and provides additional information about the indicies for the tile (bi,bj) dimensions. The second function call will write the data at, if necessary, the current time level within the model.

Examples of the initialization calls can be found in the file model/src/ini_model_io.F where these function calls:

C     Create MNC definitions for DYNVARS.h variables
      CALL MNC_CW_ADD_VNAME('iter', '-_-_--__-__t', 0,0, myThid)
      CALL MNC_CW_ADD_VATTR_TEXT('iter',1,
     &     'long_name','iteration_count', myThid)

      CALL MNC_CW_ADD_VNAME('model_time', '-_-_--__-__t', 0,0, myThid)
      CALL MNC_CW_ADD_VATTR_TEXT('model_time',1,
     &     'long_name','Model Time', myThid)
      CALL MNC_CW_ADD_VATTR_TEXT('model_time',1,'units','s', myThid)

      CALL MNC_CW_ADD_VNAME('U', 'U_xy_Hn__C__t', 4,5, myThid)
      CALL MNC_CW_ADD_VATTR_TEXT('U',1,'units','m/s', myThid)
     &     'coordinates','XU YU RC iter', myThid)

      CALL MNC_CW_ADD_VNAME('T', 'Cen_xy_Hn__C__t', 4,5, myThid)
      CALL MNC_CW_ADD_VATTR_TEXT('T',1,'units','degC', myThid)
      CALL MNC_CW_ADD_VATTR_TEXT('T',1,'long_name',
     &     'potential_temperature', myThid)
     &     'coordinates','XC YC RC iter', myThid)

initialize four VNAMEs and add one or more netCDF attributes to each.

The four variables defined above are subsequently written at specific time steps within model/src/write_state.F using the function calls:

C       Write dynvars using the MNC package
        CALL MNC_CW_SET_UDIM('state', -1, myThid)
        CALL MNC_CW_I_W('I','state',0,0,'iter', myIter, myThid)
        CALL MNC_CW_SET_UDIM('state', 0, myThid)
        CALL MNC_CW_RL_W('D','state',0,0,'model_time',myTime, myThid)
        CALL MNC_CW_RL_W('D','state',0,0,'U', uVel, myThid)
        CALL MNC_CW_RL_W('D','state',0,0,'T', theta, myThid)

While it is easiest to write variables within typical 2-D and 3-D fields where all data is known at a given time, it is also possible to write fields where only a portion (e.g., a “slab” or “slice”) is known at a given instant. An example is provided within pkg/mom_vecinv/mom_vecinv.F where an offset vector is used:

    IF (useMNC .AND. snapshot_mnc) THEN
      CALL MNC_CW_RL_W_OFFSET('D','mom_vi',bi,bj, 'fV', uCf,
&          offsets, myThid)
      CALL MNC_CW_RL_W_OFFSET('D','mom_vi',bi,bj, 'fU', vCf,
&          offsets, myThid)

to write a 3-D field one depth slice at a time.

Each element in the offset vector corresponds (in order) to the dimensions of the “full” (or virtual) array and specifies which are known at the time of the call. A zero within the offset array means that all values along that dimension are available while a positive integer means that only values along that index of the dimension are available. In all cases, the matrix passed is assumed to start (that is, have an in-memory structure) coinciding with the start of the specified slice. Thus, using this offset array mechanism, a slice can be written along any single dimension or combinations of dimensions.

9.4. Monitor: Simulation State Monitoring Toolkit

9.4.1. Introduction

pkg/monitor is primarily intended as a convenient method for calculating and writing the following statistics:

  • minimum

  • maximum

  • mean

  • standard deviation

for spatially distributed fields. By default, pkg/monitor output is sent to the “standard output” channel where it appears as ASCII text containing a %MON string such as this example:

(PID.TID 0000.0001) %MON time_tsnumber      =                     3
(PID.TID 0000.0001) %MON time_secondsf      =   3.6000000000000E+03
(PID.TID 0000.0001) %MON dynstat_eta_max    =   1.0025466645951E-03
(PID.TID 0000.0001) %MON dynstat_eta_min    =  -1.0008899950901E-03
(PID.TID 0000.0001) %MON dynstat_eta_mean   =   2.1037438449350E-14
(PID.TID 0000.0001) %MON dynstat_eta_sd     =   5.0985228723396E-04
(PID.TID 0000.0001) %MON dynstat_eta_del2   =   3.5216706549525E-07
(PID.TID 0000.0001) %MON dynstat_uvel_max   =   3.7594045977254E-05
(PID.TID 0000.0001) %MON dynstat_uvel_min   =  -2.8264287531564E-05
(PID.TID 0000.0001) %MON dynstat_uvel_mean  =   9.1369201945671E-06
(PID.TID 0000.0001) %MON dynstat_uvel_sd    =   1.6868439193567E-05
(PID.TID 0000.0001) %MON dynstat_uvel_del2  =   8.4315445301916E-08

pkg/monitor text can be readily parsed by the testreport script to determine, somewhat crudely but quickly, how similar the output from two experiments are when run on different platforms or before/after code changes.

pkg/monitor output can also be useful for quickly diagnosing practical problems such as CFL limitations, model progress (through iteration counts), and behavior within some packages that use it.

