Annotation of /MITgcm_contrib/high_res_cube/input/data_hr

# ====================
# | Model parameters |
# ====================
#
# Continuous equation parameters
 &PARM01
 tRef               = 3*23.,3*22.,21.,2*20.,19.,2*18.,17.,2*16.,15.,14.,13.,
                      12.,11.,2*9.,8.,7.,2*6.,2*5.,3*4.,3*3.,4*2.,12*1.,
 sRef               = 50*34.5,
 viscAr= 1e-3,
 no_slip_sides=.FALSE.,
 no_slip_bottom=.TRUE.,
 diffKhT=0.,
 diffK4T=0.,
 diffKrT=1.51e-5,
 diffKhS=0.,
 diffK4S=0.,
 diffKrS=1.51e-5,
 tAlpha=2.E-4,
 sBeta =7.4E-4,
 gravity=9.81,
 eosType='JMD95Z',
 readBinaryPrec=32,
 writeBinaryPrec=32,
 useSingleCPUio=.TRUE.
 hFacMinDr=50.,
 hFacMin=0.3,
 hFacInf=0.1,
 hFacSup=5.,
# z* - begin
    select_rStar=2,
    nonlinFreeSurf=4,
# * - end
 implicitDiffusion=.true.,
 implicitViscosity=.true.,
 allowFreezing=.false.,
 viscAh=0.,
 viscAhGrid=0.,
# Following change took place starting in checkpoint57v_post
# Redefine viscC?Leith*.  Change the coefficients of Leith viscosity 
# to be proportional to enstrophy dissipation length.  Thus,
#  viscC?leith?_new=pi*(viscC?leith?_old)^(1/3)
# This is now consistent with Smagorinsky and with the manual.
# viscC4Leith=1.0,
# viscC4Leithd=1.0,
# viscC4Leith=3.1416,
# viscC4Leithd=3.1416,
 viscC4Leith=1,
 viscC4Leithd=1,
 viscC2Leith=0.,
 viscA4=0.,
 useAreaViscLength=.TRUE.,
 sideDragFactor=0.,
 SadournyCoriolis=.TRUE.,
 useAbsVorticity=.TRUE.,
 bottomDragQuadratic = 0.002,
 tempAdvScheme=33,
 saltAdvScheme=33,
 StaggerTimeStep=.true.,
 multiDimAdvection=.true.,
 vectorInvariantMomentum=.TRUE.,
 rigidLid=.FALSE.,
 implicitFreeSurface=.TRUE.,
 exactConserv=.TRUE.,
 debuglevel=-1
 &

# Elliptic solver parameters
 &PARM02
 cg2dMaxIters=100,
 cg2dTargetResidual=1.E-5,
 &

# Time stepping parameters
 &PARM03
 niter0=216,
 endTime=421459200,
 abEps=0.1,
 deltaT=1200,
 cAdjFreq=0.,
 pChkptFreq=31536000,
 chkptFreq=2592000
 tauSaltClimRelax = 3842380.,
 monitorFreq=86400
 forcing_In_AB = .FALSE.
 calendarDumps = .TRUE.
 dumpInitAndLast=.FALSE.
 &

# Gridding parameters
 &PARM04
 usingCartesianGrid=.FALSE.,
 usingSphericalPolarGrid=.FALSE.,
 usingCurvilinearGrid=.TRUE.,
 delR   = 10.00, 10.00, 10.00, 10.00, 10.00, 10.00, 10.00, 10.01,
 10.03, 10.11, 10.32, 10.80, 11.76, 13.42, 16.04 , 19.82, 24.85, 
 31.10, 38.42, 46.50, 55.00, 63.50, 71.58, 78.90, 85.15, 90.18, 
 93.96, 96.58, 98.25, 99.25,100.01,101.33,104.56,111.33,122.83,
 139.09,158.94,180.83,203.55,226.50,249.50,272.50,295.50,318.50,
 341.50,364.50,387.50,410.50,433.50,456.50,
 &

