Title: RC LACE Status Report
1 RC LACE 2004
Regional Co-operation of A, CR, CZ, H,
SI, SK
Dijana Klaric
2RC LACE efforts2nd RC LACE MoU (2003-2005)
- Operations maintenance
- Networking
- Research development
3Operations maintenance
- all 6 members - individual operational
applications - SK
- almost the same domains
- mesh size (?x 12.2km - ?x 6.5 km)
- vertical resolutions (L37 - L45)
- envelope - no envelope orography
- dyn. adapt blending 3DVar (e-suite)
- maintenance and porting of SW
4Telecommunications
- RETIM2000 vs Internet
- Satellite dissemination
- DVB
- bandwidth eq. to 128 kBps link
- RETIM 40 budget
- as backup to Internet
5 Networking (Who? Why? When?)
- Decentralized research 3 WG
- work in AAA environment
- training for newcomers and WS
- ALADIN -Training on ALADIN-NH, TLS
- March 15-19, 2004
- SRNWP - 2nd WS on Verification, De Bilt
- June 14-15, 2004
- actions LACE WWW pages and FTP server
- coordinated verifications
- list of cases, MAP
6Verification project
- ALADIN Project organized by Slovenia
- started 2002
- aims
- to unify the verification on synoptic scale
- to impose the international standards
- to reduce duplication of work
- to compare different ALADIN at the same domain
- environment toward meso-scale verification
-
7Verification project
- Prototype
- station list
- 348 74
- ECMWF
- TM 430
8DB of Case Studies
9(No Transcript)
10MAP SOP cases
- ECMWF Re-analysis of MAP SOP
- different surface parameterization in ARPEGE
- Proper downscaling of
- ECMWF re-analysis
- work performed by LACE Data Manager
11Scientific Plan 2003/2004
- 2nd RC LACE Steering Committee meeting
- 2003
- Plans from year 2003 were fulfilled
- 98 person/months
- 2004
- to work on opened subjects
- to adjust RD to AAA plans
- to learn meso-NH physics ?
12Scientific Plantoward AAA compatibility
- Dynamics
- NH ALADIN is numerical core of AAA
- interfacing dynamics vs. physics is in focus
- Physics
- physics for different scales 10km, 5km, 2.5 km
- various schemas and SW
- up-scaling or downscaling approach
- Data Assimilation
- more non-classical observations
13Working Group for Dynamics and Coupling
- ?. Non-hydrostatic dynamics
- Interative schemes
- Choice of additional NH variables
- Bottom boundary condition
- Finalization of NH Dynamics
- Diabatism in NH
- ??. Dynamics other topics
- Horizontal diffusion (SLHD)
- Radiative UBC
- Physics/dynamics interface
-
14Results from WG for Dynamics and Coupling
- Dynamics/Physics interfaces
- treatment of physical tendencies in PC scheme
- mass conservation
- the mass of water removed from the atmosphere is
replaced by the dry air - ALADIN physics tendencies at origin point
- Investigation
- 1/2 at origin and 1/2 at arrival points
- stratiform prec. at arrival, rest at departure
point
15Results from WG for Dynamics and Coupling
16Working Group for Physics
- ?. Shallow convection / PBL cloudiness
- Convergence Xu-Randall and Seidl-Kann scheme
- Experiments on inversion formation and
sustenance - ??. CAPE deep convection triggering
- ???. Orographic drag/envelope
- Validation on precipitation and wind (?x10
km - 2.5 km) - ?V. Numeric of parameterization schemas
- V. Prognostic cloud water
17Results from WG for Physics
- The role of surface evaporation in the triggering
of mountain convection in ALADIN - gt Mountains with their differential evaporation
and solar heating regimes create mesoscale
baroclinic circulations and may establish an
environment locally favourable for deep
convection - Weather situation a series of days with deep
convection triggered locally by orographic
effects in the absence of large-scale forcing - Drau valley in Carinthia, Austrias southernmost
province - 24-hour model run with evaporation set equal to
zero (dx4km)
18Results from WG for Physics
- Conclusions
- Near-surface humidity convergence over the
mountain chains reduces by around 30 to the
north (dry) side of the boundary, but by only
10 20 to the south (humid) side - Convective precipitation decreases significantly
remaining convection concentrates on the
mountains along and to the south (humid) side
of the air mass boundary, where it can still
obtain enough moisture
19red numbers first precipitation at .. UTC
REF
EXP
202m specific humidity (09 UTC)
REF
EXP
212m humidity divergence (12 UTC)
Green numbers relative decrease of humidity
convergence compared to REF
REF
EXP
22Working Group for Data Assimilation
- ?. Methods - Algorithmic aspects
- Isotropy properties of the B matrix
- Multivariate humidity formulation in the B
matrix - Lonnberg -Hollingsworth versus NMC variances
- ??. Methods - Cycling
- ???. Observations
- ATOVS and MSG
- AMDAR
- 10 wind
- Wind profilers data
23Working Group for Data Assimilation (cont.)
- ???. Observations (cont.)
- Radar data
- ?V. Surface
- Snow analysis experiments
- V. Latent Heat Nudging
- VI. LAMEPS
- Optimization of ARPEGE singular vector
computations for CE - ALADIN EPS using PEACE perturbations
24Results from WG for Data Assimilation
- Assimilation of ATOVS data
- improvements of treatment of AMSU-A, AMSU-B
- Choice for radiance-bias correction for LAM
- bias corr. coefficients scan-angle biases and
- coefficients for air-mass predictors
- LAM- satellite paths are cut ? problems for
scan-angle biases - Harris and Kelly reduction of bias
- actions to enlarge domain for 3DVar
- to re-compute bias corr. Coefficients for
LAM
25Results from WG for Data Assimilation
26Results from WG for Data Assimilation
- Snow analysis with CANARI
- significant T2 overestimation in strong winter
inversion - diagnostics
- RH2 is too dry, short wave radiation is too big
- too strong 10m wind and wind gust
- NO SNOW analysis
- cure 3DVAR CANARI snow analysis modified
physics
27Results from WG for Data Assimilation
4-6. deg. err.
4-6 deg. err.
28Results from WG for Data Assimilation
- LACE Data Assimilation mini Workshop
- (Budapest, 20-22 October, 2003)
29Future Actions
- ? WS on dynamics-physics interfacing
- November 2004, Prague
- ? training in NH ALADIN
- Early winter 2005, Prague
- ? WS on maintenance
- Autumn 2005, Budapest
30Austria Croatia Czech
Republic Hungary
Slovenia Slovakia