9.4.2. Using pkg/monitor

As with most packages, pkg/monitor can be turned on or off at compile and/or run times using the packages.conf and data.pkg files.

The monitor output can be sent to the standard output channel, to an pkg/mnc–generated file, or to both simultaneously. For pkg/mnc output, the flag monitor_mnc=.TRUE. should be set within the data.mnc file. For output to both ASCII and pkg/mnc, the flag outputTypesInclusive=.TRUE. should be set within the PARM03 section of the main data file. It should be noted that the outputTypesInclusive flag will make ALL kinds of output (that is, everything written by pkg/mdsio, pkg/mnc, and pkg/monitor) simultaneously active so it should be used only with caution -– and perhaps only for debugging purposes.

CPP Flag Name





disable use of hFacZ

9.5. Grid Generation

The horizontal discretizations within MITgcm have been written to work with many different grid types including:

  • cartesian coordinates

  • spherical polar (“latitude-longitude”) coordinates

  • general curvilinear orthogonal coordinates

The last of these, especially when combined with the domain decomposition capabilities of MITgcm, allows a great degree of grid flexibility. To date, general curvilinear orthogonal coordinates have been used extensively in conjunction with so-called “cubed sphere” grids. However, it is important to observe that cubed sphere arrangements are only one example of what is possible with domain-decomposed logically rectangular regions each containing curvilinear orthogonal coordinate systems. Much more sophisticated domains can be imagined and constructed.

In order to explore the possibilities of domain-decomposed curvilinear orthogonal coordinate systems, a suite of grid generation software called “SPGrid” (for SPherical Gridding) has been developed. SPGrid is a relatively new facility and papers detailing its algorithms are in preparation. Although SPGrid is new and rapidly developing, it has already demonstrated the ability to generate some useful and interesting grids.

This section provides a very brief introduction to SPGrid and shows some early results. For further information, please contact the MITgcm support list MITgcm-support@mitgcm.org.

9.5.1. Using SPGrid

The SPGrid software is not a single program. Rather, it is a collection of C++ code and MATLAB scripts that can be used as a framework or library for grid generation and manipulation. Currently, grid creation is accomplished by either directly running MATLAB scripts or by writing a C++ “driver” program. The MATLAB scripts are suitable for grids composed of a single “face” (that is, a single logically rectangular region on the surface of a sphere). The C++ driver programs are appropriate for grids composed of multiple connected logically rectangular patches. Each driver program is written to specify the shape and connectivity of tiles and the preferred grid density (that is, the number of grid cells in each logical direction) and edge locations of the cells where they meet the edges of each face. The driver programs pass this information to the SPGrid library, which generates the actual grid and produces the output files that describe it.

Currently, driver programs are available for a few examples including cubes, “lat-lon caps” (cube topologies that have conformal caps at the poles and are exactly lat-lon channels for the remainder of the domain), and some simple “embedded” regions that are meant to be used within typical cubes or traditional lat-lon grids.

To create new grids, one may start with an existing driver program and modify it to describe a domain that has a different arrangement. The number, location, size, and connectivity of grid “faces” (the name used for the logically rectangular regions) can be readily changed. Further, the number of grid cells within faces and the location of the grid cells at the face edges can also be specified. SPGrid requirements

The following programs and libraries are required to build and/or run the SPGrid suite:

  • MATLAB is a run-time requirement since many of the generation algorithms have been written as MATLAB scripts.

  • The Geometric Tools Engine (a C++ library) is needed for the main “driver” code.

  • The netCDF library is needed for file I/O.

  • The Boost serialization library is also used for I/O:

  • a typical Linux/Unix build environment including the make utility (preferably GNU Make) and a C++ compiler (SPGrid was developed with g++ v4.x). Obtaining SPGrid

The latest version can be obtained from: Building SPGrid

The procedure for building is similar to many open source projects:

tar -xf spgrid-0.9.4.tar.gz
cd spgrid-0.9.4
export CPPFLAGS="-I/usr/include/netcdf-3"
export LDFLAGS="-L/usr/lib/netcdf-3"

where the CPPFLAGS and LDFLAGS environment variables can be edited to reflect the locations of all the necessary dependencies. SPGrid is known to work on Fedora Core Linux (versions 4 and 5) and is likely to work on most any Linux distribution that provides the needed dependencies. Running SPGrid

Within the src sub-directory, various example driver programs exist. These examples describe small, simple domains and can generate the input files (formatted as either binary *.mitgrid or netCDF) used by MITgcm.

One such example is called SpF_test_cube_cap and it can be run with the following sequence of commands:

cd spgrid-0.9.4/src
make SpF_test_cube_cap
mkdir SpF_test_cube_cap.d
( cd SpF_test_cube_cap.d && ln -s ../../scripts/*.m . )

which should create a series of output files:


where the grid_.mitgrid and grid_.nc files contain the grid information in binary and netCDF formats and the std_topology.nc file contains the information describing the connectivity (both edge–edge and corner–corner contacts) between all the faces.