# Input datasets
 &PARM05
 bathyFile      ='ETOPO2_510x6x510_ver5e_filled.bin',
 hydrogThetaFile='LEVT01_JAN_510x6x510x50.bin',
 hydrogSaltFile ='LEVS01_JAN_510x6x510x50.bin',
 &
1	dimitri	1.1	# ====================
2			# \| Model parameters \|
3			# ====================
4			#
5			# Continuous equation parameters
6			&PARM01
7			tRef = 323.,322.,21.,220.,19.,218.,17.,2*16.,15.,14.,13.,
8			12.,11.,29.,8.,7.,26.,25.,34.,33.,42.,12*1.,
9			sRef = 50*34.5,
10	dimitri	1.15	viscAr= 1e-3,
11	dimitri	1.12	no_slip_sides=.FALSE.,
12	dimitri	1.1	no_slip_bottom=.TRUE.,
13	dimitri	1.2	diffKhT=0.,
14	dimitri	1.3	diffK4T=0.,
15	dimitri	1.12	diffKrT=1.51e-5,
16	dimitri	1.2	diffKhS=0.,
17	dimitri	1.3	diffK4S=0.,
18	dimitri	1.12	diffKrS=1.51e-5,
19	dimitri	1.1	tAlpha=2.E-4,
20			sBeta =7.4E-4,
21			gravity=9.81,
22			eosType='JMD95Z',
23			readBinaryPrec=32,
24			writeBinaryPrec=32,
25			useSingleCPUio=.TRUE.
26			hFacMinDr=50.,
27	dimitri	1.9	hFacMin=0.3,
28	dimitri	1.10	hFacInf=0.1,
29	dimitri	1.4	hFacSup=5.,
30			# z* - begin
31			select_rStar=2,
32			nonlinFreeSurf=4,
33			# * - end
34	dimitri	1.1	implicitDiffusion=.true.,
35			implicitViscosity=.true.,
36	dimitri	1.4	allowFreezing=.false.,
37	dimitri	1.14	viscAh=0.,
38			viscAhGrid=0.,
39	dimitri	1.19	# Following change took place starting in checkpoint57v_post
40			# Redefine viscC?Leith*. Change the coefficients of Leith viscosity
41			# to be proportional to enstrophy dissipation length. Thus,
42			# viscC?leith?_new=pi*(viscC?leith?_old)^(1/3)
43			# This is now consistent with Smagorinsky and with the manual.
44			# viscC4Leith=1.0,
45			# viscC4Leithd=1.0,
46	dimitri	1.21	# viscC4Leith=3.1416,
47			# viscC4Leithd=3.1416,
48			viscC4Leith=1,
49			viscC4Leithd=1,
50	dimitri	1.14	viscC2Leith=0.,
51			viscA4=0.,
52	dimitri	1.20	useAreaViscLength=.TRUE.,
53			sideDragFactor=0.,
54			SadournyCoriolis=.TRUE.,
55			useAbsVorticity=.TRUE.,
56	dimitri	1.1	bottomDragQuadratic = 0.002,
57	dimitri	1.12	tempAdvScheme=33,
58			saltAdvScheme=33,
59			StaggerTimeStep=.true.,
60			multiDimAdvection=.true.,
61	dimitri	1.1	vectorInvariantMomentum=.TRUE.,
62			rigidLid=.FALSE.,
63			implicitFreeSurface=.TRUE.,
64			exactConserv=.TRUE.,
65	dimitri	1.12	debuglevel=-1
66	dimitri	1.1	&
67
68			# Elliptic solver parameters
69			&PARM02
70	dimitri	1.4	cg2dMaxIters=100,
71			cg2dTargetResidual=1.E-5,
72	dimitri	1.1	&
73
74			# Time stepping parameters
75			&PARM03
76	dimitri	1.12	niter0=216,
77	dimitri	1.16	endTime=421459200,
78	dimitri	1.1	abEps=0.1,
79	dimitri	1.12	deltaT=1200,
80	dimitri	1.1	cAdjFreq=0.,
81	dimitri	1.12	pChkptFreq=31536000,
82			chkptFreq=2592000
83	dimitri	1.5	tauSaltClimRelax = 3842380.,
84	dimitri	1.12	monitorFreq=86400
85			forcing_In_AB = .FALSE.
86	dimitri	1.13	calendarDumps = .TRUE.
87	dimitri	1.18	dumpInitAndLast=.FALSE.
88	dimitri	1.1	&
89
90			# Gridding parameters
91			&PARM04
92			usingCartesianGrid=.FALSE.,
93			usingSphericalPolarGrid=.FALSE.,
94			usingCurvilinearGrid=.TRUE.,
95			delR = 10.00, 10.00, 10.00, 10.00, 10.00, 10.00, 10.00, 10.01,
96			10.03, 10.11, 10.32, 10.80, 11.76, 13.42, 16.04 , 19.82, 24.85,
97			31.10, 38.42, 46.50, 55.00, 63.50, 71.58, 78.90, 85.15, 90.18,
98			93.96, 96.58, 98.25, 99.25,100.01,101.33,104.56,111.33,122.83,
99			139.09,158.94,180.83,203.55,226.50,249.50,272.50,295.50,318.50,
100			341.50,364.50,387.50,410.50,433.50,456.50,
101			&
102
103			# Input datasets
104			&PARM05
105	dimitri	1.12	bathyFile ='ETOPO2_510x6x510_ver5e_filled.bin',
106			hydrogThetaFile='LEVT01_JAN_510x6x510x50.bin',
107			hydrogSaltFile ='LEVS01_JAN_510x6x510x50.bin',
108	dimitri	1.1	&