|
|
EPS forecasts are ran
at TL639 resolution at 62 levels up to day 10 and with grid point
data being generated on reduced Gaussian grid N320. EPS forecasts
are ran at TL319 resolution at 62 levels from time step 246 to day
15 with grid point data being on reduced Gaussian grid N160s. In
addition, two calibration/validation forecasts are ran, one at T639
L62 (forecast NUMBER=1) and the other at T319 L62 (forecast
NUMBER=2). Data is post-processed every 3 hours to time step 144
and 6 or 12 hourly to day 15 (depending on a parameter). Step 0 is
included. Parameters available in dissemination are listed in the
Table 5.1 below.
Flux fields are
quantities accumulated since the beginning of the forecast, e.g.
all precipitation and snowfall parameters. Reducing the resolution
of the model at step T+240 requires interpolation between Gaussian
grids used in leg 1 (N320) and leg 2 (N160). As a consequence,
noise will appear in flux fields when taking differences in time
for timestep intervals starting from T+240 or spanning T+240, e.g.
precipitation for the interval T+(252-240) or T+(246-234).
To limit unnecessary
impact from interpolation on the consistency of the fields, users
wishing to extend their applications to day 15 are advised as
follows:
1. Applications
requiring products starting from or spanning step T+240 users
should specify the keyword GAUSSIAN = REDUCED, GRID = 160 in the
dissemination request. This will provide the user with all fields
on the original model grid of VarEPS leg 2.
2. For applications
requiring products starting from or spanning step T+240 users
wishing to obtain products interpolated to regular lat/lon grids
are advised to have the products from leg 1 truncated to the N160
grid prior to interpolation to their choice of lat/lon grid. This
can be achieved by specifying an additional key word, e.g. RESOL =
REDUCED GAUSSIAN 128, GRID = 0.5/0.5 in the dissemination requests.
This new feature of requesting the truncation of Gaussian grids
prior to further interpolation to regular grids will also become
available in MARS.
3. New applications
only using data starting from step T+246 will not be affected by
interpolation problems described above.
Model
levels, pressure levels and surface products
Horizontal
resolution
- 0.25 x 0.25
degrees latitude-longitude grid, or multiples thereof (leg 1)
- 0.5 x 0.5 degrees
latitude-longitude grid, or multiples thereof (leg 2)
- spectral
truncation appropriate to the forecast model in use.
- the Gaussian grid
appropriate to the forecast model in use. The following Gaussian
grid numbers are supported: 320, 200, 160, 128, 80, 48 and 32 (200
and 160 only for leg 1 data).
- any sub-area
Vertical
resolution
- pressure levels
(depending on the specific parameter and the forecast time step):
1000,925,850,700,600,500,400,300,250,200,150,100,70,50,30,20,10,7,5,3,2,1
hPa;
- model levels:
currently 62 hybrid coordinate level.
Verifying times
-T+0 to T+144 at 3
hour intervals and T+150 to T+360 at 6 hour intervals;
- Upper air
parameters on model levels as well as parameters on `potential
temperature' level for perturbed forecast, T+0 to T+144 at 3 hour
intervals and T+150 to T+168 (inclusive) at 6 hour intervals;
- * Orography field
is defined as parameter Z on model level 1 + Control forecast
only
- Table 5.1 Control
and Perturbed forecast products
|
FIELD CODE
|
MARS ABBREV.
|
FIELD NAME
|
UNITS
|
NO. OF BITS/VAL.