9.5.2. Example Grids

The following grids are various examples created with SPGrid.

9.6. Pre– and Post–Processing Scripts and Utilities

There are numerous tools for pre-processing data, converting model output and analysis written in MATLAB, Fortran (f77 and f90) and perl. As yet they remain undocumented although many are self-documenting (MATLAB routines have “help” written into them).

Here we’ll summarize what is available but this is an ever growing resource so this may not cover everything that is out there:

9.6.1. Utilities Supplied With the Model

We supply some basic scripts with the model to facilitate conversion or reading of data into analysis software. utils/scripts

In the directory utils/scripts, joinds and joinmds are perl scripts used to joining multi-part files created by MITgcm. Use joinmds. You will only need joinds if you are working with output older than two years (prior to c23). utils/matlab

In the directory utils/matlab you will find several MATLAB scripts (.m files). The principle script is rdmds.m, used for reading the multi-part model output files into MATLAB . Place the scripts in your MATLAB path or change the path appropriately, then at the MATLAB prompt type:

>> help rdmds

to get help on how to use rdmds.

Another useful script scans the terminal output file for pkg/monitor information.

Most other scripts are for working in the curvilinear coordinate systems, and as yet are unpublished and undocumented. pkg/mnc utils

The following scripts and utilities have been written to help manipulate netCDF files:

Tile Assembly:

A MATLAB script mnc_assembly.m is available for spatially “assembling” pkg/mnc output. A convenience wrapper script called gluemnc.m is also provided. Please use the MATLAB help facility for more information.


As MITgcm evolves to handle more complicated domains and topologies, a suite of matlab tools is being written to more gracefully handle the model files. This suite is called “gmt” which refers to “generalized model topology” pre-/post-processing. Currently, this directory contains a MATLAB script gmt/rdnctiles.m that is able to read netCDF files for any domain. Additional scripts are being created that will work with these fields on a per-tile basis.

9.6.2. Pre-Processing Software

There is a suite of pre-processing software for interpolating bathymetry and forcing data, written by Adcroft and Biastoch. At some point, these will be made available for download. If you are in need of such software, contact one of them.

9.7. Potential Vorticity Matlab Toolbox

Author: Guillaume Maze

9.7.1. Introduction

This section of the documentation describes a MATLAB package that aims to provide useful routines to compute vorticity fields (relative, potential and planetary) and its related components. This is an offline computation. It was developed to be used in mode water studies, so that it comes with other related routines, in particular ones computing surface vertical potential vorticity fluxes.


This toolbox was developed in 2006 for the CLIMODE project. The toolbox routines are available on this archived repository.

9.7.2. Equations Potential vorticity

The package computes the three components of the relative vorticity, \(\boldsymbol{\omega}\), defined by:

(9.1)\[\begin{split}\begin{aligned} \boldsymbol{\omega} &= \nabla \times {\bf U} = \begin{pmatrix} \omega_x\\ \omega_y\\ \zeta \end{pmatrix} \simeq \begin{pmatrix} -\partial_z v\\ -\partial_z u\\ \partial_x v - \partial_y u \end{pmatrix} \end{aligned}\end{split}\]

where we omitted the vertical velocity component (as done throughout the package).

The package then computes the potential vorticity as:

(9.2)\[\begin{split}\begin{aligned} Q &= -\frac{1}{\rho} \boldsymbol{\omega} \cdot \nabla \sigma_\theta\\ &= -\frac{1}{\rho}\left(\omega_x \frac{\partial \sigma_\theta}{\partial x} + \omega_y \frac{\partial \sigma_\theta}{\partial y} + \left(f + \zeta\right) \frac{\partial \sigma_\theta}{\partial z}\right) \end{aligned}\end{split}\]

where \(\rho\) is the density, \(\sigma_\theta\) is the potential density (both eventually computed by the package) and \(f\) is the Coriolis parameter.

The package is also able to compute the simpler planetary vorticity as:

(9.3)\[\begin{aligned} Q_{\rm spl} & = -\frac{f}{\rho}\frac{\sigma_\theta}{\partial z} \end{aligned}\] Surface vertical potential vorticity fluxes

These quantities are useful in mode water studies because of the impermeability theorem which states that for a given potential density layer (embedding a mode water), the integrated PV only changes through surface input/output.

Vertical PV fluxes due to diabatic and frictional processes are given by:

(9.4)\[J^B_z = -\frac{f}{h}\left( \frac{\alpha Q_{\rm net}}{\text{C}_p}-\rho_0 \beta S_{\rm net}\right)\]
(9.5)\[J^F_z = \frac{1}{\rho\delta_e} (\hat{\boldsymbol{k}} \times \boldsymbol{\tau}) \cdot \nabla \sigma_m\]

These components can be computed with the package. Details on the variables definition and the way these fluxes are derived can be found in Section 9.7.5.

