Documentation of the Changes in COSMO-Model 4.3

25.02.2008

In this version, the computation of some diagnostic fields has been changed in the turbulence. Also, some technical adaptations have been done.

Contents:

  1. Documentation of the Changes
  2. Summary of new and obsolete Namelist Variables
  3. Changes of the Results


1. Documentation of the Changes

Changes in the computation of the 2m temperature (by Matthias Raschendorfer)

The interpolation to the diagnostic levels has been changed. In particular, no more exponential canopy profile is assumed, but a diagnostic Prandtl layer interpolation is used even for scalars, using an adopted canopy layer resistance (and standard SYNOP lawn).

Note: Because the 2m temperature is used in the soil model, these changes do influence not only the results of the field T_2M, but also the whole forecast.

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Changes in the computation of synthetic satellite images (by Ulrich Schättler)

On February 18th, the COSMO_EU got a hard limit violation of the surface pressure for the RTTOV library: the model pressure was 1100.14 hPa!! But this was at the Death Sea, which is not too unrealistic, because there were rather cold temperatures by that time. Now, the surface pressure given to the RTTOV-library is limited by 1100 hPa (which is the hard limit).

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Technical adaptations and bug fixes

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New fields and grib numbers

Some new fields have been introduced to the COSMO-Model (for later use) and some fields now got official GRIB numbers.

Name Element Number Table Number Comment
EDR151201Eddy dissipation rate
TINC_LH32 202 needed for restart files
HORIZON 96 202 fields for topographical corrections
SWDIR_COR 97 202
SLO_ANG 98 202
SLO_ASP 99 202
SKYVIEW 100 202
ASWDIR_S 22 201
ASWDIFD_S 23 201
ASWDIFU_S 24 201
ALWD_S 25 201
ALWU_S 26 201
PRH_GSP 134 201 new moisture variables
HAIL_GSP 135 201
QH 98 201
QNC 221 201
QNR 222 201
QNI 223 201
QNS 224 201
QNG 225 201
QNH 226 201

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2. Summary of new Namelist Variables

There were no changes regarding Namelist variables:

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3. Changes of Results

The changes in the computation of the 2m temperature also influence the whole forecast, because it is used as input to the soil model.

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