|
|
3
|
PT
|
Potential
Temperature
|
K
|
16
|
|
33
|
RSN
|
Snow Density
|
kg m**-3
|
16
|
|
39
|
SWVL1
|
Volumetric Soil
Water layer 1
|
m3m-3
|
12
|
|
40
|
SWVL2
|
Volumetric Soil
Water layer 2
|
m3m-3
|
12
|
|
41
|
SWVL3
|
Volumetric Soil
Water layer 3
|
m3m-3
|
12
|
|
42
|
SWVL4
|
Volumetric Soil
Water layer 4
|
m3m-3
|
12
|
|
49
|
10FG
|
Wind gust at 10
meters
|
m/s
|
16
|
|
54
|
PRES
|
Pressure
|
Pa
|
16
|
|
59
|
CAPE
|
Convective available
potential energy
|
JKg-1
|
16
|
|
60
|
PV
|
Potential Vorticity
+
|
m2s-1Kkg-1
|
16
|
|
121
|
MX2T6
|
Max. temp. at 2m in
the past 6hours
|
K
|
12
|
|
122
|
MN2T6
|
Min. temp. at 2m in
the past 6hours
|
K
|
12
|
|
123
|
10FG6
|
Wind gust at 10m in
the past 6hours
|
m/s
|
16
|
|
129
|
Z
|
Geopotential*
|
m2s-2
|
16
|
|
130
|
T
|
Temperature
|
K
|
12
|
|
131
|
U
|
U-velocity
|
m/s
|
12
|
|
132
|
V
|
V-velocity
|
m/s
|
12
|
|
133
|
Q
|
Specific
humidity
|
kg/kg
|
12
|
|
135
|
W
|
Vertical
velocity
|
Pa/s
|
16
|
|
138
|
VO
|
Vorticity
|
s-1
|
16
|
|
139
|
STL1
|
Soil Temperature
Level 1
|
K
|
12
|
|
141
|
SD
|
Snow depth
|
m
|
12
|
|
142
|
LSP
|
Large scale
precipitation
|
m
|
16
|
|
143
|
CP
|
Convective
precipitation
|
m
|
16
|
|
144
|
SF
|
Snow fall
|
m
|
16
|
|
145
|
BLD
|
Boundary Layer
Dissipation
|
|
|
|
146
|
SSHF
|
Surface sensible
heat flux ++
|
Wm-2s
|
12
|
|
147
|
SLHF
|
Surface latent heat
flux
|
Wm-2s
|
12
|
|
151
|
MSL
|
Mean sea level
pressure
|
Pa
|
12
|
|
152
|
LNSP
|
Log surface
pressure
|
-
|
12
|
|
155
|
D
|
Divergence
|
s-1
|
16
|
|
157
|
R
|
Relative
humidity
|
-
|
8
|
|
159
|
BLH
|
Boundary Layer
Height
|
m
|
16
|
|
164
|
TCC
|
Total cloud
cover
|
(0-1)
|
8
|
|
165
|
10U
|
10 metre U
|
m/s
|
12
|
|
166
|
10V
|
10 metre V
|
m/s
|
12
|
|
167
|
2T
|
2 metre
temperature
|
K
|
12
|
|
168
|
2D
|
2 metre dewpoint
temperature
|
K
|
12
|
|
169
|
SSRD
|
Surface solar
radiation downwards
|
W m**-2 s
|
16
|
|
170
|
STL2
|
Soil Temperature
Level 2
|
K
|
12
|
|
172
|
LSM
|
Land/sea mask +
|
(0,1)
|
8
|
|
176
|
SSR
|
Surface Solar
Radiation
|
W m**-2 s
|
16
|
|
177
|
STR
|
Surface Thermal
Radiation
|
W m**-2 s
|
16
|
|
178
|
TSR
|
Top Solar
Radiation
|
W m**-2 s
|
16
|
|
179
|
TTR
|
Top Thermal
Radiation
|
W m**-2 s
|
16
|
|
180
|
EWSS
|
U-stress*
|
Nm**-2
|
12
|
|
181
|
NSSS
|
V-stress*
|
Nm**-2
|
12
|
|
182
|
E
|
Evaporation
|
m of water
|
16
|
|
183
|
STL3
|
Soil Temperature
Level 3
|
K
|
12
|
|
189
|
SUND
|
Sunshine
duration
|
s
|
16
|
|
197
|
GWD
|
Gravity Wave
Dissipation
|
W m**-2 s
|
16
|
|
198
|
SRC
|
Skin reservoir
content
|
m (ofwater)
|
12
|
|
201
|
MX2T
|
Max. temp. at 2m
since prev. post-processing
|
K
|
12
|
|
202
|
MN2T
|
Min. temp. at 2m
since prev. post-processing
|
K
|
12
|
|
228
|
TP
|
Total
precipitation
|
m
|
16
|
|
235
|
SKT
|
Skin temperature
|
K
|
12
|
|
236
|
STL4
|
Soil Temperature
Level 4
|
K
|
12
|
|
238
|
TSN
|
Temperature of snow
layer
|
K
|
16
|
|
246
|
CLWC
|
Cloud liquid water
content
|
Kg/Kg
|
12
|
|
247
|
CIWC
|
Cloud ice water
content
|
Kg/Kg
|
12
|
|
246.228
|
100U
|
100 metre U wind
component
|
m/s
|
16
|
|
247.228
|
100V
|
100 metre V wind
component
|
m/s
|
16
|
Potential
temperature and potential vorticity levels
Potential Vorticity
level products (Table 5.1) are available on 3 hour intervals 0-144
and 6 hour intervals 150 to 360 and on the level 2000 as:
- control, perturbed
and calibration/validation forecast products, parameters PT,
PRES, Z, U, V and
Q;
Potential Temperature
(Isentropic) level products (Table 5.1) are available on 3 hour
intervals 0-144 and 6 hour intervals 150 to 168 as:
- control, perturbed
and calibration/validation forecast products, parameters PV,
PRES, VO and D,
levels 300, 315, 330, 350,370, 395, 475, 600 and 850;
Control,
Perturbed and Calibration/Validation forecast requirements
The following command
language parameters are specific for the control and perturbed
forecast requirements. Other DIS parameters are listed under the
general EPS requirements above.
