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Proceedings - C-SRNWP Project

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In parallel, a direct radar observation operator has been developed and is used in case studies<br />

for reflectivity monitoring and model-to-reflectivity applications. The radar observation<br />

operator also allows to study and improve carefully the quality control checks to be operated<br />

later on in a routine operational manner. So far, conclusions are the following:<br />

►1D retrieval seems able to correct for humidity,<br />

►Quality control of data and observation operator evaluation (M. Jurašek, LACE)<br />

►Implementation in Arome is well advanced<br />

Future work:<br />

►More 1D + 3D-VAR high resolution cases<br />

►Perform cycled assimilation experiments,<br />

Collaborations:<br />

►Introduce beam blockage in observation operator (G. Haase, Hirlam)<br />

4. The Arome assimilation prototype: a R.U.C.<br />

Decision has been taken to start the preparation and the early evaluation of an Arome model<br />

based assimilation system in the context of a Rapid Update Cycle. The RUC typically is<br />

started 12 or 24 hours before the target initial time of interest, allowing thus for 5 to 9 3D-<br />

VAR data analyses in a 3-hourly frequency (13 to 25 in a 1-hourly mode). While we still wish<br />

to carefully evaluate the spin-up properties (especially in the 1 hour cycle), work also needs to<br />

be performed in order to tune the system with respect to data density. Also, in 2007, further<br />

case studies are planned, still focussing on severe cases of heavy precipitating events. Figure<br />

7 shows one such case, a typical strong event triggered by the advection of moist, warm air<br />

from the Mediterranean Sea over South-East of France. This air is orographically forced over<br />

the Cévennes mountain ridge, with some additional forcing from a synoptic upper-air trough.<br />

The result is a heavy convective mesoscale system, usually fairly stationary for several hours,<br />

which represents a major threat to the surrounding areas. Some critical aspects for a good<br />

forecast here are a good initial state for humidity, low level winds and the position and<br />

orientation of the upper air trough.<br />

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