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grib2map.tbl @ 1759

Last change on this file since 1759 was 11, checked in by aslmd, 14 years ago
spiga@svn-planeto:ajoute le modele meso-echelle martien
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1	# Header section that describes the following GRIB 2 table(s)
2	#
3	# Ind \| center \| subcenter \| Master Tbl Version \| Local Tbl Version \|
4	#-----+--------+-----------+--------------------+-------------------+
5	-1 \| 255 \| 255 \| 1 \| 1 \|
6	#
7	# The table itself
8	#
9	# The precision is controlled by the decimal and binary scale factors.
10	#
11	# The decimal scale factor is the number of digits after the decimal point
12	# that are retained. If negative, precision is reduced by 10**dec (i.e.,
13	# -1 would reduce the precision to the nearest factor of 10).
14	#
15	# When the decimal scale factor is 0, the binary scale factor indicates the
16	# precision of the data in bits.
17	#
18	# The grib2 docuementation, available from http://, describes the decimal
19	# and binary scale factors in more detail.
20	#
21	#
22	#
23	#Dis\|Cat\|Prm\| \| \|Dec \|Bin \|
24	#cip\|gor\|Num\| WRF Id(s) \| Description \|Fctr\|Fctr\|
25	#---+---+---+-----------+------------------------------------------+----+----+
26	0 \| 0 \| 0 \| T2,TSK \| Temperature \| 2 \| 0 \|
27	0 \| 0 \| 2 \| TH2,THZ0,T\| Potential Temperature \| 1 \| 0 \|
28	0 \| 0 \|192\| T_INIT \| Initial Potential Temperature \| 3 \| 0 \|
29	0 \| 0 \|193\| RTHFTEN \| Temp. Tendency in Grell Cumulus [K/s] \| 6 \| 0 \|
30	0 \| 0 \|194\| T_BASE \| Base State T in Idealized Cases [K] \| 2 \| 0 \|
31	0 \| 0 \|195\| T_1 \| Restart Parameter \| 4 \| 0 \|
32	0 \| 0 \|196\| T_2 \| Restart Parameter \| 4 \| 0 \|
33	0 \| 0 \|197\| H_DIABATIC\| Previous Timestep Condensational heating \| 7 \| 0 \|
34	0 \| 0 \|198\| RTHCUTEN \| Coupled theta tend(cumulus sch)[Pa K s-1]\| 3 \| 0 \|
35	0 \| 0 \|199\| RTHRATEN \| Coupled theta tend due to radia [Pa K/s] \| 3 \| 0 \|
36	0 \| 0 \|200\| RTHRATLW \| Coupled theta tend due to lw rad [Pa K/s]\| 3 \| 0 \|
37	0 \| 0 \|201\| RTHRATSW \| Coupled theta tend due to sw rad [Pa K/s]\| 3 \| 0 \|
38	0 \| 0 \|202\| MOL \| TStar in Similarity theory [K] \| 3 \| 0 \|
39	0 \| 0 \|203\| THC \| Thermal Inertia [Cal /(cm K s^.5)] \| 3 \| 0 \|
40	0 \| 0 \|204\| RTHBLTEN \| Coupled theta tend due to PBL [Pa K/s] \| 4 \| 0 \|
41	0 \| 1 \| 0 \| QSFC \| Specific Humidity [kg/kg] \| 5 \| 0 \|
42	0 \| 1 \| 2 \|QVAPOR,Q2,QVG\|Humidity Mixing Ratio [kg/kg] \| 5 \| 0 \|
43	0 \| 1 \| 6 \|SFCEVP \| Evaporation [kg/m^2] \| 3 \| 0 \|
