Numerical Weather Prediction

ITSC19 NWP Survey

Please send updates or corrections to the NWP WG co-chairs. 

   Table 1    Overview 

InstituteData Assimilation SystemRadiative Transfer ModelATOVS assimilatedBias Correction SchemeStatus
(applies to all tables)
GlobalRegional or Km ScaleRadiancesRetrievalsRARS
//EC//
//(Canada)//
4DVAR & EnKF3DVARRTTOV8.7YESNONOOff-line//// 1 January 2012
//ECMWF//
(Europe)
Hybrid 4DVAR/EnsRTTOV10.1YESNOYESVAR7March 2014
met.no
(Norway)
3DVARRTTOV7YESNOYESOff-line1 January 2012
US-FNMOC/NRL
(USA)
4DVAR3DVARCRTMYESYES(RD)YESOff-line1 January 2012
//DWD//
(Germany)
3DVARnudgingRTTOV7YESNOYESOff-line//// 1 January 2012
//Met Office//
(UK)
Hybrid 4DVAR/Ens4DVARRTTOV7YESNOYESOff-line//// 1 January 2012
DMI
(Denmark)
3DVARRTTOV8.5YESNOYESOff-line1 March 2010
//JMA//
(Japan)
4DVAR4DVARRTTOV9.3YESNOYESVAR1 January 2012
//Meteo France//
(France)
4DVAR+Ens3DVARRTTOV9.2YESNOYESVAR//// 1 January 2012
//NCEP//
(USA)
3DVAR3DVARCRTMYESNOYESVAR1 January 2012
BoM
(Australia)
4DVAR4DVARRTTOV7YESNONOOff-line1 January 2012
CPTEC/INPE
(Brazil)
3DVAR3DVARN/ANOYESN/AN/A1 January 2012
//OMSZ//
(Hungary)
3DVARRTTOV8.5YESNOYESVAR1 January 2012
 SMHI
(Sweden)
  4DVAR RTTOV7 YESNONO Off-line 1 January 2012
 CNMCA
(Italy)
  LETKF RTTOV10.2 YESNO (monitoring)YES Off-line 1 January 2012
 KMA
(Korea)
4DVAR4DVARRTTOV7YESNOYESOff-line 1 January 2012
 NCMRWF
(India)
3DVAR CRTMYESNONOVAR 1 January 2012

G global
R
 regional
GD
 global deterministic
RD regional deterministic
                                                            Table prepared by ITWG/NWP WG                                                    

   Table 2     NWP Systems and Use of ATOVS

InstituteGlobalRegionalData assimilationRadiative transfer modelATOVS radiance assim (level)ATOVS retrievalsRARS
DeterministicEnsembleDeterministicEnsemble
EC
 (Canada)
35 km L80 (10d)66 km L40 (20m) (16d)15 km L80 (2d)
2.5 km L58
35 km L28 (3d)GD: 4D-Var T108 L80
GE: EnKF 100 km  L58 (192m)
RD: 3DVAR T200 L80
RTTOV 8.7Level 1b preprocessed to 1c with AAPPNONO
ECMWF (Europe)T1279 L137 (10d)T639 up to 10d, T319 d10-15, L62, 51m4D-Var T1279 L137 with T255 final inner loopRTTOV 10.1Level 1c (after antenna pattern correction)NOEARS, AP-RARS
met.no (Norway)8km L60 (2.75d),
12 km L60
3D-VarRTTOV 7Level 1cNOEARS
FNMOC/NRL (USA)T319 L42 (7.5d)T119 L30, 24m, 10dGD: 4D-Var-AR T119 L42
GE: 4D-Var-AR T119 L30
RD: 3D-Var 27/9/3 km
CRTMlevel 1b processed to level 1c with AAPPYes (RD)YES
DWD
(Germany)
20 km L60 (7d)7 km L40
2.8 km L50
2.8 km, 20m, 21hGD: 3D-Var
RD: nudging
RTTOV 7Level 1bNOYES (G)
Met Office
(UK)
25 km L70 (6d)60 km L70, 24m, 3d12 km L70
1.5 km L70
18 km, 24m, 2dGD: 4D-Var 60 km L70
RD 12 km: 4D-Var 24 km
RD 1.5 km:
3D-Var + Latent Heat nudging 1.5 km
RTTTOV 7Level 1b/1cNOEARS AP-RARS SA-RARS
DMI
(Denmark)
0.15 deg (16 km) L40 0.09 deg (10 km)
L40 0.03 deg (3.3 km)
L40 0.05 deg (5.6 km) L40
3D-VAR 0.15 deg L40
3D-Var 0.09 deg L40
3D-Var 0.09 deg L40
Inceremental
RTTOV 8.5Level 1c from AAPPNOEARS
JMA (Japan)T959 L60T319 L60 (51m) (9d)5 km L50T319 L60, 11m, 5dGD: 4D-Var T319 L60
RD: 4D-Var 15 km
RTTOV 9.3Level 1cNOEARS, AP-RARS, SP-RARS
Météo France (France)T798C2.4 L70 (4d)T538C2.4 L65 (35m)2.5 km L6025 km (35m) (4d)GD: 4D-Var+ensemble T323C1 L70
RD: 3D-Var 2.5 km
 
