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Contract Number HPRN-CT-1999-00057
Core Project Title ALADIN Training NETtwork
Acronym ALATNET
Start Date 01/03/2000
Finish Date 29/02/2004
Duration 48
Objectives ALATNET (ALADIN Training NETwork) aims at diversifying and widening the international research effort around the Numerical Weather Prediction (NWP) Limited Area Model ALADIN. This software is currently used both for daily short-range weather forecast (15 operational versions exist, most of them running in dynamical adaptation mode) and for research purposes.
The research effort was focused on the following topics: non-hydrostatic modelling of the atmospheric flow, diabatic forcing at small scales (when both "resolved" and "parameterized" computations mix their effects), parameterisation of surface processes, coupling strategies for high resolution applications and continuous data assimilation, use of the optimal control formalism to assimilate meteorological observations at the finest possible scales, development of interfaces to new types of remote-sensed data, noise control in both model runs and data assimilation procedures.
None of this topic, taken individually, was likely to be the vector for a complete breakthrough in atmospheric science. But all of them were required steps for the basic objective : to built the ALADIN NWP system up to a state where it can treat the dynamics and physics of atmospheric phenomena at scales down to 10 km and where it can assimilate in a continuous and balanced mode all relevant data for the prediction of extreme weather events.
Partnerships Till before ALATNET the basic training courses and the scientific progress around ALADIN were centralized in Toulouse and widely supported by Météo-France. However local training actions had developed along the last years and a few decentralized research units emerged.
ALATNET offered the opportunity to go further towards the decentralization of scientific initiative and training effort, while facing the current main scientific challenges of NWP.
The research efforts were distributed among 5 leading centres (in Toulouse, Brussels, Prague, Budapest and Ljubljana) and were opened to a closer cooperation with other European NWP teams (UK, Italy) through a broader welcome of students.
The coordination of scientific developments and training actions received special care so that they would benefit equally to all partners and preserve the main properties of the software (portability, flexibility, generality, modularity), which ensure that every option remains available to every NWP ALADIN partner team.

