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The High-Resolution Numerical Weather Prediction Systems for the 2010 Vancouver Olympics. S. B élair, J.Mailhot Meteorological Research Division, Environment Canada. WWRP VRWG and MWFRWG joint meeting, Berlin, Germany, 10 Sept. 2011. 3. 2. 1. - PowerPoint PPT Presentation
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S. Bélair, J.Mailhot
Meteorological Research Division, Environment Canada
The High-Resolution Numerical Weather The High-Resolution Numerical Weather Prediction Systems for the Prediction Systems for the 2010 Vancouver Olympics2010 Vancouver Olympics
WWRP VRWG and MWFRWG joint meeting, Berlin, Germany, 10 Sept. 2011
VANCOUVER-2010: EC’s EXPERIMENTAL MESOSCALE SYSTEMS
(Thanks to Juan Sebastian Fontecilla)
15-kmGEM-LAM
2.5-kmGEM-LAM
IC + LBC 1-kmGEM-LAM
33-kmGEM-LAM
IC + LBC
REGIONAL EPS
HIGH-RESOLUTION DETERMINISTICATMOSPHERIC SYSTEM
2D-external landsurface System(100 m)
Single-Point
EXTERNAL LAND SURFACE SYSTEM
Adaptor
1 2
3
33-kmGEM-LAM
33-kmGEM-LAM
33-kmGEM-LAM
20 members
Mailhot et al., 2010: BAMS., 91, 1073-1085.
GEM-LAM integrations, twice daily, starting from 0000 and 1200 UTC GEM-Regional forecasts:
LAM-15 km → 2.5 km → 1 km
1 km
2.5 km
WhistlerWhistler
VancouverVancouver
15 km
Comes with:
Improved dynamics
Improved physics
New diagnostic outputs
NESTING STRATEGY FOR LAM-V10 MESOSCALE NWP SYSTEM
CUSTOMIZED OUTPUT PACKAGE
TemperatureTemperature
Dewpoint, RHDewpoint, RH
Surface windsSurface winds
Cloud cover:Cloud cover:Low, mid, highLow, mid, highLow level windsLow level winds
Wind gustsWind gusts
WindchillWindchillCloud baseCloud base
QPF: QPF: /1h, /3h,/1h, /3h, /6h, /6h, cumulativecumulative
QPF QPF by type:by type:cumul. , instant.cumul. , instant.
2-D maps2-D maps(1 km)(1 km)
Visibility: Visibility: fog, rain, snow, fog, rain, snow, resultantresultant
CUSTOMIZED OUTPUT PACKAGE
MeteogramsMeteograms(1 km)(1 km)
General WxGeneral Wx
T, TT, Tdd etc. etc.Wind and GustsWind and Gusts
PrecipitationPrecipitationPCP RatesPCP Rates
Clouds and visibilityClouds and visibility
SnowSnow
EC’s EXTERNAL LAND SURFACE MODELING for VO2010
(Thanks to Juan Sebastian Fontecilla)
100-m snow analyses
Great decrease of T2m errors (bias shown here)
Bernier et al., 2011, J. Hydromet., 12, 508-530.
OBJECTIVE EVALUATION...
Surface variables: snow depth, snow density, snow albedo, surface temperature, soil moisture (if applicable).
Traditional near-surface variables: temperature, humidity, winds (speed and direction)
New near-surface variables: wind gusts, visibility (fog, rain, snow, total)
Clouds and precipitation: Cloud base height, cloud coverage (low, mid, and high levels), QPF (total and by type, instantaneous and cumulative), density of falling snow
Visibility, Whistler, 13 March 2010
Snow density (falling), 23 Feb. 2010