RTTOV 9.2
level 1cNOEARS, AP-RARS
NCEP
(USA)
T574 L64 (7.5d)
T190 L64 (16d)
T254L42, 84m, 1-8d
T190L42, 84m, 8-16d
12 km L60
4 km L50
16 km L35 (21m) (3.6d)GD: 3D-Var T574 L64
RD: 3D-Var 12 km
CRTMLevel 1bNOYes (G)
BoM
(Australia)
80 km L50 (10d)37.5 km L50GD: 4D-Var 100 km L50
RD: 4D-Var 75 km L50
RTTOV 7Level 1d from AAPP Met OfficeNONO
CPTEC/INPE (Brazil)45 km L64 (7d)100 km L28, 40m, 15d15 km L5020 km, 21m,  10dGD: 3D-Var 40 km
RD: 3D-Var 15 km
CRTMYESNOYES
OMSZ (Hungary)8 km L49 (2.25d)
2.5 km L60 (2d)
8 km (11m) L49 (2d)RD: 3D-Var 8 km L49
RD: 3D-Var 2.5 km L60
RTTOV 8.5Level 1cNOEARS
 SMHI
(Sweden)
   10 km L60  4D-Var RTTOV7 YES NO EARS
 CNMCA
(Italy)
  7 km L40
2.8 km L50
 R: LETKF 10 km RTTOV9.2 Level 1c NOEARS
 KMA
(Korea)
 25 km L70, 10.5d 40 km L70, 10d 12 km L70
1.5 km L70
  G: 4D-Var 75 km L70
R 12 km: 4D-Var 36 km L70
R 1.5 km: 3D-Var + FGAT
 RTTOV7 Level 1d from AAPP from Met Office NO EARS, AP-RARS, SA-RARS
 NCMRWF (India)T574L64    3DVARCRTM Level 1b NONO

CODES
         G
 Global
         R
 Regional
       GD
 Global deterministic
       RD
 Regional deterministic
       GE
 Global ensemble
       RE
 Regional ensemble
       Tn
 Truncation wavenumber
       Ln
 Number of levels
    (nd)
 number of days
   
