Proceedings - C-SRNWP Project
Proceedings - C-SRNWP Project
Proceedings - C-SRNWP Project
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Data Assimilation for LM<br />
Method: Nudging towards observations<br />
Implementation: Continuous cycle<br />
Analyzed variables: horizontal wind vector, potential temperature, relative humidity, 'nearsurface'<br />
pressure (i.e. at the lowest model level)<br />
Observations:<br />
SYNOP, SHIP,DRIBU: station pressure, wind (stations below 100m above msl) and humidity<br />
TEMP,PILOT: wind,temperature: all standard levels up to 300 hPa; humidity:all levels up to<br />
300 hPa; geopotential used for one “near-surface” pressure increment.<br />
AIRCRAFT: all wind and temperature data<br />
WIND PROFILER: all wind data (not included in blacklisted stations)<br />
Quality Control: Comparison with the model fields from the assimilation run itself.<br />
A Latent Heat Nudging scheme is also implemented for testing.<br />
3. Recent developments.<br />
During this last year, five new version of LM have been released. The present one is the<br />
version 3.21 which is going to became the future LM reference version 4.1. The most<br />
relevant changes with respect to last year are:<br />
– The implementation of snow density to the multilayer soil model<br />
– Some changes and tuning in the assimilation scheme. Much work has been<br />
done to allow the assimilation of temperature and humidity profiles retrieved<br />
from satellite data by means of a 1-DVAR technique (1-DVAR Special<br />
<strong>Project</strong>). This scheme is now under tuning and extensive testing.<br />
– The implementation of the FLake Model<br />
– Some changes to Runge-Kutta Scheme (RK Priority <strong>Project</strong>)<br />
– The complete harmonization with the LMK code<br />
– The adaptation of the code and of the input files to support the run of LM in<br />
Ensemble Mode by parameters perturbations (SREPS Special <strong>Project</strong>)<br />
Another important and relevant upgrading of LM was the Climate Mode extension of the code<br />
to allow and support the use of the model in climate applications. Major changes were related<br />
to the restart of the model and to the output now available also in NetCDF format. This<br />
cooperation with the CLM group already gave some useful feedbacks to the COSMO<br />
community highlighting some technical inconsistencies and bugs of the model and testing the<br />
long-term behaviour of LM. For more information see the presentation by Andrea Will<br />
available at the 2006 COSMO general Meeting WEB site.<br />
4. LM operational applications.<br />
The LM runs operationally at the different COSMO Countries. The operational integration<br />
domains, the correspondent horizontal resolution and the driving models are reported in figure<br />
1.<br />
For more details please see the national reports in this Newsletter issue.<br />
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