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Figure 4: One case of intercomparison of various data assimilation procedures. (a) 00-03h range; (b) 03-06h range; (c) 06-09h range. Towards “HARMONIE” The progressive merging of HIRLAM and ALADIN activities is for the ALADIN consortium both the main challenge and the most promising long-term perspective. Things are progressing at a reasonable speed (neither too quickly, nor too slowly), even if not always as homogeneously as one would ideally wish. But such an endeavour was lacking identity without a name, be it only to be used selectively and progressively. Peter Lynch removed this lack via the following proposal: HIRLAM ALADIN Research (towards) Meso-scale Operational NWP In Euromed There cannot be any more fitting conclusion for this brief introduction to the other ALADIN contributions to this Newsletter. 29
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 10 and 11: Cornel Soci National Meteorological
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 32 and 33: 2.3 COSMO 30
Page 34 and 35: The COSMO's organization consists o
Page 36 and 37: − a scheme including graupel cont
Page 38 and 39: DWD Germany: LM-E 7 km BCs from GME
Page 40 and 41: 4. Further development of the Runge
Page 42 and 43: interpretation and adaptation issue
Page 44 and 45: 2.4 HIRLAM 42
Page 46 and 47: smallest institutes contribute a so
Page 48 and 49: is ongoing. Studies on the impact o
Page 50 and 51: Fig. 1: Examples of verification sc
Page 52 and 53: 2.5 UKMO 50
Page 54 and 55: Figure 2: Global model Cycle G38 -
Page 56 and 57: NAE Model developments Cycle Date M
Page 58 and 59: Figure 7: Impact of domain extensio
Page 60 and 61: 3 National status reports 58
Page 62 and 63: LIMITED AREA MODELLING ACTIVITIES A
Page 64 and 65: and Staufer, 2006): the areas of in
Page 66 and 67: Concentrating on the 2m temperature
Page 68 and 69: National status report for Croatian
Page 70 and 71: DART cruise (Dynamics of the Adriat
Page 72 and 73: ËØØÙ× ÖÔÓÖØ Ó Ø Þ ÀÝ
Page 74 and 75: 3.4 Denmark 72
Page 76 and 77: Daily error (bias and st.dev.) in 2
Page 78 and 79: 3.5 Estonia 76
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To evaluate baric (includes nonhydr
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of NWP environment at EMHI to ECMWF
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3.6 Finland 82
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main features of the RCR suite are
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Figure 2. Integration domain and in
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Status of operational and research
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■ ■ autoconversion in the micro
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3.8 Germany 92
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The limited area Lokal-Modell (LM)
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egional NMS have to use 12h “old
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LIMITED AREA MODELLING ACTIVITIES A
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different ALADIN model versions (op
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The recent version of the system is
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Introduction NWP at Met Éireann -
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Nested Hourly Analysis A separate n
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3.11 Italy 108
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● experimental run of a parallel
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Fig. 5 Model orography over Italy f
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A simple parameterization for detra
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Single-column modeling versus mesos
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Results are presented which are val
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Probabilistic 0-12 h forecasts of (
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3.13 Portugal 122
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⇒ Improvement of verification too
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(a) Figure 4 Portuguese NWP archive
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3.14 Romania 128
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- additional post processing: stabi
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• Operational verification versus
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3.15 Slovakia 134
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HPC ARCHIVE IBM @server pSeries 690
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Figure 4: 6h forecast of 1h cumulat
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Limited Area Modelling Activities i
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duration of intensity above thresho
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3.17 Spain 144
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presents the block diagramme of the
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ONR integration area HNR - CNN inte
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3.18 Sweden 150
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• Kain-Fritsch convection • Ras
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3.19 Switzerland 154
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1000 wind profiles. Assimilation of
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many stations (Fig. 2b). In the sin
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4 Scientific presentations on numer
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ÝÒÑ× ² ÓÙÔÐÒ ÄÁÆ Ò Ä
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ÙÖ ½ ¾ ÒÓÒ¹ÐÒÖ ÓÛ Ü
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ÊÚ×Ø ÒØÖ ÓÖ ÔÝ××¹ÝÒ
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4.2 J. Masek: Idealized tests of AL
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¢ £ ÑÓ¬ Ý ÒØÖÓÙØÓÒ Ó
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ÄØÖÐ ÓÙÒÖÝ ØÖØÑÒØ Ù
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0.40 8 16 24 32 40 48 56 64 0.40 0.
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Ù× Ó Ñ××Ò ÒÐÝØÐ ×ÓÐ
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ÓÒÐÙ×ÓÒ× ÈÖ×ÒØ ÐÞ ¾
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5.1 C. Schraff: COSMO: Overview and
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model. They prevent the uncontrolle
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efficiently and does not have sever
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Furthermore, work on assimilating s
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The Latent Heat Nudging Scheme of C
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is partly due to the double penalty
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Leuenberger D.,2005: High-resolutio
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Aladin consortium activities in dat
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suggests however to filter the smal
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Figure 5: 2m temperature biases for
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Figure 7: 3 hour aggregated precipi
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5.4 G. Bölöni: Data assimilation
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3D-FGAT Tests with the 3D-FGAT meth
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Fig.5 Temperature RMSE (thick line)
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6.1 M. Bush: Physics improvements i
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Figure 2: Smoothing of Mass Flux Pr
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Solution to the ‘Valley cooling p
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Figure 7: log10 vis as a function o
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The distribution of the source term
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Dust forecasting The aim of the Dus
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Tropospheric chemistry in the Unifi
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The Convective-Scale UM: Current St
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generally very similar from case to
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the convective dynamics leading to
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Case A radar 0 100 km compare 10 km
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(a) Figure 8 Results from idealised
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6.3 S. Tijm: HIRLAM Physics develop
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with the new surface scheme. The sa
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Mesoscale physics In the HIRLAM-Ala
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6.4 S. Gollvik: Snow, forest and la
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ÑÓÖ ÔÝ×Ð ×Ñ¸ ÛÖ Ø ×Ò
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Ï Ð×Ó Ú ÒÓÔÝ ÛØÖ × Ú
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ËÓÑ ÀÁÊÄÅ ÚÖØÓÒ× ÀÖ
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ÙÖ ÓÑÔÖ×ÓÒ× ØÛÒ Ø Ò
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6.5 N. Pristov et at.: ALARO-0 Phys
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aerosols was neglected, i.e. cloud
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Figure 3: Vertical profiles of sola
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2.2 Mixing length parameterisation
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G.-J. Steeneveld, G. Svensson, P. T
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7.1 Y. Wang: LAMEPS Development of
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spread of 500hPa geopotential and 8
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case study. The method of the initi
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ECMWF EPS forecast were not spoiled
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. Blending method seems to be promi
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Recent Experiences with the INM Mul
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4. Conclusions Since the year 2001
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Figure 3 Example of a stamp chart o
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Figure 5 Example of one determinist
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Figure 8 Stamp map of reliability a
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Ì ÇËÅÇ¹ËÊÈË ÔÖÓØ º
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ÙÖ ½ ÁÆÅ ËÊÈË ÓÑÒº ´
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ÒØÖÐ ÔÖØ Ó Ø ÐÔ× ´ÒÓ
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7.4 P. Eckert: COSMO ensemble syste
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Verification of COSMO LEPS The COSM
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Ch. Frei, MeteoSwiss The verifying
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8 EWGLAM final discussion 290
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Next SRNWP Meetings At the invitati
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13th SRNWP Meeting 12 October 2006,
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Under the general term "interoperab
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Redaction Committee for Interoperab
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- statistical and physical adaptati
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