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Cornel Soci National Meteorological Administration Romania Philippe Steiner MeteoSwiss Switzerland Jürgen Steppeler Deutscher Wetterdienst Germany Sander Tijm KNMI Netherlands Martina Tudor Meteorological & Hydrological Service Croatia Per Unden SMHI Sweden Filip Vana Czech Hydrometeorological Institute Czech Republic Josette Vanderborght Institut Royal Météorologique Belgique André Walser MeteoSwiss Switzerland Xiaohua Yang Danish Meteorological Institute Denmark 8
1.3 Programme Monday, 9th October 2006 8:15 – 8:45 Registration 9:00 Opening by the Director of MeteoSwiss, D. Keuerleber and organisational matters 09:15 – 11:30 Presentation of the Consortia and ECMWF chair: Marco Arpagaus 09:15 – 09:30 Tiziana Paccagnella COSMO 09:30 – 09:45 Mike Bush UK Met Office 09:45 – 10:00 Jeanette Onvlee HIRLAM 10:00 – 10:15 Jean-François Geleyn ALADIN 10:15 – 10:30 Dijana Klaric LACE 10:30 – 11:00 Coffee break 11:00 – 11:30 Mariano Hortal ECMWF 11:30 – 14:45 Presentations of national posters chair: Per Unden Harald Seidl Austria Josette Vanderborght Belgium Stjepan Ivatek-Sahdan Croatia Filip Vana Czech Republic Bent Sass Denmark Aarne Männik Estonia Carl Fortelius Finland Claude Fischer France Jan-Peter Schulz Germany Andras Horanyi Hungary 12:30 – 13:45 Lunch break James Hamilton Massimo Bonavita Gerard Cats Maria José Monteiro Cornel Soci Maria Derkova Neva Pristov Bartolome Orfila Lars Meuller Philippe Steiner Mike Bush 14:45 – 15.15 Poster session Ireland Italy Netherlands Portugal Romania Slovakia Slovenia Spain Sweden Switzerland United Kingdom 15:15 – 15:45 Coffee break 15:45 – 17:45 Scientific presentations on numerics and coupling numerics/physics Chair: Claude Fischer 15:45 – 16:15 Terry Davies Lateral boundary conditions, variable resolution or both? 9
Page 1: NEWSLETTER of the 28 th EWGLAM and
Page 4 and 5: Newsletter of the 28th EWGLAM and 1
Page 6 and 7: 6.2 P. Clark et al.: The Convective
Page 8 and 9: 1.1 Foreword In 2006, MeteoSwiss ha
Page 12 and 13: 16:15 - 16:45 Filip Vana general Dy
Page 14 and 15: 2 Consortia and ECMWF reports 12
Page 16 and 17: Research Progress at ECMWF 2005-200
Page 18 and 19: ocean data assimilation system for
Page 20 and 21: Physical Aspects 1) The introductio
Page 22 and 23: either with a 1-dimensional observa
Page 24 and 25: 2.2 ALADIN 22
Page 26 and 27: Another important event happened, i
Page 28 and 29: • However inspection of T2m forec
Page 31 and 32: Figure 4: One case of intercomparis
Page 33 and 34: The COSMO Consortium in 2005-2006 T
Page 35 and 36: 2. Model system overview The key fe
Page 37 and 38: Data Assimilation for LM Method: Nu
Page 39 and 40: 2. LM performance known, critically
Page 41 and 42: expected to result in an improved r
Page 43 and 44: Schrodin, R. and H. Heise, 2002: Th
Page 45 and 46: HIRLAM-A activities in 2006 Jeanett
Page 47 and 48: addition, research on the construct
Page 49 and 50: HIRLAM Reference System development
Page 51 and 52: Fig. 2: Case study for 10 June 2006
Page 53 and 54: Unified Model Developments 2006 Met
Page 55 and 56: Figure 4: Noise in increments from
Page 57 and 58: Cycle Date Model change and impact
Page 59 and 60: 1.5km On-demand model Figure 8: 1.5
Page 61 and 62:
3.1 Belgium 59
Page 63 and 64:
• A prognostic mass-flux scheme f
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Perspectives The integrated package
Page 67 and 68:
3.2 Croatia 65
Page 69 and 70:
New computer Core of the new comput
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3.3 Czech Republic 69
Page 73 and 74:
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LAM efforts at Estonian Meteorologi
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grid is 186x170 points in horizonta
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McDonald, A., and J. E. Haugen, 199
Page 85 and 86:
Operational NWP Activities at the F
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Model Forecast model Limited area g
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3.7 France 87
Page 91 and 92:
Fig.1. The ALADIN-France domain, wi
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Towards AROME, A first try of a Rap
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Status Report of the Deutscher Wett
Page 97 and 98:
In August 2006 production with the
Page 99 and 100:
3.9 Hungary 97
Page 101 and 102:
• LBC coupling at every 3 hours O
Page 103 and 104:
IFS as driving model for ALADIN. Th
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3.10 Ireland 103
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Filtering: Fourth order implicit ho
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The next chart shows wind arrows at
Page 111 and 112:
Italian Meteorological Service Stat
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Fig.3 Integration domain for LM- EU
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3.12 Netherlands 113
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esults with fixed entrainment and d
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simulation. In order to allow a goo
Page 121 and 122:
