ERA-interim
The ERA-interim dataset comprise a large amount of reanalysis data covering years 1989-2008, created by
the European Centre for Medium-Range Weather Forecasts.
A comprehensive description of the ERA-interim dataset can be found at http://www.ecmwf.int/research/era/do/get/era-interim.
Data available at NoSerC
A part of the ERA-interim dataset is now available on the national storage facility NorStore.
Please send an E-mail to Egil Støren at met.no if you want access to these data.
Surface or single level parameters in 0.5° x 0.5° resolution |
Parameters at 60 model levels in 1° x 1° resolution |
Fields based on analysis:
10U 10 metre U wind component (m s**-1)
10V 10 metre V wind component (m s**-1)
2D 2 metre dewpoint temperature (K)
2T 2 metre temperature (K)
CI Sea-ice cover (0 - 1)
MSL Mean sea level pressure (Pa)
SKT Skin temperature (K)
SP Surface pressure (Pa)
STL1 Soil temperature level 1 (K)
STL2 Soil temperature level 2 (K)
STL3 Soil temperature level 3 (K)
STL4 Soil temperature level 4 (K)
SWVL1 Volumetric soil water layer 1 (m**3 m**-3)
SWVL2 Volumetric soil water layer 2 (m**3 m**-3)
SWVL3 Volumetric soil water layer 3 (m**3 m**-3)
SWVL4 Volumetric soil water layer 4 (m**3 m**-3)
TCC Total cloud cover (0 - 1)
Accumulated fields based on forecast:
These fields are based on accumulated fields from forecast runs at 00 and 12 UTC.
For each variable, four fields are computed for each day. These are identified
by "Hour of reference time of data" (RT) = 0 or 12, and "Time range one" (T1) = 6 or 12.
The (RT,T1) combinations (0,6) (0,12) (12,6) and (12,12) corresponds to six hour accumulated
values from UTC 00, 06, 12 and 18 respectively. Originally, the (0,12) and (12,12) fields
contained 12 hour accumulated values from reference time, but the corresponding (0,6) and
(12,6) fields have been substracted in order to obtain an homogenous time series with six
hour accumulated values.
SSRD Surface solar radiation downwards (W m**-2 s)
TP Total precipitation (m)
Other surface level variables based on forecast:
BLH Boundary layer height (m)
Constant surface fields:
Land-sea mask (0 - 1)
Surface geopotential (m**2 s**-2)
|
Fields based on analysis:
D Divergence (s**-1)
T Temperature (K)
VO Vorticity (relative) (s**-1)
Z Geopotential (m**2 s**-2)
|
|