44	0 \| 1 \| 9 \| RAINNC \| Large-scale precip (non-conv)[Kg/m^2] \| 2 \| 0 \|
45	0 \| 1 \| 10\| RAINC \| Convective precipitation [kg/m^2] \| 2 \| 0 \|
46	0 \| 1 \| 13\| WEASD,SNOW\| Water equivalent of snow depth [kg/m^2] \| 2 \| 0 \|
47	0 \| 1 \| 11\|SNOWH,SNOWCU,ACSNOW\|Snow depth [m] \| 4 \| 0 \|
48	0 \| 1 \| 22\| QCLOUD,QCG\| Cloud water mixing ratio [kg/kg] \| 6 \| 0 \|
49	0 \| 1 \| 23\| QICE \| Ice water mixing ratio [kg/kg] \| 5 \| 0 \|
50	0 \| 1 \| 24\| QRAIN \| Rain water mixing ratio [kg/kg] \| 5 \| 0 \|
51	0 \| 1 \| 25\| QSNOW \| Snow water mixing ratio [kg/kg] \| 5 \| 0 \|
52	0 \| 1 \| 32\| QGRAUP \| Graupel mixing ratio [kg/kg] \| 5 \| 0 \|
53	0 \| 1 \|192\| LH \| Latent heat flux [W/m^2] \| 2 \| 0 \|
54	0 \| 1 \|193\| ACSNOM \| Accumulated melted snow [cm] \| 2 \| 0 \|
55	0 \| 1 \|194\| RAINNCV \| Large-scale precip rate [kg/m^2/s] \| 7 \| 0 \|
56	0 \| 1 \|195\| RAINCV \| Convective precip rate [kg/m^2/s] \| 7 \| 0 \|
57	0 \| 1 \|196\| QFX \| Upward moisture flux [kg/m^s] \| 6 \| 0 \|
58	0 \| 1 \|197\| HFX \| Upward heat flux at the surface [W/m^2] \| 1 \| 0 \|
59	0 \| 1 \|198\| QNI \| Ice crystal number concentration \| 0 \| 0 \|
60	0 \| 1 \|199\| QV_BASE \| Base State QV in Idealized Cases \| 5 \| 0 \|
61	0 \| 1 \|200\| CT \| Countergradient term [K] \| 5 \| 0 \|
62	0 \| 1 \|201\| QZ0 \| Specific humidity at rough length [kg/kg]\| 5 \| 0 \|
63	0 \| 1 \|202\| CUPPT \| Acc cnv rain since last call to rad \| 4 \| 0 \|
64	0 \| 1 \|203\| F_ICE_PHY \| Fraction of Ice (eta mp state variable) \| 2 \| 0 \|
65	0 \| 1 \|204\| F_RAIN_PHY\| Fraction of Rain (eta mp state variable) \| 2 \| 0 \|
66	0 \| 1 \|205\|F_RIMEF_PHY\| Mass Ratio of Rimed Ice(eta mp variable) \| 2 \| 0 \|
67	0 \| 1 \|206\| RQVCUTEN \| Coupled QV tend(cum sch)[Pa kg kg-1 s-1] \| 6 \| 0 \|
68	0 \| 1 \|207\| RQRCUTEN \| Coupled QR tend(cum sch)[Pa kg kg-1 s-1] \| 6 \| 0 \|
69	0 \| 1 \|208\| RQCCUTEN \| Coupled QC tend(cum sch)[Pa kg kg-1 s-1] \| 6 \| 0 \|
70	0 \| 1 \|209\| RQSCUTEN \| Coupled QS tend(cum sch)[Pa kg kg-1 s-1] \| 6 \| 0 \|
71	0 \| 1 \|210\| RQICUTEN \| Coupled QI tend(cum sch)[Pa kg kg-1 s-1] \| 6 \| 0 \|
72	0 \| 1 \|211\| RAINBL \| Acc pcp over BL time step [kg/m^2] \| 2 \| 0 \|
73	0 \| 1 \|212\| NCA \| Counter of cloud relax in KF \| 2 \| 0 \|
74	0 \| 1 \|213\| APR_GR \| Precip from closure (old grell) [mm/hr] \| 4 \| 0 \|
75	0 \| 1 \|214\| APR_W \| Precip from closure W [mm/hr] \| 4 \| 0 \|
76	0 \| 1 \|215\| APR_MC \| Precip from closure Krish MV [mm/hr] \| 4 \| 0 \|
77	0 \| 1 \|216\| APR_ST \| Precip from closure Stability [mm/hr] \| 4 \| 0 \|
78	0 \| 1 \|217\| APR_AS \| Precip from closure AS-Type [mm/hr] \| 4 \| 0 \|
