MLAdjust/input.A4FlxF/data

# ====================
# | Model parameters |
# ====================
#
# Continuous equation parameters
 &PARM01
 viscAr=5.E-5,
#- This is the background viscosity used; total=viscah+viscleith
# viscAh=1.E2,
# viscA4=1.E2,
#- This is the background viscosity used on vorticity points
# viscAhZ=1.E2,
# viscA4Z=1.E2,
#- This is the background viscosity used on divergence points
# viscAhD=1.E2,
# viscA4D=1.E2,
#- viscAhD and viscAhZ are set to viscah if they are unset initially
#
#- This is a maximum gridscale Reynolds number limiter
# viscAhReMax=10.,
# viscA4ReMax=10.,
#- This is a minimum autoscaling viscosity
# viscAhGridMin=.01,
# viscA4GridMin=.01,
#- This is the standard Leith Viscosity, prop to grad(curl v_h)
#viscC2leith = 1.85,
 viscC4leith = 1.85,
# -This is an additional Leith Viscosity, prop to grad(div.v_h)
#  It traps instabilities that have no signal in grad(curl v_h)
#viscC2leithD = 1.85,
 viscC4leithD = 1.85,
# This is harmonic Smagorinsky Coefficient
# 0.2-0.9 = value from 3-d turbulence theory; Smagorinsky (1993)
# 2.2-4   = stable oceanic values (Griffies and Hallberg, 2000)
# 1. smag is approximately the same as 1.85 leith+leithd for this grid spacing
#viscC2smag = 1.,
 viscC4smag = 1.,
#- This is the max Viscosity used, be it Smag or Leith, and it scales
#  with grid size and timestep
#viscAhGridMax = 1.,
 viscA4GridMax = 1.,
#- This uses the full grad(vort) and grad(div)
 useFullLeith=.TRUE.,
#- This uses the Strain-Tension form for calculating viscous terms
#useStrainTensionVisc=.TRUE.,
#no_slip_sides=.FALSE.,
 no_slip_bottom=.FALSE.,
#vectorInvariantMomentum=.TRUE.,
 ivdc_kappa=10.,
 implicitDiffusion=.TRUE.,
 implicitViscosity=.TRUE.,
 f0=7.29E-5,
 beta=0.E-11,
 useJamartWetPoints=.TRUE.,
 eosType='LINEAR',
# Using Temperature as only Active Tracer
 tAlpha=2.E-4,
# Using Salinity as Spice
 sBeta =0.E-4,
 gravity=9.81,
 rhoNil=1035.,
 implicitFreeSurface=.TRUE.,
 staggerTimeStep=.TRUE.,
 tempAdvScheme=33,
 saltAdvScheme=33,
 readBinaryPrec=64,
 writeBinaryPrec=64,
 &

# Elliptic solver parameters
 &PARM02
 cg2dMaxIters=1000,
 cg2dTargetResidual=1.E-11,
 cg3dMaxIters=40,
 cg3dTargetResidual=1.E-9,
 &

# Time stepping parameters
 &PARM03
 nIter0=36,
#endTime=864000.,
#- for testing, only run for 12 iterations:
 nTimeSteps=12,
 deltaT=1200.,
 abEps=0.01,
#- for testing, reduce amount of output by commenting out output frequencies:
# pchkptFreq=43200.,
#taveFreq=7200.,
#dumpFreq=7200.,
#diagFreq=7200.,
 monitorSelect=2,
 monitorFreq=1200.,
 &