We now give some simple explanations about these fluxes and how they can reduce the PV value of an oceanic potential density layer. Diabatic process

Let’s take the PV flux due to surface buoyancy forcing from (9.4) and simplify it as:

\[\begin{aligned} J^B_z \simeq -\frac{\alpha f}{h \text{C}_p} Q_{\rm net}\end{aligned}\]

When the net surface heat flux \(Q_{\rm net}\) is upward, i.e., negative and cooling the ocean (buoyancy loss), surface density will increase, triggering mixing which reduces the stratification and then the PV.

\[\begin{split}\begin{aligned} Q_{\rm net} &< 0 \phantom{WWW}\text{(upward, cooling)} \\ J^B_z &> 0 \phantom{WWW}\text{(upward)} \\ -\rho^{-1} \nabla \cdot J^B_z &< 0 \phantom{WWW}\text{(PV flux divergence)} \\ PV &\searrow \phantom{WWWi}\text{where } Q_{\rm net}<0 \end{aligned}\end{split}\] Frictional process: “Down-front” wind-stress

Now let’s take the PV flux due to the “wind-driven buoyancy flux” from (9.5) and simplify it as:

\[\begin{split}\begin{aligned} J^F_z &= \frac{1}{\rho\delta_e} \left( \tau_x\frac{\partial \sigma}{\partial y} - \tau_y\frac{\partial \sigma}{\partial x} \right) \\ &\simeq \frac{1}{\rho\delta_e} \tau_x\frac{\partial \sigma}{\partial y} \end{aligned}\end{split}\]

When the wind is blowing from the east above the Gulf Stream (a region of high meridional density gradient), it induces an advection of dense water from the northern side of the Gulf Stream to the southern side through Ekman currents. Then, it induces a “wind-driven” buoyancy lost and mixing which reduces the stratification and the PV.

\[\begin{split}\begin{aligned} (\hat{\boldsymbol{k}} \times \boldsymbol{\tau}) \cdot \nabla \sigma &> 0 \phantom{WWW}\text{("Down-front" wind)} \\ J^F_z &> 0 \phantom{WWW}\text{(upward)} \\ -\rho^{-1} \nabla \cdot J^F_z &< 0 \phantom{WWW}\text{(PV flux divergence)} \\ PV &\searrow \phantom{WWW}\text{where } (\hat{\boldsymbol{k}} \times \boldsymbol{\tau}) \cdot \nabla \sigma>0 \end{aligned}\end{split}\] Diabatic versus frictional processes

A recent debate in the community arose about the relative role of these processes. Taking the ratio of (9.4) and (9.5) leads to:

\[\begin{split}\begin{aligned} \frac{J^F_z}{J^B_z} & = \frac{ \dfrac{1}{\rho\delta_e} (\hat{\boldsymbol{k}} \times \boldsymbol{\tau}) \cdot \nabla \sigma } {-\dfrac{f}{h}\left( \dfrac{\alpha Q_{\rm net}}{\text{C}_p} - \rho_0 \beta S_{\rm net}\right)} \\ &\simeq \frac{Q_{\rm Ek}/\delta_e}{Q_{\rm net}/h} \nonumber \end{aligned}\end{split}\]

where appears the lateral heat flux induced by Ekman currents:

\[\begin{split}\begin{aligned} Q_{\rm Ek} & = -\frac{\text{C}_p}{\alpha\rho f} (\hat{\boldsymbol{k}} \times \boldsymbol{\tau}) \cdot \nabla \sigma \nonumber \\ & = \frac{\text{C}_p}{\alpha}\delta_e \vec{\bf u}_{\rm Ek} \cdot \nabla \sigma\end{aligned}\end{split}\]

which can be computed with the package. In the aim of comparing both processes, it will be useful to plot surface net and lateral Ekman-induced heat fluxes together with PV fluxes.

9.7.3. Key routines

  • A_compute_potential_density.m: Compute the potential density field. Requires the potential temperature and salinity (either total or anomalous) and produces one output file with the potential density field (file prefix is SIGMATHETA). The routine uses utils/matlab/densjmd95.m, a Matlab counterpart of the MITgcm built-in function to compute the density.

  • B_compute_relative_vorticity.m: Compute the three components of the relative vorticity defined in (9.1). Requires the two horizontal velocity components and produces three output files with the three components (files prefix are OMEGAX, OMEGAY and ZETA).

  • C_compute_potential_vorticity.m: Compute the potential vorticity without the negative ratio by the density. Two options are possible in order to compute either the full component (term into parenthesis in (9.2) or the planetary component (\(f\partial_z\sigma_\theta\) in (9.3)). Requires the relative vorticity components and the potential density, and produces one output file with the potential vorticity (file prefix is PV for the full term and splPV for the planetary component).

  • D_compute_potential_vorticity.m: Load the field computed with and divide it by \(-\rho\) to obtain the correct potential vorticity. Require the density field and after loading, overwrite the file with prefix PV or splPV.

