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Sub-km External Surface Modeling to Improve Numerical Prediction over Ecosystems, Cities, and Water Surfaces S. Bélair, M. Abrahamowicz, S. Leroyer, N. Bernier, N. Gauthier, V. Souvanlasy, A. Leroux, and J.-P. Gauthier Meteorological Research Division Environment Canada CMOS/AMS 2012 Congress, Montreal, June 1rst, 2012 ENVIRONMENT CANADA’s EXTERNAL SURFACE MODELING SYSTEM ATMOS MODEL LOW-RES MODEL or OBS or ANALYSES ATMOSPHERIC FORCING at FIRST ATMOS. MODEL LEVEL (T, q, U, V) ATMOSPHERIC FORCING at SURFACE (RADIATION and PRECIPITATION) External Surface Models With horizontal resolution as high as that of surface databases (e.g., 100 m) HIGH-RES 2D INTEGRATION Computational cost of off-line surface modeling system is much less than an integration of the atmospheric model HIGH-RESOLUTION MODELING of the URBAN ENVIRONMENT (120m) Nocturnal 2m air temperature (simulation, 120m) § 6 July, 01:00 LST Montreal Island °C 22 21 20 19 18 17 16 15 14 ► UHI : 5-6 °C (Leroyer et al. 2011) HIGH-RESOLUTION MODELING OVER MOUNTAINS (VO2010) 100-m snow analyses Great decrease of T2m errors (bias shown here) (Bernier et al. 2011, 2012) (Thanks to Juan Sebastian Fontecilla) LAND SURFACE PARAMTERS A VERY IMPORTANT ELEMENT of SUCCESS… MODIS ALBEDO CLIM. MODIS NDVI CLIM. BIOME-BGC CLIM. ALL DATABASES GTOPO30 SRTM-DEM ASTER-DEM CDED1 GLCC CCRS GlobCover LCC-2000 CanVec Census FAO STATSGO SMAP SM HWSDB GenPhysX / UrbanX Vegetation fractions Urban parameters Water fraction Soil texture Pre-Surf Orographic parameters Water fraction GEM or GEM-Surf LEAF AREA INDEX VEG. FRACTIONS VEG. PARAMETERS ALBEDOs ROOT-ZONE DEPTH SAND CLAY URBAN PARAMETERS Building Fraction (%) 60+ Q 50 40 Vegetation (Various Types) 35 30 25 20 10 Pavement Streets è 100m Urban Fields over Toronto Google Maps DOWNSCALING LAI: SOURCES of INFORMATION 30m 200m LCC-2000 Land Use / Land Cover (types) 1km 10km TARGET RESOLUTION MODIS 10-year NDVI climatology Grass Forests (Belair et al., in preparation) Biome-BGC 10-year Clim from runs (LAI) LAI OVER SOUTHERN ONTARIO and SOUTHERN QUEBEC PRELIMINARY TESTSTOWARDS an IMPLEMENTATION over CANADA: HIGH-RESOLUTION NUMERICAL PREDICTION of LAND SURFACE TEMPERATURES QUALITATIVE EVALUATION AGAINST MODIS SURFACE TEMPS Spatial variability of land surface temperature depends on … Vegetation Albedo Emissivity Soil texture Soil moisture Radiative forcing PLANS for OPERATIONAL IMPLEMENTATION at MSC (2013) è120 hr forecast run (every 6hr) t=0 Best estimates of Hourly Forcing SW, LW – REG-15 km, 6-12 hr. – at surface UU,VV – REG-15km, 0-6 hr. – at screen lev. (10m) P0 – REG-15km, 0-6 hr. – at surface Hourly Forcing at 1st atmospheric level From Reg-15km and Global-33km forecasts (TT, HU, SW, LW,UU,VV,P0,PR ) Forcing is downscaled and adapted to Gem-Surf Resolution PR –Canadian Precipitation Analysis (CaPA) – at surface TT, HU – Optimal Interpolation (OI) – at screen lev. (2m) Analysis Analysis t-6h 6h. Gem-Surf Run Pre-Processor of Geophysical Fields èCoherence & Consistency tests for GenPhysx and UrbanX variables è Calculation of time-dependent variables (e.g,LAI,α) t=0 120h. Gem-Surf Forecast Provides best estimates of : • Soil Moisture • Surface Temp. Pre-Processor • Snow charac. (density, depth,albedo) • Urban charac. (roof, wall, road temp. etc.) è Continuous (Analysis) Cycle Hourly Forcing Analysis t-12h t-6h Pre-Processor 06 Z Forecast t=0 Pre-Processor t+6h Pre-Processor 12 Z Forecast 18 Z Forecast 120hr 120hr t+12h Pre-Processor 00 Z Forecast 120hr t-6h Pre-Processor 06 Z Forecast 120hr Pre-Processor 12 Z Forecast 120hr 18 Z Foreca