ELF>@@ O= "7Ln`L@="O B)D:JZjH 7@VD?;.6(<d7 ,9,@<@L A\lF|(<@)lp:9E @KJ,M< 9LH\`GlL&|tx$ 2D `|,<L<\l|,Hdh?C33 (! @,`A<L LX\\=l|B"<@!d l,< ALA\l|0B $ @I( "L #p R  G &( %7 %F %U, %dT sX  $ , 4, <A DV Lk T \ d l t |   ( = R g |        $ 9 N c x    ( 0 8 @ H P X5 `J h_ pt x        1 F [ p       - B(W0l8@HPX`hpx)>Sh}%:Ody (0 8!@6HKP`Xu`hpx  .8Qd]z. 8 B L V `l";R6H76H7UHHp=uaH}H ALE3HINHEH}HE<HUHEHu33HUH]@UHATAUAVSH`II=}HH AL3HHG@KHGHHHGP<HHBHHG`!HHBHHGpHHBHHDžNHHBHHDžHHBHHDž H HBHHDž0H0HBHHDž@H@HBHHDžPHPHBHHDž`AH`HBHHDžpCHpHBHHDžHHBHHDžHHBHHDžHHBHH 3LHIGI@HH 3LHI6I@HH 3LHIUI@HH 3LHI>I@HH 3LHI:I@HH 3LHI-I@HH 3LHI5I@HH 3L HI;I@HH 3L0HI6I@HH 3L@HI+I@HH 3LPHI8I@HH 3L`HI?I@HH 3LpHI?I@HH 3LHI@I@HH 3LHI I@HH E33HHH 3LHIEI@HH 3LHI'I@HH 3L3HII@HH 3LHI(I@HH 3LHII@HH 3LHII@HH 3LHI9I@HH 3LHI8I@HH 3L HIDI@HH 3L0HII@HH 3L@HIJI@HH 3LPHIII@HH 3L`HILI@HH 3LpHI8I@HH 3LHII@HH 3LHIFI@HH 3LHI%I@HH 3LHII@HH 3LHI#I@HH 3LHII@HH 3LHII@HH 3LHII@HH 3LHII@HH 3LHII@HH 3L HI1I@HH 3L0HII@HH 3L@HII@HH 3LPHII@HH 3L`HII@HH 3LpHII@HH 3LHI;I@HH 3LHII@HH 3LHII@HH 3LHII@HH 3LHII@HH 3LHII@HH 3LHI>I@HH 3LHIBI@HH 3LHI2I@HH 3LHI2I@HH 3L HII@HH 3L0HI I@HH 3L@HI I@HH 3LPHI?I@HH 3L`HI@I@HH 3LpHII@HH 3LHII@HH 3LHI<I@HH 3LHII@HH 3LHII@HH 3LHII@HH 3LHIAI@HH 3LHI I@HH 3LHI!I@HH 3LHII@HH 3LHI;I@HH 3L HI I@HH 3L0HII@HH 3L@HII@HH 3LPHII@HH 3L`HII@HH 3LpHI@I@HH 3LHI@I@HH 3LHII@HH 3LHII@HH 3LHI/I@HH 3LHIAI@HH 3LHII@HH 3LHII@HH 3LHIHI@HH 3LHI!I@HH 3LHI"I@HH 3L HII@HH 3L0HIQI@HH 3L@HIFI@HH 3LPHI%I@HH 3L`HI$I@HH 3LpHI$I@HH 3LEHI$HEHH 3LEHI$HEHH 3LEHIHEHH 3LEHIIHELHHH+HHLHLLHHcHUHH]LHĿHu33HUHe[A^A]A\]D8888888888888888888888888888888888888888888888888888888888888888888888888888888888888888888888888888888888888888888Usage: mpirun -np nproc pcc2hist [-h] [-r res] [-v] [input_file] [output_file]pcc2hist is a program to convert from the CSIRO conformal cubic atmosphericUsage: mpirun -np nproc pcc2hist [-h] [-r res] [-v] [input_file] [output_file] -r res where res is the resolution in degrees of the output file (Default resolution is approximately equal to model resolution).There are also several options controlling the horizontal interpolation --interp=linear Use bi-linear horizonal interpolation rather than standard bicubicNote that the missing option only works with linear or nearest horizontal interpolation. Default is to extrapolate temperaturebelow surface with standard lapse rate and to use end values forThe program reads a control namelist file called cc.nml. The namelist ktc int -1 Timestep increment (-1 means do all) sdate int -1 If these are set to positive integers they stime int -1 specify the date/time range of the output edate int -1 data. It's not necessary to set any of kta, ndate int -1 Obsolete method for selecting a singleIt is also possible to interpolate to specified pressure levels byNote that this uses simple spline extrapolation above and belowthe top and bottom model levels. This may give odd results so beFor the ocean depths, interpolation can be specified according towill save just temp, tsu and psl. Setting hnames="all" will saveall available variables. Particular variables can be excluded byThe hfreq and htype fields are required and should not be changedCommand line options can be replaced with the following namelist optionsint_default = 0 (bicubic), 1 (nearest), 2 (bilinear), 5 (none), 9 (tapm)vextrap = 0 (default), 1 (linear), 2 (none), 3 (missing), pcc2hist -h for full list of options and more information.model history file to a regular lat-lon netcdf file suitablefor processing by other programs.Command line options are -h for help (this message) -v for version numberand extrapolation to pressure levels below the surface --interp=nearest Use nearest value rather than interpolation --interp=none No interpolation. Output on cubic grid --interp=tapm Interpolation to TAPM grid --vextrap=linear Linear extrapolation below surface --vextrap=none Use end values rather than extrapolation --vextrap=missing Set values below surface as missing --cordex Format output for CORDEX --nounderscore Remove underscore from variable namesother fields.is called 'input' and the variables are NAME TYPE DEFAULT FUNCTION Selection of time steps kta int 0 First timestep to process ktb int 9999999 Last timestep to process etime int -1 ktb or ktc in this case. ntime int -1 time. Boundaries of output region minlon real 0 maxlon real 360 minlat real -90 maxlat real 90 The boundary for the TAPM output region is lx int >0 ly int >0 dx real >0 dy real >0 Output levels are the intersection of the following minlev int 1 maxlev int kl minsig real 0. maxsig real 1.By default the output variables are on the model sigma levels.setting the logical input variable use_plevs to T.The input array plevs specifies the levels to use.E.g.use_plevs = Tplevs = 1000, 850, 500, 200, 100careful.It is also possible to interpolate to height in meters usinguse_meters = Tmlevs = 10, 50, 100, 1000use_depth = Tdlevs = 5, 10, 50, 100, 500, 1000A second namelist section allows precise control over whichvariables are saved. For example&histnlhnames = "temp", "tsu", "psl"hfreq = 1, htype = "inst"/setting xnames. E.g.hnames = "all", xnames="sdot"will save everything but the vertical velocity.for normal use.ifile = input_fileofile = output_filehres = res 4 (lapse rate)cf_compliant = true or falsecordex_compliant = true or falseno_underscore = true or falsesave_ccam_parameters = true or falsepcc2hist version x $4AC 4\AC NABBC  usage_m.f90 usage_m._ usage_m_mp_usage_` usage_m_mp_help_ 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