79	0 \| 1 \|218\| APR_CAPMA \| Precip from max CAP [mm/hr] \| 4 \| 0 \|
80	0 \| 1 \|219\| APR_CAPME \| Precip from mean CAP [mm/hr] \| 4 \| 0 \|
81	0 \| 1 \|220\| APR_CAPMI \| Precip from min CAP [mm/hr] \| 4 \| 0 \|
82	0 \| 1 \|221\| PR_ENS \| Precip rate in Grell \| 4 \| 0 \|
83	0 \| 1 \|222\| RQVFTEN \| Moisture tendency in Grell [kg/s] \| 6 \| 0 \|
84	0 \| 1 \|223\| CLDEFI \| Precipitation efficiency in BMJ \| 4 \| 0 \|
85	0 \| 1 \|224\| RQVBLTEN \| Coupled QV tend due to PBL [Pa kg/(kg s)]\| 0 \| 24 \|
86	0 \| 1 \|225\| RQCBLTEN \| Coupled QC tend due to PBL [Pa kg/(kg s)]\| 0 \| 24 \|
87	0 \| 1 \|226\| RQIBLTEN \| Coupled QI tend due to PBL [Pa kg/(kg s)]\| 0 \| 24 \|
88	0 \| 1 \|227\| FLQC \| Surface exchange coefficient for moisture\| 6 \| 0 \|
89	0 \| 1 \|228\| QSG \| Surface saturation wv mixing ratio[kg/kg]\| 6 \| 0 \|
90	0 \| 1 \|229\| MAVAIL \| Surface moisture availability \| 4 \| 0 \|
91	0 \| 2 \| 2 \| U,U10,UZ0 \| U-component of wind [m/s] \| 2 \| 0 \|
92	0 \| 2 \| 3 \| V,V10,VZ0 \| V-component of wind [m/s] \| 2 \| 0 \|
93	0 \| 2 \| 7 \| WW \| Sigma coordinate vertical velocity [s^-1]\| 3 \| 0 \|
94	0 \| 2 \| 9 \| W \| Geometric vertical velocity [m/s] \| 4 \| 0 \|
95	0 \| 2 \|192\| U_BASE \| Base State X Wind in Idealized Cases \| 3 \| 0 \|
96	0 \| 2 \|193\| V_BASE \| Base State Y Wind in Idealized Cases \| 3 \| 0 \|
97	0 \| 2 \|194\| U_1 \| Restart Parameter \| 4 \| 0 \|
98	0 \| 2 \|195\| U_2 \| Restart Parameter \| 4 \| 0 \|
99	0 \| 2 \|196\| V_1 \| Restart Parameter \| 4 \| 0 \|
100	0 \| 2 \|197\| V_2 \| Restart Parameter \| 4 \| 0 \|
101	0 \| 2 \|198\| W_1 \| Restart Parameter \| 0 \| 24 \|
102	0 \| 2 \|199\| W_2 \| Restart Parameter \| 0 \| 24 \|
103	0 \| 2 \|200\| SFCEXC \| Exchange coefficient [m/s] \| 5 \| 0 \|
104	0 \| 2 \|201\| AKHS \| Sfc exchange coefficient for heat [m/s] \| 5 \| 0 \|
105	0 \| 2 \|202\| AKMS \| Sfc exch coefficient for momentum [m/s] \| 3 \| 0 \|
106	0 \| 2 \|203\| W0AVG \| Average VV for KF Cum Scheme [m/s] \| 6 \| 0 \|
107	0 \| 2 \|204\| MASS_FLUX \| Downdraft mass flux in grell [mb/hr] \| 4 \| 0 \|
108	0 \| 2 \|205\| RUBLTEN \| Coupled X-wind tend due to PBL [Pa m/s^2]\| 2 \| 0 \|
109	0 \| 2 \|206\| RVBLTEN \| Coupled X-wind tend due to PBL [Pa m/s^2]\| 2 \| 0 \|
110	0 \| 2 \|207\| UST \| UStar in Similarity theory [m/s] \| 4 \| 0 \|
111	0 \| 2 \|208\| FLHC \| Surface exchange coefficient for heat \| 3 \| 0 \|
112	0 \| 3 \| 0 \| P,PSFC \| Pressure [Pa] \| 1 \| 0 \|
113	0 \| 3 \| 1 \| PMSL \| Pressure reduced to MSL [Pa] \| 1 \| 0 \|
114	0 \| 3 \| 4 \| PHP \| Geopotential [m^2/s^2] \| 3 \| 0 \|