 (nm) number of members   

Table 3    Use of ATOVS Radiances in NWP

CentreNWP Systems using ATOVSThinningBias Corr.Other PreprocAMSU-AAMSU-B/MHSHIRS
SatelliteChannelsSatelliteChannelsSatelliteChannels
N15N16N17N18N19AQMOland/seasea/low toposeaN15N16N17N18N19AQMOland/seasea/low toposeaN15N16N17N18N19AQMOland/seasea/low toposea
 EC
(Canada)
GD, RD, GEGD, RD: 150km
GE: 250km(1)
 HK off-line
dynamic (2)
screen for CLW
and precip
X X XXX X7-146 4-5X XX  X3-4  2,5       
 ECMWF
(Europe)
GD,GE125kmvariational X XXX X7-14 5-6    XX X3-5      X 124-7,11,
14,15
 met.no
(Norway)
RD
(HIRLAM)
50 km HK off-line
static
cloud clearingXX X    4-10                    
 FNMOC/NRL
(USA)
GD, GE140km(4)HK off-line
dynamic(5)
screen for high CLWXX  XX XX6-14  4-5 XXX  4-5          
DWD
(Germany)
GD200kmoff-line static(6)screen for CLW and precip. X  X X X   5-14                    
Met Office
(UK)
GD,RD, GE G=125/154km
R=80km
off-linecalibration
Remap to HIRS
X   X X  X 6-14 4-5X  XX X  3-5     G G   4-7,11
12,15
DMI
(Denmark)
RD (HIRLAM)0.9 deg (100km) HK off-line
static
 XX  X X X4-10(7)      X X X   3-5          
 JMA
(Japan)
GD,GEG: AMSU-A 250km,
AMSU-B 180km
R: 45 km
off-line for scan bias, remainder with variationalcloud/rain
classification
XX X XXX8-136-74-5 X  XX  X  3-5          
Météo France
(France)
GD,RD125km;
80 km IASI RD
 variational X X X X XX5-13(8,9)5-13 5-13X  X  X3-53-53-5   X  X X 124-7,11,
14,15
NCEP
(USA)
GD,RD G=145km
R=120km IR,
60km MW
 variational(10)X  X XX X1-13,15   X  X G X1-5     X X2-15  
BoM
(Australia)
GD,RDG=154km
R=80km
HK off-line(11)(12)  X  X X X7-14 64-5    X  X  3-5  X X  X X  4-7,11
12,15
 CPTEC/INPE
(Brazil)
GD, RD 145 km  X  XX X    X  X  X      X X X   
OMSZ
(Hungary)
 RD80kmvariational  XX  X   5-12   X  X   3-5            
 SMHI (Sweden) RD (HIRLAM) 0.9 degHK off-linestatic  X X        5-10                    
 CNMCA (Italy) RD R=120 km off-line dynamic Screen for CLW and precip  X  X X  X 7-10 5-6 5-10 (3)(3)(3)(3)(3)(3)(3)  3-45          
 KMA (Korea) GD, RD, GE G=154 km
R=80 km
off-line (120 X  X X X  X 7-14  4-14 X   X X X  3-5    X  X  X   2-8, 10, 15
 NCMRWF (India) GD  variational  X   X X X X 1-10, 12, 13   X  X X X 1-5     X X  X 2-15  

NOTE: All centres reject some channels from certain satellites for which the radiance data are known to be bad. These details are not provided here.

CODES
          G
 Global
          R
 Regional
        GD
 Global deterministic
        RD
 Regional deterministic
        GE
 Global ensemble
        RE
 Regional ensemble
 Nxx,XX
 NOAA-XX
        MO
 Metop
        AQ Aqua  

       off-line dynamic     bias corrections updated and applied to data before each analysis
     variational
              e.g VarBC, where bias corrections are computed during variational analysis as part of minimization
      HK                        
 Harris and Kelly type bias correction (thickness predictors)       
      sea/low topo
       assimilation over ocean and low topograohy land 
     CLW
                     cloud liquide water  

          NOTES  

                  (1)    Thinning to be reduced to 150 km (currently being tested)

                  (2)     Bias correction is off-line static for AMSU-A channels 11-14

                  (3)     AMSU-B/MHS assimilation is being tested

                  (4)     Start with taking every 4th point along scan, from every other scan line (skipping pattern to sample every scan point), then further reduce to approximately 140 km.

                  (5)     VarBC code developed, to be tested this spring.

                  (6)     Switch to an online bias correction scheme soon

                  (7)     Channels 4-5 not assimilated over sea ice

                  (8)     AMSU-A ch. 5-6 not assimilated over sea ice

                  (9)     AMSU-A channels in range 5-13 not assimilated: N15 (6,11) N16 (5-10,12) AQ (5-7) MO (7)

                (10)     Calibration and for RARS data removal of antenna correction (G), Calibration ( R )

                (11)     Bias correction soon to become offline adaptive

                (12)     Cailibration and pre-processing via AAPP at Met Office. Cloud detection, land/sea/ice determination in OPS pre-processor as part of Met Office UM suite.

   Table 4     Use of ATOVS Retrievals in NWP

CentreATOVS retrievals
Used in radiance assimilation e.g. QcAssimilatedNWP systemScheme/ProductVariable(s)Vertical resolutionHorizontal samplingExcludedBias correction
 EC
(Canada)
 NO NO       
ECMWF
(Europe)
NO NO       
met.no
(Norway)
 NONO       
FNMOC/NRL
(USA)
NOYESRD (COAMPS, NAVDAS) NESDISTemperatureFull to 10 mb1.5 degrees
(167 km)
over landNO
DWD
(Germany)
NO NO       
Met Office
(UK)
YES (1) (in GD) NO       
DMI
(Denmark)
NO NO       
 JMA
(Japan)
NONO 
Météo France
(France)
NONO       
 NCEP
(USA)
NO NO       
BoM
(Australia)
YES (2)NO       
CPTEC=INPE
(Brazil)
NONO      
OMSZ
(Hungary)
NO NO       
 SMHI
(Sweden)
         
 CNMCA
(Italy)
 NONO RD EUMETSATTemperatureUp to 10 hPa   
 KMA
(Korea)
 YES NO       
 NCMRWF
(India)
 NONO       

NOTES

(1) Run 1D-var prior to assimilation which analyses skin temperature and for advanced IR sounders cloud cover and emissivity which is used in the forward calculations in 4D-var.

