7. Operational version in Czech Republic

(more details vana++at++chmi.cz)

Since 1st January 2003 every LACE Member exploits its own operational application of ALADIN. The recent ALADIN/LACE application operated in Prague LACE centre became the ALADIN/CE (CE standing for Central Europe) configuration of CHMI. In the beginning of 2003 it naturally kept its continuity with the previous LACE suite.

1. Evolution of the ALADIN/CE application

The ALADIN/CE suite switched to the version COCONUT+++ of the model physics :

27/05/2003 at 12 UTC network time for the production run and at 06 UTC network time for the assimilation cycle : COCONUT+++.

This physics package became operational in ARPEGE mid-April 2003. According to the original plan in Prague the switch to this model version was thought only for the end of June, together with the move to the new computer NEC-SX6 and to a higher cycle of ALADIN (AL25T1). However, with the start of warm season, the operational version CYCORA_ter+++ was not providing reasonable values of CAPE; these were extremely high. This fact together with the requirement of correct validation between the old cycle AL12 and the new one AL25T1 lead to the back-phasing of the COCONUT physics to the still operational cycle AL12 on the old computer NEC-SX4 (insufficient memory on the SX4 machine was the blocking factor). The COCONUT package was validated and gave the same results with both cycles. Meantime, already in March, the parallel testing started in comparison with the operational CYCORA_ter+++ version. These tests have shown that the COCONUT version as implemented in ARPEGE does not give completely satisfactory scores (at least neutral). For example, the bias of 2 m temperature got considerably worse, it became too cold (suite ABZ). Many other tests were made, see the description below. Finally, the satisfactory solution was found when coming back on the radiation scheme (+), on the nebulosity scheme (+) and on the horizontal diffusion coefficients (+) to the CYCORA_ter tunings.

Impact on the forecast : neutral scores, the CAPE values get reasonable compared to CYCORA_ter+++.

Technical impact : none.

The ALADIN/CE suite switched to cycle AL25T1 on new computer NEC-SX6 :

30/06/2003 at 12 UTC network time for the production run and at 06 UTC network time for the assimilation cycle : AL25T1 on NEC-SX6

In the beginning of 2003, CHMI purchased a new computer, the starting configuration is NEC-SX6/B with 4 processors and 32 Gbytes of shared memory (one node). The machine was installed in March and the acceptance tests were successfully completed on 10th June 2003. The switch of the complete ALADIN/CE suite took place on 30th June 2003, in its version COCONUT+++ on cycle AL25T1. As first future step, the resolution of ALADIN/CE will be increased.

Beside the model configurations needed for the operational suite, a considerable effort was put to the installation and validation of the ODB software. Not all ODB tools were however validated before the end of June.

Impact on the forecast : neutral.

Technical impact : important increase in the memory consumption due to the data flow, different from the old shared memory code.

2. Parallel suites

The following parallel tests were launched to assess the impact of different modifications:

  • - Suite ABY : It was the test of new tuning of the gravity-wave drag and orographic lift when the envelope orography is abandoned (following the study of Dunja Drvar). The scores were not satisfactory and the mean-sea-level pressure maps have shown that the drag and lift do not compensate enough the blocking effects of the envelope. Further study will take place.
  • - Suite ABZ : It tested the COCONUT version of physics; at the same time the horizontal diffusion intensity was increased twice. The scores were not the best. There was a too cold bias of 2m temperature, computed against SYNOP observations and compared to the operational version.
  • - Suite ACA : This test is based on the ABZ suite, but it comes back on the cloudiness scheme. The scores compared to ABZ are worse and they remain not satisfactory, compared to the operational version.
  • - Suite ACB : This suite should have been comparable to the model version known under the name DICORA (used in ARPEGE before COCONUT). The scores were not satisfactory either. Later on it was found that there was a mistake in leaving the switch LSRCONT =.true. (it should be switched off with DICORA).
  • - Suite ACC : This test was based on the COCONUT version (suite ABZ) however a different tuning was used for the mixing length. The goal was to find the reason of the worse scores of COCONUT. The results were not really changed by this retuning.
  • - Suites ACD, ACE, ACF : All these tests were based on the DICORA version, adding the shear-linked convection or using various tunings. The results were not better and they did not help much to discover the reason of the bad COCONUT scores. On top, all these tests were affected by the mistake (setup of LSRCONT ) made in the preparation of DICORA (suite ACB).
  • - Suite ACG : Since the DICORA version did not lead to any improvement or to any clue on the COCONUT scores, we came back to COCONUT in this test. On top of coming back to the operational version (CYCORA_ter) for the cloudiness scheme, the same was made for the radiation scheme. This test gave reasonably neutral scores for a trial period in winter. As it was a promising configuration, it was also re-tested for a summer period, this time even with a little improvement of the geopotential score. Within the summer period test it was noticed, however, that the field structures of humidity convergence or CAPE were not as sharp as in the operational version. Therefore several single case tests were made in order to see what could cause the damping.
  • - Single test ACI, ACJ, ACK: In these tests the convection tuning was modified (for parameters GCVPSI , GCOMOD, LSRCONT respectively) with respect to the ACG suite. The results (field structures) were almost the same as in case of ACG.
  • - Single test ACL : This test is based again on the ACG settings, but the horizontal diffusion coefficients were set back to the values of the operational version. Indeed, too strong diffusion in ACG was the reason of too smooth fields. Therefore it was decided to keep the horizontal diffusion tuning without change. The ACL settings then became operational on 27th May and it got the name COCONUT+++ (first (+) for cloudiness scheme, second (+) for the radiation scheme and third (+) for the horizontal diffusion).
  • - Suite ACH : This test was inspired by a study made with ARPEGE, where a better precision of computation of the semi-Lagrangian trajectory was tried (using three iterations instead of two in the trajectory computation). The test was based on the ACG suite and it was compared both with ACG and with the operational version. Surprisingly, the scores were worse in altitude, namely in bias of geopotential, which made worse also the RMSE geopotential score. This test was then left aside but perhaps some study can be later made around this issue.
  • - Suite ACM : test of the AL25T1 cycle with the COCONUT+++ settings on the SX6 machine. It was compared to the AL12 cycle with the COCONUT+++ settings on the SX4 machine (operational version since 27th May). The scores were perfectly neutral. The comparison was confirmed by the same result obtained for the 24 h cumulated precipitation forecast with both suites. The ACM suite became operational on the SX6 machine on 30th June 2003.
  • The results of parallel tests may be consulted on / pages.