115	0 \| 3 \|192\| PHB \| Base-state geopotential [m^2/s^2] \| 0 \| 0 \|
116	0 \| 3 \|193\| PH \| Perturbation geopotential [m^2/s^2] \| 1 \| 0 \|
117	0 \| 3 \|194\| MUB \| Base-state dry air mass in column [Pa] \| 1 \| 0 \|
118	0 \| 3 \|195\| MU \| Perturbation dry air mass in column [Pa] \| 1 \| 0 \|
119	0 \| 3 \|196\| MU0 \| Initial dry air mass in column [Pa] \| 0 \| 0 \|
120	0 \| 3 \|197\| PB \| Base-state pressure [Pa] \| 0 \| 0 \|
121	0 \| 3 \|198\| GRDFLX \| Ground heat flux [W/m^2] \| 1 \| 0 \|
122	0 \| 3 \|199\| Z_BASE \| Base State Height in Idealized Cases \| 5 \| 0 \|
123	0 \| 3 \|200\| PH_1 \| Restart Parameter \| 3 \| 0 \|
124	0 \| 3 \|201\| PH_2 \| Restart Parameter \| 3 \| 0 \|
125	0 \| 3 \|202\| PH0 \| Initial geopotential \| 1 \| 0 \|
126	0 \| 3 \|203\| MU_1 \| Restart Parameter \| 3 \| 0 \|
127	0 \| 3 \|204\| MU_2 \| Restart Parameter \| 3 \| 0 \|
128	0 \| 3 \|205\| AL \| Inverse perturbation density [m3 kg-1] \| 5 \| 0 \|
129	0 \| 3 \|206\| ALT \| Inverse density [m3 kg-1] \| 4 \| 0 \|
130	0 \| 3 \|207\| XF_ENS \| Mass flux PDF in GRELL \| 4 \| 0 \|
131	0 \| 4 \| 0 \| GSW \| Net short wave flux [W/m^2] \| 3 \| 0 \|
132	0 \| 4 \|192\| SWDOWN \| Downward short wave flux [W/m^2] \| 1 \| 0 \|
133	0 \| 4 \|193\| TOTSWDN \| Radiation State Variable \| 2 \| 0 \|
134	0 \| 4 \|194\| RSWTOA \| Radiation State Variable \| 4 \| 0 \|
135	0 \| 4 \|195\| RLWTOA \| Radiation State Variable \| 4 \| 0 \|
136	0 \| 4 \|196\| CZMEAN \| Radiation State Variable \| 4 \| 0 \|
137	0 \| 4 \|197\| CFRACL \| Radiation State Variable \| 4 \| 0 \|
138	0 \| 4 \|198\| CFRACM \| Radiation State Variable \| 4 \| 0 \|
139	0 \| 4 \|199\| CFRACH \| Radiation State Variable \| 4 \| 0 \|
140	0 \| 4 \|200\| ACFRST \| Radiation State Variable \| 4 \| 0 \|
141	0 \| 4 \|201\| NCFRST \| Radiation State Variable \| 4 \| 0 \|
142	0 \| 4 \|202\| ACFRCV \| Radiation State Variable \| 4 \| 0 \|
143	0 \| 4 \|203\| NCFRCV \| Radiation State Variable \| 4 \| 0 \|
144	0 \| 5 \| 0 \| GLW \| Net long wave flux [W/m^2] \| 2 \| 0 \|
145	0 \| 5 \|193\| TOTLWDN \| Radiation State Variable \| 4 \| 0 \|
146	0 \| 6 \| 1 \| CLDFRA \| Total Cloud Cover [%] \| 2 \| 0 \|
147	0 \| 6 \|192\| TAUCLDI \| Cloud optical thickness for ice \| 2 \| 0 \|
148	0 \| 6 \|193\| TAUCLDC \| Cloud optical thickness for water \| 2 \| 0 \|
149	0 \| 13\|192\|MASS_AER_WATER\| aerosol liquid water content \| 6 \| 0 \|
150	0 \| 13\|193\|MASS_AER_DRY\| dry aerosol mass \| 6 \| 0 \|
151	0 \| 19\| 1\| ALBEDO \| Albedo [%] \| 2 \| 0 \|
152	0 \| 19\| 11\|TKE,TKE_MYJ\| Turbulent Kinetic Energy [J/kg] \| 3 \| 0 \|
153	0 \| 19\|192\| ALBBCK \| Background Albedo [%] \| 4 \| 0 \|