# Gridding parameters
 &PARM04
 usingCartesianGrid=.TRUE.,
 delR= 40*5.0,
 dxSpacing=1.E3,
 dySpacing=1.E3,
 &

# Input datasets
 &PARM05
 bathyFile='topo_sl.bin',
 hydrogThetaFile='thetaInitial.bin',
 hydrogSaltFile='spiceInitial.bin',
 &
1	# ====================
2	# \| Model parameters \|
3	# ====================
4	#
5	# Continuous equation parameters
6	&PARM01
7	viscAr=5.E-5,
8	#- This is the background viscosity used; total=viscah+viscleith
9	# viscAh=1.E2,
10	# viscA4=1.E2,
11	#- This is the background viscosity used on vorticity points
12	# viscAhZ=1.E2,
13	# viscA4Z=1.E2,
14	#- This is the background viscosity used on divergence points
15	# viscAhD=1.E2,
16	# viscA4D=1.E2,
17	#- viscAhD and viscAhZ are set to viscah if they are unset initially
18	#
19	#- This is a maximum gridscale Reynolds number limiter
20	# viscAhReMax=10.,
21	# viscA4ReMax=10.,
22	#- This is a minimum autoscaling viscosity
23	# viscAhGridMin=.01,
24	# viscA4GridMin=.01,
25	#- This is the standard Leith Viscosity, prop to grad(curl v_h)
26	#viscC2leith = 1.85,
27	viscC4leith = 1.85,
28	# -This is an additional Leith Viscosity, prop to grad(div.v_h)
29	# It traps instabilities that have no signal in grad(curl v_h)
30	#viscC2leithD = 1.85,
31	viscC4leithD = 1.85,
32	# This is harmonic Smagorinsky Coefficient
33	# 0.2-0.9 = value from 3-d turbulence theory; Smagorinsky (1993)
34	# 2.2-4 = stable oceanic values (Griffies and Hallberg, 2000)
35	# 1. smag is approximately the same as 1.85 leith+leithd for this grid spacing
36	#viscC2smag = 1.,
37	viscC4smag = 1.,
38	#- This is the max Viscosity used, be it Smag or Leith, and it scales
39	# with grid size and timestep
40	#viscAhGridMax = 1.,
41	viscA4GridMax = 1.,
42	#- This uses the full grad(vort) and grad(div)
43	useFullLeith=.TRUE.,
44	#- This uses the Strain-Tension form for calculating viscous terms
45	#useStrainTensionVisc=.TRUE.,
46	#no_slip_sides=.FALSE.,
47	no_slip_bottom=.FALSE.,
48	#vectorInvariantMomentum=.TRUE.,
49	ivdc_kappa=10.,
50	implicitDiffusion=.TRUE.,
51	implicitViscosity=.TRUE.,
52	f0=7.29E-5,
53	beta=0.E-11,
54	useJamartWetPoints=.TRUE.,
55	eosType='LINEAR',
56	# Using Temperature as only Active Tracer
57	tAlpha=2.E-4,
58	# Using Salinity as Spice
59	sBeta =0.E-4,
60	gravity=9.81,
61	rhoNil=1035.,
62	implicitFreeSurface=.TRUE.,
63	staggerTimeStep=.TRUE.,
64	tempAdvScheme=33,
65	saltAdvScheme=33,
66	readBinaryPrec=64,
67	writeBinaryPrec=64,
68	&
69
70	# Elliptic solver parameters
71	&PARM02
72	cg2dMaxIters=1000,
73	cg2dTargetResidual=1.E-11,
74	cg3dMaxIters=40,
75	cg3dTargetResidual=1.E-9,
76	&
77
78	# Time stepping parameters
79	&PARM03
80	nIter0=36,
81	#endTime=864000.,
82	#- for testing, only run for 12 iterations:
83	nTimeSteps=12,
84	deltaT=1200.,
85	abEps=0.01,
86	#- for testing, reduce amount of output by commenting out output frequencies:
87	# pchkptFreq=43200.,
88	#taveFreq=7200.,
89	#dumpFreq=7200.,
90	#diagFreq=7200.,
91	monitorSelect=2,
92	monitorFreq=1200.,
93	&
94
95	# Gridding parameters
96	&PARM04
97	usingCartesianGrid=.TRUE.,
98	delR= 40*5.0,
99	dxSpacing=1.E3,
100	dySpacing=1.E3,
101	&
102
103	# Input datasets
104	&PARM05
105	bathyFile='topo_sl.bin',
106	hydrogThetaFile='thetaInitial.bin',
107	hydrogSaltFile='spiceInitial.bin',
108	&