  • compute_density.m: Compute the density \(\rho\) from the potential temperature and the salinity fields.

  • compute_JFz.m: Compute the surface vertical PV flux due to frictional processes. Requires the wind stress components, density, potential density and Ekman layer depth (all of them, except the wind stress, may be computed with the package), and produces one output file with the PV flux \(J^F_z\) (see (9.5) and with JFz as a prefix.

  • compute_JBz.m: Compute the surface vertical PV flux due to diabatic processes as:

    \[\begin{aligned} J^B_z & = -\frac{f}{h}\frac{\alpha Q_{\rm net}}{\text{C}_p} \end{aligned}\]

    which is a simplified version of the full expression given in (9.4). Requires the net surface heat flux and the mixed layer depth (of which an estimation can be computed with the package), and produces one output file with the PV flux \(J^B_z\) and with JBz as a prefix.

  • compute_QEk.m: Compute the horizontal heat flux due to Ekman currents from the PV flux induced by frictional forces as:

    \[\begin{aligned} Q_{\rm Ek} & = - \frac{\text{C}_p \delta_e}{\alpha f}J^F_z\end{aligned}\]

    Requires the PV flux due to frictional forces and the Ekman layer depth, and produces one output with the heat flux and with QEk as a prefix.

  • eg_main_getPV: A complete example of how to set up a master routine able to compute everything from the package.

9.7.4. Technical details File name

A file name is formed by three parameters which need to be set up as global variables in MATLAB before running any routines. They are:

  • the prefix, i.e., the variable name (netcdf_UVEL for example). This parameter is specified in the help section of all diagnostic routines.

  • netcdf_domain: the geographical domain.

  • netcdf_suff: the netcdf extension (nc or cdf for example).

Then, for example, if the calling MATLAB routine had set up:

global netcdf_THETA netcdf_SALTanom netcdf_domain netcdf_suff
netcdf_THETA    = 'THETA';
netcdf_SALTanom = 'SALT';
netcdf_domain   = 'north_atlantic';
netcdf_suff     = 'nc';

the routine A_compute_potential_density.m to compute the potential density field, will look for the files:


and the output file will automatically be: SIGMATHETA.north_atlantic.nc.

Otherwise indicated, output file prefix cannot be changed. Path to file

All diagnostic routines look for input files in a subdirectory (relative to the MATLAB routine directory) called ./netcdf-files, which in turn is supposed to contain subdirectories for each set of fields. For example, computing the potential density for the timestep 12H00 02/03/2005 will require a subdirectory with the potential temperature and salinity files like:


The output file SIGMATHETA.north\_atlantic.nc will be created in ./netcdf-files/200501031200/. All diagnostic routines take as argument the name of the timestep subdirectory into ./netcdf-files. Grids

With MITgcm numerical outputs, velocity and tracer fields may not be defined on the same grid. Usually, UVEL and VVEL are defined on a C-grid but when interpolated from a cube-sphere simulation they are defined on a A-grid. When it is needed, routines allow to set up a global variable which define the grid to use.

9.7.5. Notes on the flux form of the PV equation and vertical PV fluxes Flux form of the PV equation

The conservative flux form of the potential vorticity equation is:

(9.6)\[\begin{aligned} \frac{\partial \rho Q}{\partial t} + \nabla \cdot \vec{\bf J} & = 0 \end{aligned}\]

where the potential vorticity \(Q\) is given by (9.2).

The generalized flux vector of potential vorticity is:

\[\begin{aligned} \vec{\bf J} & = \rho Q \vec{\bf u} + \vec{\bf N}_Q \end{aligned}\]

which allows to rewrite (9.6) as:

(9.7)\[\begin{aligned} \frac{DQ}{dt} & = - \frac{1}{\rho} \nabla \cdot \vec{\bf N}_Q \end{aligned}\]

where the non-advective PV flux \(\vec{\bf N}_Q\) is given by:

(9.8)\[\begin{aligned} \vec{\bf N}_Q & = -\frac{\rho_0}{g}B \vec{\boldsymbol{\omega}}_a + \vec{\bf F} \times \nabla \sigma_\theta \end{aligned}\]

Its first component is linked to the buoyancy forcing:

\[\begin{aligned} B & = -\frac{g}{\rho_o}\frac{D \sigma_\theta}{dt} \end{aligned}\]

and the second one to the non-conservative body forces per unit mass:

\[\begin{aligned} \vec{\bf F} & = \frac{D \vec{\bf u}}{Dt} + 2 \vec{\boldsymbol{\Omega}} \times \vec{\bf u} + \nabla p \end{aligned}\]

Note that introducing \(B\) into (9.8) yields:

\[\begin{aligned} \vec{\bf N}_Q & = \boldsymbol{\omega}_a \frac{D \sigma_\theta}{dt} + \vec{\bf F} \times \nabla \sigma_\theta \end{aligned}\] Determining the PV flux at the ocean’s surface

In the context of mode water study, we are particularly interested in how the PV may be reduced by surface PV fluxes because a mode water is characterized by a low PV value. Considering the volume limited by two \(iso-\sigma_\theta\), PV flux is limited to surface processes and then vertical component of \(\vec{\bf N}_Q\). It is supposed that \(B\) and \(\vec{\bf F}\) will only be non-zero in the mixed layer (of depth \(h\) and variable density \(\sigma_m\)) exposed to mechanical forcing by the wind and buoyancy fluxes through the ocean’s surface.