154	0 \| 19\|193\| TKE_1 \| Restart Parameter \| 3 \| 0 \|
155	0 \| 19\|194\| TKE_2 \| Restart Parameter \| 3 \| 0 \|
156	0 \|191\|192\| CFN \| CFN from WRF [?] \| 3 \| 0 \|
157	0 \|191\|193\| CFN1 \| CFN1 from WRF [?] \| 3 \| 0 \|
158	0 \|191\|194\| ZNU \| Eta values on half (mass) levels \| 6 \| 0 \|
159	0 \|191\|195\| ZNW \| Eta values on full (w) levels \| 6 \| 0 \|
160	0 \|191\|196\| DN \| DN values [dimensionless] \| 4 \| 0 \|
161	0 \|191\|197\| DNW \| DNW values [dimensionless] \| 4 \| 0 \|
162	0 \|191\|198\| RDN \| Inverse DN values [dimensionless] \| 3 \| 0 \|
163	0 \|191\|199\| RDNW \| Inverse d(eta) values for full (w) levels\| 3 \| 0 \|
164	0 \|191\|200\| FNP \| Lower weight for vertical strection [dim]\| 5 \| 0 \|
165	0 \|191\|201\| FNM \| Upper weight for vertical strection [dim]\| 5 \| 0 \|
166	0 \|191\|202\| MAPFAC_M \| Map Scale Factor [dimensionless] \| 4 \| 0 \|
167	0 \|191\|203\| MAPFAC_U \| Map Scale Factor [dimensionless] \| 4 \| 0 \|
168	0 \|191\|204\| MAPFAC_V \| Map Scale Factor [dimensionless] \| 4 \| 0 \|
169	0 \|191\|205\| F \| Coriolis sine latitude term \| 6 \| 0 \|
170	0 \|191\|206\| E \| Coriolis cosine latitude term \| 6 \| 0 \|
171	0 \|191\|207\| PBLH \| Planetary boundary layer height [m] \| 0 \| 0 \|
172	0 \|191\|208\| ZS \| Depths of centers of soil layers [m] \| 3 \| 0 \|
173	0 \|191\|209\| DZS \| Thicknesses of soil layers [m] \| 3 \| 0 \|
174	0 \|191\|210\| XLAT \| Latitude [deg] \| 4 \| 0 \|
175	0 \|191\|211\| XLONG \| Longitude [deg] \| 4 \| 0 \|
176	0 \|191\|212\| COSALPHA \| Local cosine of map rotation \| 6 \| 0 \|
177	0 \|191\|213\| SINALPHA \| Local sine of map rotation \| 6 \| 0 \|
178	0 \|191\|214\| NEST_POS \| Nest Position \| 0 \| 0 \|
179	0 \|191\|215\| ALB \| Restart Parameter (??) \| 4 \| 0 \|
180	0 \|191\|216\| EXCH_H \| Exchange coefficients \| 3 \| 0 \|
181	0 \|191\|217\| KPBL \| Level of PBL top [m] \| 1 \| 0 \|
182	0 \|191\|218\| HTOP \| Top of convection level \| 1 \| 0 \|
183	0 \|191\|219\| HBOT \| Bottom of convection level \| 1 \| 0 \|
184	0 \|191\|220\| TKESFCF \| TKE at the surface [m^/s^2] \| 3 \| 0 \|
185	0 \|191\|253\|WRF_SCALAR \| Scalar Output data in local section \| 0 \| 0 \|
186	0 \|191\|254\|WRF_GLOBAL \| Global Output data in local section \| 0 \| 0 \|
187	0 \|192\| 1 \| U_BXS \| \| 0 \| 0 \|
188	0 \|192\| 2 \| U_BXE \| \| 0 \| 0 \|
189	0 \|192\| 3 \| U_BYS \| \| 0 \| 0 \|
190	0 \|192\| 4 \| U_BYE \| \| 0 \| 0 \|
191	0 \|192\| 5 \| U_BTXS \| \| 2 \| 0 \|
192	0 \|192\| 6 \| U_BTXE \| \| 2 \| 0 \|
193	0 \|192\| 7 \| U_BTYS \| \| 2 \| 0 \|
194	0 \|192\| 8 \| U_BTYE \| \| 2 \| 0 \|
