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Daily error (bias and st.dev.) in 24h 10mW [m/s] in Sep 2006 (EWGLAM stat.) 2.0 T15 oper ECH 1.0 M1U 4DV 1.5 [m/s] 1.0 0.5 0.0 02 09 16 23 30 day ÙÖ ½ ½¼Ñ ÛÒ × Ò ×Øº ÚØÓÒ Ò ËÔØº ¾¼¼ ÓÖ ÓÔÖØÓÒÐ Ì½¸ ÐÝ ÖÙÒ × ÓÒ ¹ÎÊ ´Å½Íµ Ò Ø ÅÏ ÐÓÐ ÑÓÐ ÚÖ¬ ÓÒ ÏÄÅ ×ØØÓÒ Ð×Ø 116 114 linear fit 200607 running 12mnth mean Normaliseret maalkrav 112 110 108 106 104 102 100 98 Jan 2002 Jan 2003 Jan 2004 Jan 2005 Jan 2006 Jan 2007 Jan 2008 Jan 2009 ÙÖ ¾ ÆÓÖÑÐ× ÓÖ×Ø ÒÜ ×Ò ¾¼¼¾ × Ù× ÓÔÖØÓÒÐÐÝ Ø ÅÁº
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NEWSLETTER of the 28 th EWGLAM and
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Newsletter of the 28th EWGLAM and 1
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6.2 P. Clark et al.: The Convective
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1.1 Foreword In 2006, MeteoSwiss ha
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Cornel Soci National Meteorological
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16:15 - 16:45 Filip Vana general Dy
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2 Consortia and ECMWF reports 12
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Research Progress at ECMWF 2005-200
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ocean data assimilation system for
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Physical Aspects 1) The introductio
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either with a 1-dimensional observa
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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
Page 65 and 66: Perspectives The integrated package
Page 67 and 68: 3.2 Croatia 65
Page 69 and 70: New computer Core of the new comput
Page 71 and 72: 3.3 Czech Republic 69
Page 73 and 74: ¾¿ Ø Ó ÂÒÙÖÝ ¾¼¼ ËÛØ
Page 75: ÏÄÅ ÊÔÓÖØ ¾¼¼ ÖÓÑ Ø
Page 79 and 80: LAM efforts at Estonian Meteorologi
Page 81 and 82: grid is 186x170 points in horizonta
Page 83 and 84: McDonald, A., and J. E. Haugen, 199
Page 85 and 86: Operational NWP Activities at the F
Page 87 and 88: Model Forecast model Limited area g
Page 89 and 90: 3.7 France 87
Page 91 and 92: Fig.1. The ALADIN-France domain, wi
Page 93 and 94: Towards AROME, A first try of a Rap
Page 95 and 96: 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
Page 105 and 106: 3.10 Ireland 103
Page 107 and 108: Filtering: Fourth order implicit ho
Page 109 and 110: The next chart shows wind arrows at
Page 111 and 112: Italian Meteorological Service Stat
Page 113 and 114: Fig.3 Integration domain for LM- EU
Page 115 and 116: 3.12 Netherlands 113
Page 117 and 118: esults with fixed entrainment and d
Page 119 and 120: simulation. In order to allow a goo
Page 121 and 122: layer for three contrasting nights
Page 123 and 124: 21 UTC). The severe thunderstorm fo
Page 125 and 126: 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
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NWP activities in INM Bartolomé Or
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1 System definition • Creation of
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MSLP June-August 2006 Geopotential
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NATIONAL STATUS REPORT on Operation
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Model input The observations used f
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Numerical Weather Prediction at Met
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The setup is based on a new numeric
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weight of importance in the voting
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4.1 F. Vana: Dynamics & Coupling, A
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Ô¸ ×ØÐ Ò ÒÓÒ¹ÐÒÖ «Ù
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ÙÖØÖ ÒÚ×ØØÓÒ ÔÖÓÚ Ø
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Ì ×Ô¬ ÓÒÐÙ×ÓÒ× ÓÖ Ø
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ÁÐÞ Ø×Ø× Ó ÄÁÆ¹ÆÀ Ý
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¯ ÒÐÐÝ Ø Ò×ØÐØÝ Ó ØÛ
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ÀÓÖÞÓÒØÐ Ñ× ×Þ Û× ¡
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ÔÓØÒØÐ ÓÛ ×¸ Ù×Ø Ø
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ÒÓÒ¹ÝÖÓ×ØØ ÝÖÓ×ØØ 1
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5 Scientific presentations on data
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COSMO: Overview and Strategy on Dat
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Meteorology in Hamburg (MPI-M). The
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temperature forecasts, this had a s
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5.2 D. Leuenberger et al.: The Late
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scaling factor α and of the latent
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a) b) RAD 1 2 3 4 5 6 7 8 9 10 det
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5.3 C. Fischer and A. Horanyi: Alad
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Figure 1: analysis increments of wi
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3) Averaged emissivities + dynamica
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In parallel, a direct radar observa
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►Algorithms: • FGAT (with Hunga
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Data assimilation activities in LAC
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Fig.3 RMSE difference (WDEF-NAM2).
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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
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The Murk aerosol is based on the ur
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Relaxation term Due to these proble
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Figure 12: SOx emissions in 1990 an
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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
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the Met Office Large Eddy Model (LE
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Figure 4 Domains used in high resol
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1.0 95th percentile threshold Fract
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Figure 10 Surface precipitation rat
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HIRLAM Physics developments Sander
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strong winds. This causes a too lar
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epresenting the weather in the case
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ËÒÓÛ¸ ÓÖ×Ø Ò Ð ×ÔØ×
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£ ½ ×Ò ¼ Þ ×Ò ×Ò · ¼
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¿º½ ÊØÓÒ Ò Ø ÓÖ×Ø Ï
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ÙÖ Ì¾Ñ ×¸ ÐØ ÒÛ ×ÙÖ
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×ÖÔØÓÒ Ó Ð ÑÓÐº Ìº
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ALARO-0 Physics developments at LAC
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eflectance for sample of 3-layer in
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2.1 Pseudo prognostic turbulent kin
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TKE and the integral buoyancy of th
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7 Scientific presentations on predi
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LAMEPS Development of ALADIN-LACE Y
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The more iterations performed, the
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uncertainty in the model physics, t
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In Budapest, dynamical downscaling
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7.2 J. García-Moya et al.: Recent
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Currently the size of the super ens
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Palmer, T.N., Alessandri, A., Ander
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Figure 4 Example of probability map
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More than 15 mm/6 hours Figure 6 Re
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7.3 C. Marsigli et al.: The COSMO S
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ÔÓ××Ð Ù×× Ó ÓÖ×Ø ÖÖ
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ÇËÅÇßËÊÈË × ½ßÑÑÖ
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¾℄ ÅÖ×Ð¸ º¸ ÅÓÒØÒ¸
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Overview COSMO ensemble systems Pie
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COSMO-LEPS 16-MEMBER EPS An objecti
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The used models are LAMI (Italy), a
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28th EWGLAM Meeting 9-11 October 20
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9 SRNWP business meeting report 293
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Minutes of the Meeting Participatio
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Training and Education Activities i
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These reports were very divers, fro
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Contacts with the Academia In his d
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