Given the assumption of a mechanical forcing confined to a thin surface Ekman layer (of depth \(\delta_e\), eventually computed by the package) and of hydrostatic and geostrophic balances, we can write:

(9.9)\[\begin{split}\begin{aligned} \vec{\bf u}_g & = \frac{1}{\rho f} \hat{\boldsymbol{k}} \times \nabla p \\ \frac{\partial p_m}{\partial z} & = -\sigma_m g \\ \frac{\partial \sigma_m}{\partial t} + \vec{\bf u}_m \cdot \nabla \sigma_m & = -\frac{\rho_0}{g}B \end{aligned}\end{split}\]


(9.10)\[\begin{aligned} \vec{\bf u}_m & = \vec{\bf u}_g + \vec{\bf u}_{\rm Ek} + o(R_o) \end{aligned}\]

is the full velocity field composed of the geostrophic current \(\vec{\bf u}_g\) and the Ekman drift:

(9.11)\[\begin{aligned} \vec{\bf u}_{\rm Ek} & = -\frac{1}{\rho f} \hat{\boldsymbol{k}} \times \frac{\partial \boldsymbol{\tau}}{\partial z} \end{aligned}\]

(where \(\boldsymbol{\tau}\) is the wind stress) and last by other ageostrophic components of \(o(R_o)\) which are neglected.

Partitioning the buoyancy forcing as:

(9.12)\[\begin{aligned} B & = B_g + B_{\rm Ek} \end{aligned}\]

and using (9.10) and (9.11), (9.9) becomes:

\[\begin{aligned} \frac{\partial \sigma_m}{\partial t} + \vec{\bf u}_g \cdot \nabla \sigma_m & = -\frac{\rho_0}{g} B_g \end{aligned}\]

revealing the “wind-driven buoyancy forcing”:

\[\begin{aligned} B_{\rm Ek} & = \frac{g}{\rho_0}\frac{1}{\rho f}\left(\hat{\boldsymbol{k}} \times \frac{\partial \boldsymbol{\tau}}{\partial z}\right)\cdot \nabla \sigma_m \end{aligned}\]

Note that since:

\[\begin{aligned} \frac{\partial B_g}{\partial z} & = \frac{\partial}{\partial z}\left(-\frac{g}{\rho_0} \vec{\bf u}_g \cdot \nabla \sigma_m\right) = -\frac{g}{\rho_0}\frac{\partial \vec{\bf u}_g}{\partial z} \cdot \nabla \sigma_m = 0 \end{aligned}\]

\(B_g\) must be uniform throughout the depth of the mixed layer and then being related to the surface buoyancy flux by integrating (9.12) through the mixed layer:

(9.13)\[\begin{aligned} \int_{-h}^0 B\,dz &= h B_g + \int_{-h}^0 B_{\rm Ek}\,dz = \mathcal{B}_{\rm in} \end{aligned}\]

where \(\mathcal{B}_{\rm in}\) is the vertically integrated surface buoyancy (in)flux:

(9.14)\[\begin{aligned} \mathcal{B}_{\rm in} & = \frac{g}{\rho_o}\left( \frac{\alpha Q_{\rm net}}{\text{C}_p} - \rho_0\beta S_{\rm net}\right) \end{aligned}\]

with \(\alpha\simeq 2.5\times10^{-4}\, \text{K}^{-1}\) the thermal expansion coefficient (computed by the package otherwise), \(\text{C}_p=4187 \text{ J kg}^{-1}\text{K}^{-1}\) the specific heat of seawater, \(Q_{\rm net}\text{ (W m$^{-2}$)}\) the net heat surface flux (positive downward, warming the ocean), \(\beta\text{ ((g/kg)$^{-1}$)}\) the saline contraction coefficient, and \(S_{\rm net}=S*(E-P)\text{ ((g/kg) m s$^{-1}$)}\) the net freshwater surface flux with \(S\text{ (g/kg)}\) the surface salinity and \((E-P)\text{ (m s$^{-1}$)}\) the fresh water flux.