195	0 \|192\| 9 \| V_BXS \| \| 0 \| 0 \|
196	0 \|192\| 10\| V_BXE \| \| 0 \| 0 \|
197	0 \|192\| 11\| V_BYS \| \| 0 \| 0 \|
198	0 \|192\| 12\| V_BYE \| \| 0 \| 0 \|
199	0 \|192\| 13\| V_BTXS \| \| 2 \| 0 \|
200	0 \|192\| 14\| V_BTXE \| \| 2 \| 0 \|
201	0 \|192\| 15\| V_BTYS \| \| 2 \| 0 \|
202	0 \|192\| 16\| V_BTYE \| \| 2 \| 0 \|
203	0 \|192\| 17\| W_BXS \| \| 4 \| 0 \|
204	0 \|192\| 18\| W_BXE \| \| 4 \| 0 \|
205	0 \|192\| 19\| W_BYS \| \| 4 \| 0 \|
206	0 \|192\| 20\| W_BYE \| \| 4 \| 0 \|
207	0 \|192\| 21\| W_BTXS \| \| 5 \| 0 \|
208	0 \|192\| 22\| W_BTXE \| \| 5 \| 0 \|
209	0 \|192\| 23\| W_BTYS \| \| 5 \| 0 \|
210	0 \|192\| 24\| W_BTYE \| \| 5 \| 0 \|
211	0 \|192\| 25\| PH_BXS \| \| -2 \| 0 \|
212	0 \|192\| 26\| PH_BXE \| \| -2 \| 0 \|
213	0 \|192\| 27\| PH_BYS \| \| -2 \| 0 \|
214	0 \|192\| 28\| PH_BYE \| \| -2 \| 0 \|
215	0 \|192\| 29\| PH_BTXS \| \| 0 \| 0 \|
216	0 \|192\| 30\| PH_BTXE \| \| 0 \| 0 \|
217	0 \|192\| 31\| PH_BTYS \| \| 0 \| 0 \|
218	0 \|192\| 32\| PH_BTYE \| \| 0 \| 0 \|
219	0 \|192\| 33\| T_BXS \| \| -1 \| 0 \|
220	0 \|192\| 34\| T_BXE \| \| -1 \| 0 \|
221	0 \|192\| 35\| T_BYS \| \| -1 \| 0 \|
222	0 \|192\| 36\| T_BYE \| \| -1 \| 0 \|
223	0 \|192\| 37\| T_BTXS \| \| 2 \| 0 \|
224	0 \|192\| 38\| T_BTXE \| \| 2 \| 0 \|
225	0 \|192\| 39\| T_BTYS \| \| 2 \| 0 \|
226	0 \|192\| 40\| T_BTYE \| \| 2 \| 0 \|
227	0 \|192\| 41\| MU_BXS \| \| 2 \| 0 \|
228	0 \|192\| 42\| MU_BXE \| \| 2 \| 0 \|
229	0 \|192\| 43\| MU_BYS \| \| 2 \| 0 \|
230	0 \|192\| 44\| MU_BYE \| \| 4 \| 0 \|
231	0 \|192\| 45\| MU_BTXS \| \| 4 \| 0 \|
232	0 \|192\| 46\| MU_BTXE \| \| 4 \| 0 \|
233	0 \|192\| 47\| MU_BTYS \| \| 4 \| 0 \|
234	0 \|192\| 48\| MU_BTYE \| \| 4 \| 0 \|
235	0 \|192\| 49\| QVAPOR_BXS\| \| 1 \| 0 \|
236	0 \|192\| 50\| QVAPOR_BXE\| \| 1 \| 0 \|
237	0 \|192\| 51\| QVAPOR_BYS\| \| 1 \| 0 \|
238	0 \|192\| 52\| QVAPOR_BYE\| \| 1 \| 0 \|
239	0 \|192\| 53\|QVAPOR_BTXS\| \| 6 \| 0 \|
240	0 \|192\| 54\|QVAPOR_BTXE\| \| 6 \| 0 \|
241	0 \|192\| 55\|QVAPOR_BTYS\| \| 6 \| 0 \|
242	0 \|192\| 56\|QVAPOR_BTYE\| \| 6 \| 0 \|
243	0 \|192\| 57\| QCLOUD_BXS\| \| 1 \| 0 \|
244	0 \|192\| 58\| QCLOUD_BXE\| \| 1 \| 0 \|
245	0 \|192\| 59\| QCLOUD_BYS\| \| 1 \| 0 \|
246	0 \|192\| 60\| QCLOUD_BYE\| \| 1 \| 0 \|
247	0 \|192\| 61\|QCLOUD_BTXS\| \| 7 \| 0 \|
248	0 \|192\| 62\|QCLOUD_BTXE\| \| 7 \| 0 \|
249	0 \|192\| 63\|QCLOUD_BTYS\| \| 7 \| 0 \|
250	0 \|192\| 64\|QCLOUD_BTYE\| \| 7 \| 0 \|
251	0 \|192\| 65\| QRAIN_BXS \| \| 1 \| 0 \|
252	0 \|192\| 66\| QRAIN_BXE \| \| 1 \| 0 \|
253	0 \|192\| 67\| QRAIN_BYS \| \| 1 \| 0 \|
254	0 \|192\| 68\| QRAIN_BYE \| \| 1 \| 0 \|
255	0 \|192\| 69\| QRAIN_BTXS\| \| 7 \| 0 \|