Applications (A) Links with operations:
Most results of the work on physical parameterisations have already an operational application in several ALADIN applications. Blending assimilation is now operational in a few of them as well and full 3D-Var is in test at two places. But the most spectacular outcome is perhaps the now planned application of the non-hydrostatic ALADIN option in about twenty-five Euro-Mediterranean countries thanks to the choice of the HIRLAM group to join forces with us on this issue.
(B) Publications (extended abstracts and papers):
(i) Gospodinov, I., V. Spiridonov, P. Bénard and J.-F. Geleyn, 2002 : A refined semi-Lagrangian vertical trajectory scheme applied to a hydrostatic atmospheric model. Q. J. R. Meteorol. Soc.. (ii) Siroka, M., G. Boloni, R. Brozkova, A. Dziedzic, C. Fischer, J.-F. Geleyn, A. Horanyi, W. Sadiki and C. Soci, 2001 : Innovative developments for a 3D-Var analysis in a Limited Area Model: scale selection and blending cycle. Research activities in atmospheric and oceanic modelling. (iii) Soci, C., A. Horanyi and C. Fischer, 2003: High resolution sensitivity studies using the adjoint of the ALADIN mesoscale numerical weather prediction model. Idöjaras. (iv) Brozkova, R., D. Klaric, S. Ivatek-Sahdan, J.-F. Geleyn, V. Cassé, M. Siroka, G. Radnoti, M. Janousek, K. Stadlbacher and H. Seidl, 2001 : DFI blending: an alternative tool for preparation of the initial conditions for LAM. Research activities in atmospheric and oceanic modelling. (v) Siroka, M., C. Fischer, V. Cassé, R. Brozkova and J.-F., Geleyn, 2002: The definition of mesoscale selective forecast error covariances for a limited area variational analysis. Meteorology and Atmospheric Physics. (vi) Bénard, P., 2003: Stability of semi-implicit and iterative centred-implicit time discretisations for various equation systems used in NWP, Mon. Wea. Rev.. (vii) Bénard, P., 2004: On the use of a wider class of linear systems for the design of constant coefficients semi-implicit time-schemes in NWP. Mon. Wea. Rev.. (viii) Bénard, P., R. Laprise, J. Vivoda and P. Smolikova, 2004: Stability of leap-frog constant-coefficient semi-implicit schemes for the fully elastic system of Euler equations; flat-terrain case. Mon. Wea. Rev. (ix) Termonia, P., 2003: Monitoring and improving the temporal interpolation of lateral-boundary-coupling data for limited-area models. Mon. Wea. Rev..
Training Aspects ALATNET offered pre-Doc and post-Doc positions in 5 teams : at Météo-France (only pre-Doc), IRM (only post-Doc), CHMI, HMS (only pre-Doc) and HMIS (only pre-Doc) respectively.
Research topics were distributed so that each centre may specialize, but responsibilities in each of the three historical research directions for NWP (dynamics and numerical methods, physical parameterisations, data assimilation) were shared by at least two teams. This enabled a larger choice for students, a wider spreading of experience and a better control of the project completion.
The French team is part of large research institute and benefited from experience in NWP at the global scale, but the smaller teams allowed a closer contact with operational weather prediction.
Theoretical training courses, exploring the leading-edge topics of NWP (high-resolution modelling, data assimilation, numerical methods) and open to the whole European NWP community, were organized regularly and completed the local, practical, training for newcomers.
Results After the four years of activity of ALATNET the following results have been registered.
(A) Research actions:
(i) In the part concerning the non-hydrostatic formulation: (a) the semi-implicit three-time-level semi-Lagrangian version of ALADIN has been stabilised (it was thus the first or second version of this type in the world to run with Courant numbers bigger than one) while the search for a more and more optimal choice of prognostic variables led to a mixed prognostic-diagnostic solution that gives a theoretical explanation for the (up to now) empirically justified technique used in the Canadian model MC2; (b) the iterative process that leads to the two-time-level mirror version of the previously mentioned one has also been stabilised, and has been optimised to even higher stability; (c) the problem of the lower boundary condition in the semi-Lagrangian case has been solved with two possible methods. (ii) For the ALADIN variational tools the build of a solidly justified prototype of high resolution 3D-Var is achieved with emphasis on (d) structure functions computed with the so-called "lagged mode" (i.e. concentrating on the scales that were not analysed by the model providing the lateral boundary conditions) and (e) on the use of blending by digital filter initialisation (a fully novel method for providing a spin-up-free "first guess" at fine scale) to balance the high resolution data assimilation in a way that preserves most of the innovation coming from the observations. Still in this area, the work on specific features (f) for the humidity and land surface analysis has lead to a 2D-Var pioneering method with excellent results. (iii) For high resolution physics the prognostic treatment of convective characteristics (g) is achieved and emphasis has shifted on the one hand to the relaxation of other 'larger scale' constraints for convection and on the other hand to the other potential prognostic variables (turbulent kinetic energy and condensates) while (h) the unexpected link between stable boundary layer fluxes and cyclogenesis much downstream in the flux has been confirmed with an improved and smoother parameterisation of the turbulent fluxes in such cases. (iv) On a more case-to-case basis important progress was also achieved in the following areas: (i) snow evolution modelling and snow analysis, (j) understanding the respective roles of orography, time-stepping, non-hydrostatism and horizontal resolution in the control of numerical noise, (k) comprehension of the reasons why the previous attempt to build a radiative upper boundary condition failed, (l) role of the "regularised physics" in TL/AD processes at high resolution, (m) a new formulation of the drag and lift effects of the sub-grid scale orography, (n) a completely new way to look at the problem of information monitoring between coupling and coupled models, (o) an alternative to the constant coefficient lateral diffusion schemes in spectral models and (p) a new way to analyse sources of latent non-linear instability and stiffness in diabatic models.
(B) Teaching actions:
(i) practical training organized regularly for newcomers locally in each ALATNET centre.
(ii) ALATNET Seminar on High Resolution Modelling, Radostovice (CZ),15-26 May, 2000.
(iii) ALATNET Seminar on Data Assimilation, Gourdon (F), 11-22 June, 2001.
(iv) ALATNET Seminar on Numerical Methods, Kranjska Gora (Si), 27-31 May 2002.
(v) ALATNET Concluding seminar, Kiralyret (Hu), 15-17 October 2003.
(C) Fulfilled Young Researchers contracts:
(i) Post-Doc in Brussels: Martin GERA (Sk) and Ilian GOSPODINOV (Bg).
(ii) Pre-Doc in Toulouse: Gianpaolo BALSAMO (It, PhD already defended), Margarida BELO-PEREIRA (Pt), Andre SIMON (Sk), Cornel SOCI (Ro, PhD already defended) and Malgorzata SZCZECH (Po).
(iii) Pre-Doc in Budapest: Steluta ALEXANDRU (Ro).
(iv) Pre-Doc in Ljubljana: Raluca RADU (Ro) and Klaus STADLBACHER (Au).
(vi) Pre-Doc in Prague: Jozef VIVODA (Sk). Pos-Doc in Prague: Christopher SMITH (UK).

Web Site http://www.cnrm.meteo.fr/alatnet/
Fellowship Type Research Training Networks FP5
Last Update 29/04/2004
Partners
Partner Name Institution and Department Name Town Name Country
Prof. Alfred QUINET Institut Royal Météorologique BRUSSELS Belgium
Dr. Radmila BROZKOVA Cesky HydroMeteorologicky Ustav PRAHA Czech Republic
Dr. Andras HORANYI Hungarian Meteorological Service BUDAPEST Hungary
M. Jure JERMAN Ministry of Environment and Physical Planning, HydroMeteorological Institute of Republic of Slovenia LJUBLJANA Slovenia
Coordinator Jean-François GELEYN
CNRM/GMAP
Meteo-France
42 Avenue G. Coriolis
31057 TOULOUSE CEDEX 1
France
Phone: +33(0)5.61.07.84.50
FAX: +33(0)5.61.07.84.53
jean-francois.geleyn@meteo.fr

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