(2)
1D-Var

Table 5       Use of AIRS and IASI Radiances in NWP

Note: For some centres, further information on channel numbers and observation errors for AIRS and IASI can be found at the end of this document. Also, please note the definitions of the bands below the table.  

CentreAIRSIASI
15 microns (1)Window + O3 (2)H2O (3)Short Wave (4)15 microns (1)Window + O3 (2)H2O (3)Short Wave (4)
LandOceanLandOceanLandOceanLandOceanLandOceanLandOceanLandOceanLandOcean
 EC
(Canada)
 4 190 1026 330 2414 430 190 00 0
 ECMWF
(Europe)
 48 81 0 32 0 7 0 19 0 153 0 28 0 9 0 1 (*)
 met.no
(Norway)
                
 FNMOC/NRL
(USA)
 31 51      13 25 51      
 DWD
(Germany)
                
 Met Office
(UK)
 46 75 0 19 0 47 0 0 87 87 14 21 30 30 0 0
 DMI
(Denmark)
                
 JMA
(Japan)
                
 Meteo France
(France)
 0 54 0 0 0 0 0 0 50 64 0 4 9 9 0 0
 NCEP
(USA)
 75 75 11 11 20 20 14 14 116 116 45 45 4 4  
 BoM
(Australia)
  20  12  16  14        
 CPTEC/INPE
(Brazil)
                
 SMHI
(Sweden)
                
 CNMCA
(Italy)
                
 KMA
(Korea)
 0 20 0 11 0 16 0 0 95 124 0 29 24 30 00
 NCMRWF
(India)
 75  11  20  14  116  45  4   

Notes:

(1) 15 microns: 650 – 770 cm^-1

(2) Window + 03: 770 – 1210 cm^-1

(3) H2O: 1210 – 2000 cm^-1

(4) Short wave: 2000 – 2700 cm^-1

(*) Channel 5480 – this is really a WV channel, but falls into the short-wave band in the above categorisation. 

Table 6      Treatment of cloudy sounder radiances in NWP

CentreHIRSAIRSIASIAMSU-AAMSU-B/MHS
EC
(Canada)
n/aICICICIC
 ECMWF
(Europe)
 IC & SVIC & SVIC & SVICIC
 met.no
(Norway)
     
 FNMOC/NRL
(USA)
 n/a ICICICIC
 DWD
(Germany)
   HH 
 Met Office
(UK)
 HHSV
(with dynamic selection of weakly cloud-affected channels)
SV
(with dynamic selection of weakly cloud-affected channels)
ACIC
 DMI
(Denmark)
     
 JMA
(Japan)
    ICIC
Meteo France
(France)
 ICIC & SVIC & SV IC IC
 NCEP
(USA)
ICICICIC IC
 BoM
(Australia)
 HHHH ICIC
 CPTEC/INPE
(Brazil)
     
 SMHI
(Sweden)
     
 KMA
(Korea)
  ICIC  
 NCMRWF
(India)
     

Notes:

HH: Hole hunting: search for FOVS for which all channels are clear, and only assimilate these clear-sky radiances. Cloud-affected radiances are not assimilated.

IC: Insensitive channels: search for channels and spots which are considered clear, and only assimilate these clear radiances; clouds might be present for lower-peaking channels, but only channels insensitive to these clouds are assimilated. Cloud-affected radiances are not assimilated.

CC: Cloud clearing: method to transform potentially cloud-affected observed radiances to clear radiances, and then assimilate these modified radiances.

SV: Sink variable: cloud parameters are retrieved or analysed as a sink variable in 1D/3D/4D-Var, allowing the assimilation of certain cloud-affected radiances. The retrieved or analysed cloud information does not directly affect the model cloud fields.

AC: Assimilate clouds: assimilation of cloud-affected radiances, using information from model clouds and with feedback on model clouds.

Additional information

Some centres have kindly provided further information on channel usage and observation errors, especially for AIRS and IASI, but occasionally also for other instruments. These are provided below:

EC (Canada) as of 1 January 2012

FNMOC/NRL (USA) AMSUA AIRS AQUA and IASI METOPA as of 1 January 2012

Meteo France (France) as of 1 January 2012

NCEP (USA) as of 1 January 2012