256	0 \|192\| 70\| QRAIN_BTXE\| \| 7 \| 0 \|
257	0 \|192\| 71\| QRAIN_BTYS\| \| 7 \| 0 \|
258	0 \|192\| 72\| QRAIN_BTYE\| \| 7 \| 0 \|
259	0 \|192\| 73\| QICE_BXS \| \| 2 \| 0 \|
260	0 \|192\| 74\| QICE_BXE \| \| 2 \| 0 \|
261	0 \|192\| 75\| QICE_BYS \| \| 2 \| 0 \|
262	0 \|192\| 76\| QICE_BYE \| \| 2 \| 0 \|
263	0 \|192\| 77\| QICE_BTXS \| \| 7 \| 0 \|
264	0 \|192\| 78\| QICE_BTXE \| \| 7 \| 0 \|
265	0 \|192\| 79\| QICE_BTYS \| \| 7 \| 0 \|
266	0 \|192\| 80\| QICE_BTYE \| \| 7 \| 0 \|
267	0 \|192\| 81\| QSNOW_BXS \| \| 2 \| 0 \|
268	0 \|192\| 82\| QSNOW_BXE \| \| 2 \| 0 \|
269	0 \|192\| 83\| QSNOW_BYS \| \| 2 \| 0 \|
270	0 \|192\| 84\| QSNOW_BYE \| \| 2 \| 0 \|
271	0 \|192\| 85\| QSNOW_BTXS\| \| 7 \| 0 \|
272	0 \|192\| 86\| QSNOW_BTXE\| \| 7 \| 0 \|
273	0 \|192\| 87\| QSNOW_BTYS\| \| 7 \| 0 \|
274	0 \|192\| 88\| QSNOW_BTYE\| \| 7 \| 0 \|
275	0 \|192\| 89\| QGRAUP_BXS\| \| 2 \| 0 \|
276	0 \|192\| 90\| QGRAUP_BXE\| \| 2 \| 0 \|
277	0 \|192\| 91\| QGRAUP_BYS\| \| 2 \| 0 \|
278	0 \|192\| 92\| QGRAUP_BYE\| \| 2 \| 0 \|
279	0 \|192\| 93\|QGRAUP_BTXS\| \| 7 \| 0 \|
280	0 \|192\| 94\|QGRAUP_BTXE\| \| 7 \| 0 \|
281	0 \|192\| 95\|QGRAUP_BTYS\| \| 7 \| 0 \|
282	0 \|192\| 96\|QGRAUP_BTYE\| \| 7 \| 0 \|
283	0 \|192\| 97\| QNICE_BXS \| \| 4 \| 0 \|
284	0 \|192\| 98\| QNICE_BXE \| \| 4 \| 0 \|
285	0 \|192\| 99\| QNICE_BYS \| \| 4 \| 0 \|
286	0 \|192\|100\| QNICE_BYE \| \| 4 \| 0 \|
287	0 \|192\|101\| QNICE_BTXS\| \| 7 \| 0 \|
288	0 \|192\|102\| QNICE_BTXE\| \| 7 \| 0 \|
289	0 \|192\|103\| QNICE_BTYS\| \| 7 \| 0 \|
290	0 \|192\|104\| QNICE_BTYE\| \| 7 \| 0 \|
291	0 \|193\|192\| FCX \| Relaxation term for boundary zone \| 4 \| 0 \|
292	0 \|193\|193\| GCX \| 2nd Relaxation term for boundary zone \| 4 \| 0 \|
293	0 \|193\|194\|MP_RESTART_STATE\|state vect for microphysics restarts \| 4 \| 0 \|
294	0 \|193\|195\|TBPVS_STATE\| state for etampnew microphysics \| 4 \| 0 \|
295	0 \|193\|196\|TBPVS0_STATE\| state for etampnew microphysics \| 4 \| 0 \|
296	1 \| 0 \| 1 \| SFROFF \| Storm surface runoff [kg/m^2] \| 4 \| 0 \|
297	1 \| 0 \|192\| SOILT1 \| Temperature inside snow \| 2 \| 0 \|
298	1 \| 0 \|193\| TSNAV \| Average snow temperature \| 2 \| 0 \|
299	1 \| 0 \|194\| UDROFF \| Baseflow-groundwater runoff [kg/m^2] \| 4 \| 0 \|
300	2 \| 0 \| 0 \| LANDMASK \| Land Cover (1=land,2=sea) \| 1 \| 0 \|
301	2 \| 0 \| 1 \| ZNT \| Time Varying Roughness length [m] \| 6 \| 0 \|
302	2 \| 0 \| 4 \| VEGFRA \| Vegetation [%] \| 1 \| 0 \|
303	2 \| 0 \| 7 \|HGT,SOILHGT,DIST\| Terrain Height [m] \| 2 \| 0 \|
304	2 \| 0 \|192\| LU_INDEX \| Land Use Index [Cat] \| 1 \| 0 \|