|
TYPE
|
=
|
CONTROL FORECAST
PERTURBED
FORECAST
CALIBRATION
VALIDATION
|
[CF]
[PF]
[CV]
|
|
DOMAIN
|
=
|
GLOBAL
|
[G]
|
(default)
|
|
NUMBER
|
=
|
n-ENSEMBLE
NUMBER
|
[1-50]
off
[1-2]
|
(for TYPE=PF)
(for TYPE=CF)
(for TYPE=CV)
|
|
LEVTYPE
|
=
|
PRESSURE LEVEL
POTENTIAL
VORTICITY
POTENTIAL
TEMPERATURE ]
|
[PL]
[PV]
[PT]
|
|
LEVELIST
|
=
|
* (value of
pressure)
1000/850/700/500/200
NB ALL is not
permitted
(See 5.4.2 for
LEVTYPE=PT/PV products);
(1 - 62 for
LEVTYPE=ML)
|
|
GRID
|
=
|
*
*/*
AUTOMATIC [AUTO]
If the form a/b is
used, a latitude-longitude grid is defined, where:
a= grid resolution
(deg.) along a latitude line (i.e. East/West)
b= grid resolution
(deg.) along a longitude line (i.e. North/South)
0.25/0.25 or
multiples thereof (leg 1);
0.5/0.5 or
multiples thereof (leg 2);
If a single
positive integer is coded, it is interpreted as Gaussian grid
number for grids defined as GAUSSIAN=REDUCED or REGULAR. The
following Gaussian grid numbers are supported: 320, 200, 160, 128,
80, 48 and 32 (320 and 200 only for leg 1 data);
AUTOMATIC - values
for the parameter GRID will be defined automatically based on
STREAM/DOMAIN as well as RESOL/ GAUSSIAN parameter values;
|
|
STEP
|
=
|
* (hours)
l gives forecast
time step(s);
00/TO/144/BY/3
150/TO/360/by/6
(Dissemination
requirements validation tool provides detailed log on the
availability of each
specific product)
NB ALL, is not
permitted.
|
|
PARAM
|
=
|
Field name
abbreviation
*
NB ALL is not
permitted.
Available
parameters are listed in the Table 5.1.
|
GRIB
section 1 definition for Control, Perturbed and
Calibration/Validation forecast products
By convention, ECMWF
always uses octet 41 to define which set of local definitions
follow. The set of local definitions for EPS Control and Perturbed
forecast fields:
- Table 5.2 GRIB
section 1 definition for Control and Perturbed forecast
products
|
Octet
|
Ksec1 element
|
Contents
|
|
41
42
43
|
37
38
39
|
ECMWF local GRIB use
definition identifier.
30 = Ensemble
forecast data.
Class:
1 = Operations
Type:
10 = Control
forecast
11 = Perturbed
forecast
|
|
44-45
46-49
|
40
41
|
Stream:
1035 = Ensemble
forecasts
Version number or
experiment identifier.
(4 ASCII characters,
right justified)
|
|
50
|
42
|
Number:
Set to 0 for MARS
labelling (simple labelling)
When element 40 =
1035, this is the ensemble forecast number.
When element 39 =
10, this is the control forecast number and is set to 0.
|
|
51
52
53
|
43
44
45
|
The total number of
forecasts in an ensemble; the
number includes the
control forecast.
Ocean Atmosphere
Coupling
Reserved . Set to
0.
|
|
54-55
56-59
60-61
|
-
46
47
|
Padding
Leg base Date (in
format YYYYMMDD)
Leg base Time (in
format hhmm)
|
|
62
63-66
|
48
49
|
Leg Number
Reserved . Set to
0.
|
|
67-70
71-74
75-106
|
50
51
|
Climate date - from
(YYYYMMDD)
Climate date - to
(YYYYMMDD)
Reserved . Set to
0.
|
|