Introducing the body force in the Ekman layer:

\[\begin{aligned} F_z & = \frac{1}{\rho}\frac{\partial \boldsymbol{\tau}}{\partial z} \end{aligned}\]

the vertical component of (9.8) is:

\[\begin{split}\begin{aligned} \vec{\bf N}_Q \cdot \hat{\boldsymbol{k}} &= -\frac{\rho_0}{g}(B_g+B_{\rm Ek}) \omega_z + \frac{1}{\rho} \left( \frac{\partial \boldsymbol{\tau}}{\partial z} \times \nabla \sigma_\theta \right) \cdot \hat{\boldsymbol{k}} \\ &= -\frac{\rho_0}{g}B_g\omega_z -\frac{\rho_0}{g} \left[ \frac{g}{\rho_0}\frac{1}{\rho f} \left( \hat{\boldsymbol{k}} \times \frac{\partial \boldsymbol{\tau}}{\partial z} \right) \cdot \nabla \sigma_m \right]\omega_z + \frac{1}{\rho} \left( \frac{\partial \boldsymbol{\tau}}{\partial z}\times \nabla \sigma_\theta \right)\cdot\hat{\boldsymbol{k}}\\ &= -\frac{\rho_0}{g}B_g\omega_z + \left(1-\frac{\omega_z}{f}\right)\left(\frac{1}{\rho}\frac{\partial \boldsymbol{\tau}}{\partial z} \times \nabla \sigma_\theta \right)\cdot\hat{\boldsymbol{k}}\end{aligned}\end{split}\]

and given the assumption that \(\omega_z\simeq f\), the second term vanishes and we obtain:

(9.15)\[\begin{aligned} \vec{\bf N}_Q \cdot \hat{\boldsymbol{k}} & = -\frac{\rho_0}{g}f B_g . \end{aligned}\]

Note that the wind-stress forcing does not appear explicitly here but is implicit in \(B_g\) through (9.13): the buoyancy forcing \(B_g\) is determined by the difference between the integrated surface buoyancy flux \(\mathcal{B}_{\rm in}\) and the integrated “wind-driven buoyancy forcing”:

\[\begin{split}\begin{aligned} B_g &= \frac{1}{h}\left( \mathcal{B}_{\rm in} - \int_{-h}^0B_{\rm Ek}dz \right) \\ &= \frac{1}{h}\frac{g}{\rho_0}\left( \frac{\alpha Q_{\rm net}}{\text{C}_p} - \rho_0 \beta S_{\rm net}\right) - \frac{1}{h}\int_{-h}^0 \frac{g}{\rho_0}\frac{1}{\rho f}\left (\hat{\boldsymbol{k}}\times \frac{\partial \boldsymbol{\tau}}{\partial z} \right) \cdot \nabla \sigma_m dz \\ &= \frac{1}{h}\frac{g}{\rho_0}\left( \frac{\alpha Q_{\rm net}}{\text{C}_p} - \rho_0 \beta S_{\rm net}\right) - \frac{g}{\rho_0}\frac{1}{\rho f \delta_e}\left (\hat{\boldsymbol{k}}\times \boldsymbol{\tau} \right) \cdot \nabla \sigma_m\end{aligned}\end{split}\]

Finally, from (9.8), the vertical surface flux of PV may be written as:

\[\begin{split}\begin{aligned} \vec{\bf N}_Q \cdot \hat{\boldsymbol{k}} &= J^B_z + J^F_z \\ J^B_z &= -\frac{f}{h}\left( \frac{\alpha Q_{\rm net}}{\text{C}_p}-\rho_0 \beta S_{\rm net}\right) \\ J^F_z &= \frac{1}{\rho\delta_e} (\hat{\boldsymbol{k}}\times \boldsymbol{\tau}) \cdot \nabla \sigma_m \end{aligned}\end{split}\]

9.8. pkg/flt – Simulation of float / parcel displacements

9.8.1. Introduction

This section describes the pkg/flt package and is largely based on the original documentation provided by Arne Biastoch and Alistair Adcroft circa 2001. pkg/flt computes float trajectories and simulates the behavior of profiling floats during a model run. Profiling floats (e.g.) Argo) typically drift at depth and go back to the surface at pre-defined time intervals. However, pkg/flt can also simulate observing devices such as non-profiling floats or surface drifters.

The package’s core functionalities are operated by the flt_main call in forward_step (see below for details). Checkpointing is supported via flt_write_pickup called in packages_write_pickup.

Time-stepping of float locations is based on a second- or fourth-order Runga-Kutta scheme (Press et al., 1992, Numerical Recipes). Velocities and positions are interpolated between grid points to the simulated device location, and various types of noise can be added the simulated displacements. Spatial interpolation is bilinear close to boundaries and otherwise a polynomial interpolation. Float positions are expressed in local grid index space.

9.8.2. Compile-time options in FLT_OPTIONS.h

CPP Flag Name





allow three-dimensional float displacements



use alternative method of adding random noise



add noise also to the vertical velocity of 3D floats



revert to old second-order Runge-Kutta



prevent floats to re-enter the opposite side of a periodic domain



prevent floats to re-enter the opposite side of a periodic domain



allow experimentation with pkg/flt + exch2 despite incomplete implementation

9.8.3. Compile-time parameters in FLT_SIZE.h include:

parameter (max_npart_tile = 300)

is the maximum number of floats per tile. Should be smaller than the total number of floats when running on a parallel environment but as small as possible to avoid too large arrays. The model will stop if the number of floats per tile exceeds max_npart_tile at any time.

parameter (max_npart_exch = 50)

is the maximum number of floats per tile that can be exchanged with other tiles to one side (there are 4 arrays) in one timestep. Should be generally small because only few floats leave the tile exactly at the same time.