305	2 \| 0 \|193\| CANWAT \| Plant Canopy Surface Water [kg/m^2] \| 4 \| 0 \|
306	2 \| 0 \|194\| SNOWC \| Snow cover [%] \| 1 \| 0 \|
307	2 \| 0 \|195\| XLAND \| Land cover (land=1; sea=0) [fraction] \| 1 \| 0 \|
308	2 \| 0 \|196\| TOPOSTDV \| Standard Deviation of topography \| 3 \| 0 \|
309	2 \| 0 \|197\| TOPOSLPX \| Sub-gridscale mean topographic slope \| 6 \| 0 \|
310	2 \| 0 \|198\| TOPOSLPY \| Sub-gridscale mean topographic slope \| 6 \| 0 \|
311	2 \| 0 \|199\| SLOPECAT \| Topographical Categorical Slope \| 1 \| 0 \|
312	2 \| 0 \|200\| LANDUSEF \| Land use categorical fraction on mass gr \| 3 \| 0 \|
313	2 \| 0 \|201\| SOILCTOP \| Top layer soil type as a categ. fraction \| 3 \| 0 \|
314	2 \| 0 \|202\| SOILCBOT \| Bot layer soil type as a categ. fraction \| 3 \| 0 \|
315	2 \| 0 \|203\| RMOL \| 1./Monin Ob. Length [dimensionless] \| 2 \| 0 \|
316	2 \| 0 \|204\| SHDMAX \| Annual MAX veg fraction \| 3 \| 0 \|
317	2 \| 0 \|205\| SHDMIN \| Annual MIN veg fraction \| 3 \| 0 \|
318	2 \| 0 \|206\| Z0 \| Background Roughness length [m] \| 6 \| 0 \|
319	2 \| 0 \|207\| EMISS \| Surface Emissivity \| 4 \| 0 \|
320	2 \| 3 \| 0 \| ISLTYP \| Soil Type \| 1 \| 0 \|
321	2 \| 3 \| 1 \|TSLB,ST000010,ST010040,ST040100,ST100200\|Soil Temperature\|1\| 0 \|
322	2 \| 3 \| 2 \| SMSTOT \| Soil Moisture content [kg/m^2] \| 3 \| 0 \|
323	2 \| 3 \| 4 \| TMN \| Ground Reservoir Temperature \| 1 \| 0 \|
324	2 \| 3 \|192\| SOILW \| Volumetric soil moisture [fraction] \| 4 \| 0 \|
325	2 \| 3 \|193\| SOILL \| Liquid volumetric soil moisture[fraction]\| 4 \| 0 \|
326	2 \| 3 \|194\| SMSTAV \| Moisture availability [%] \| 4 \| 0 \|
327	2 \| 3 \|195\| IVGTYP \| Vegetation type \| 1 \| 0 \|
328	2 \| 3 \|196\| SOILCAT \| Soil Category \| 1 \| 0 \|
329	2 \| 3 \|197\| VEGCAT \| Vegetation Category \| 1 \| 0 \|
330	2 \| 3 \|198\| SH2O \| Soil liquid water [m^3/m^3] \| 3 \| 0 \|
331	2 \| 3 \|199\| SMOIS \| Soil moisture [m^3/m^3] \| 3 \| 0 \|
332	2 \| 3 \|200\| SNOALB \| Annual MAX snow albedor in fraction \| 4 \| 0 \|
333	2 \| 3 \|201\| SMFR3D \| Soil Ice \| 2 \| 0 \|
334	2 \| 3 \|202\|KEEPFR3DFLAG\| Flag - 1. Forzen Soil Yes, 0 - NO \| 1 \| 0 \|
335	2 \| 3 \|203\| CAPG \| Heat capacity for soil [j /(K m^3)] \| 0 \| 0 \|
336	10 \| 2 \| 0 \| XICE \| Ice Concentration [fraction] \| 1 \| 0 \|
337	10 \| 3 \| 0 \| SST \| Temperature \| 2 \| 0 \|
338	#
339	# Ind \| center \| subcenter \| Master Tbl Version \| Local Tbl Version \|
340	#-----+--------+-----------+--------------------+-------------------+
341	-1 \| 252 \| 255 \| 1 \| 1 \|
342	#
343	# Another table could go here.
344	#

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