layer for three contrasting nights
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21 UTC). The severe thunderstorm fo
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Limited Area Modelling Activities a
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(a) Figure 2 ALADIN/Portugal geogra
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een locally implemented as an optim
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LAM ACTIVITIES IN ROMANIA Cornel SO
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Fig.3 HRM domain, 78 cumulated prec
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- Experiments : variation of the fr
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NWP activities at Slovak Hydrometeo
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Operational suite upgrades • 23/0
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3.16 Slovenia 139
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First experiments with new physical
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• resolution of meteorological fi
Page 147 and 148:
NWP activities in INM Bartolomé Or
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1 System definition • Creation of
Page 151 and 152:
MSLP June-August 2006 Geopotential
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NATIONAL STATUS REPORT on Operation
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Model input The observations used f
Page 157 and 158:
Numerical Weather Prediction at Met
Page 159 and 160:
The setup is based on a new numeric
Page 161 and 162:
weight of importance in the voting
Page 163 and 164:
4.1 F. Vana: Dynamics & Coupling, A
Page 165 and 166:
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Page 181 and 182:
5 Scientific presentations on data
Page 183 and 184:
COSMO: Overview and Strategy on Dat
Page 185 and 186:
Meteorology in Hamburg (MPI-M). The
Page 187 and 188:
temperature forecasts, this had a s
Page 189 and 190:
5.2 D. Leuenberger et al.: The Late
Page 191 and 192:
scaling factor α and of the latent
Page 193 and 194:
a) b) RAD 1 2 3 4 5 6 7 8 9 10 det
Page 195 and 196:
5.3 C. Fischer and A. Horanyi: Alad
Page 197 and 198:
Figure 1: analysis increments of wi
Page 199 and 200:
3) Averaged emissivities + dynamica
Page 201 and 202:
In parallel, a direct radar observa
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►Algorithms: • FGAT (with Hunga
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Data assimilation activities in LAC
Page 207 and 208:
Fig.3 RMSE difference (WDEF-NAM2).
Page 209 and 210:
6 Scientific presentations on physi
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Physics improvements in the NAE mod
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The top panel in figure 3 shows tha
Page 215 and 216:
The Murk aerosol is based on the ur
Page 217 and 218:
Relaxation term Due to these proble
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Figure 12: SOx emissions in 1990 an
Page 221 and 222:
Buncefield oil depot fire Figure 15
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6.2 P. Clark et al.: The Convective
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y the model (e.g. streaks of gradua
Page 227 and 228:
the Met Office Large Eddy Model (LE
Page 229 and 230:
Figure 4 Domains used in high resol
Page 231 and 232:
1.0 95th percentile threshold Fract
Page 233 and 234:
Figure 10 Surface precipitation rat
Page 235 and 236:
HIRLAM Physics developments Sander
Page 237 and 238:
strong winds. This causes a too lar
Page 239 and 240:
epresenting the weather in the case
Page 241 and 242:
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£ ½ ×Ò ¼ Þ ×Ò ×Ò · ¼
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ALARO-0 Physics developments at LAC
Page 253 and 254:
eflectance for sample of 3-layer in
Page 255 and 256:
2.1 Pseudo prognostic turbulent kin
Page 257 and 258:
TKE and the integral buoyancy of th
Page 259 and 260:
7 Scientific presentations on predi
Page 261 and 262:
LAMEPS Development of ALADIN-LACE Y
Page 263 and 264:
The more iterations performed, the
Page 265 and 266:
uncertainty in the model physics, t
Page 267 and 268:
In Budapest, dynamical downscaling
Page 269 and 270:
7.2 J. García-Moya et al.: Recent
Page 271 and 272:
Currently the size of the super ens
Page 273 and 274:
Palmer, T.N., Alessandri, A., Ander
Page 275 and 276:
Figure 4 Example of probability map
Page 277 and 278:
More than 15 mm/6 hours Figure 6 Re
Page 279 and 280:
7.3 C. Marsigli et al.: The COSMO S
Page 281 and 282:
ÔÓ××Ð Ù×× Ó ÓÖ×Ø ÖÖ
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Page 287 and 288:
Overview COSMO ensemble systems Pie
Page 289 and 290:
COSMO-LEPS 16-MEMBER EPS An objecti
Page 291 and 292:
The used models are LAMI (Italy), a
Page 293 and 294:
28th EWGLAM Meeting 9-11 October 20
Page 295 and 296:
9 SRNWP business meeting report 293
Page 297 and 298:
Minutes of the Meeting Participatio
Page 299 and 300:
Training and Education Activities i
Page 301 and 302:
These reports were very divers, fro
Page 303:
Contacts with the Academia In his d
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