9.8.4. Run-time options in data.flt include:


is the time interval in seconds to sample float position and dynamic variables (T,S,U,V,Eta). To capture the whole profile cycle of a PALACE float this has to be at least as small as the shortest surface time


is the time interval in seconds to sample a whole profile of T,S,U,V (as well as positions and Eta). This has to chosen at least as small as the shortest profiling interval.


If FLT_NOISE is defined then this is the amplitude that is added to the advection velocity by the random number generator.


is the base filename of the float positions without tile information and ending (e.g. float_pos)


selects variables to output following float trajectories (=0 : none ; =1 : position only ; =2 : +p,u,v,t,s)


selects variables to output when floats profile (=0 : none ; =1 : position only ; =2 : +p,u,v,t,s)


is equal to deltaTClock by default


is the time step when floats are initialized


converts float initial positions to local, fractional indices (.TRUE. by default)

Notes: flt_int_prof is the time between getting profiles, not the the return cycle of the float to the surface. The latter can be specified individually for every float. Because the mechanism for returning to the surface is called in the profiling routine flt_int_prof has to be the minimum of all iup(max_npart). The subsampling of profiles can be done later in the analysis.

Notes: All profiling intervals have to be an integer multiple of flt_int_prof. The profile is always taken over the whole water column. For example, let’s assume that one wants a first set of floats with 5 days profiling interval and 24 hours surface time, and another one with 10 days profiling interval and 12 hours surface time. To capture all of the floats motions, one then would have to set flt_int_traj=43200 and flt_int_prof=432000.

9.8.5. Input Files

If nIter0.EQ.FLT_Iter0 then flt_init_varia first looks for a global file (e.g. float_pos.data). If that file does not exists then flt_init_varia looks for local files (e.g. float_pos.001.001.data, etc.) or for local pickup files that have been generated during a previous model run (e.g. pickup_flt.ckptA.001.001.data, etc.).

The first line of these input file provides:

  • the number of floats on that tile in the first record

  • the total number of floats in the sixth record

Notes: when using a global file at first-time initialization both fields should be the same.

Afterwards the input files contain one 9-element double-precision record for each float:

npart   A unique float identifier (1,2,3,...)
tstart  start date of integration of float (in s)
  - If tstart=-1 floats are integrated right from the beginning
xpart   x position of float (in units of XC)
ypart   y position of float (in units of YC)
kpart   actual vertical level of float
kfloat  target level of float
       - should be the same as kpart at the beginning
iup     flag if the float
  - should profile   ( >  0 = return cycle (in s) to surface)
  - remain at depth  ( =  0 )
  - is a 3D float    ( = -1 ).
  - should be advected WITHOUT additional noise ( = -2 ).
    (This implies that the float is non-profiling)
  - is a mooring     ( = -3 ), i.e. the float is not advected
itop    time of float the surface (in s)
tend    end date of integration of float (in s)
  - If tend=-1 floats are integrated till the end of the integration

Notes: an example how to write a float file (write_float.F) is included in the verification experiment documented below.

9.8.6. Output Files

The output consists of 3 sets of local files:

  • pickup_flt* : last positions of floats that can be used for restart

  • float_trajectories* : trajectories of floats and actual values at depth

  • float_profiles* : profiles throughout the whole water column

9.8.7. Verification Experiment

The verification experiment is based on exp4 (flow over a Gaussian in a channel). The two main difference is that an additional wind forcing was introduced to speed up the currents.

A few utilities are included that were supposedly used to prepare input for pkg/flt and / or visualize its output:


9.8.8. Algorithm details

A summary of what flt_main.F currently does is as follows:


A summary of included fortran files is provided inside flt_main.F:

Main Routines:
C     o flt_main       - Integrates the floats forward and stores
C                        positions and vertical profiles at specific
C                        time intervals.
C     o flt_readparms  - Read parameter file
C     o flt_init_fixed - Initialise fixed
C     o flt_init_varia - Initialise the floats
C     o flt_restart    - Writes restart data to file (=> renamed: flt_write_pickup)
C     Second Level Subroutines:
C     o flt_runga2     - Second order Runga-Kutta inetgration (default)
C     o flt_exchg      - Does a new distribution of floats over tiles
C                        after every integration step.
C     o flt_up         - moves float to the surface (if flag is set)
C                        and stores profiles to file
C     o flt_down       - moves float to its target depth (if flag is set)
C     o flt_traj       - stores positions and data to file
C     o flt_interp_linear  - contains blinear interpolation scheme
C     o flt_mapping        - contains mapping functions & subroutine
C     o flt_mdsreadvector  - modified mdsreadvector to read files