Ninth Workshop on Meteorological Operational Systems. Timeliness and Impact of Observations in the CMC Global NWP system

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Ninth Workshop on Meteorological Operational Systems ECMWF, Reading, United Kingdom 10 14 November 2003 Timeliness and Impact of Observations in the CMC Global NWP system Réal Sarrazin, Yulia Zaitseva and Gilles Verner Canadian Meteorological Centre Meteorological Service of Canada Environnement Canada Centre météorologique canadien Environment Canada Canadian Meteorological Centre

Outline CMC current global NWP suite and observations usage Impact of observation types from OSEs with the global forecasting system Impact of reception delays and short cut-off time constraints Outlook of the future CMC NWP system Final remarks

CMC Operational Models GEM model (global, regional, meso) 3D-Var assimilation on model surfaces (T108) Background errors from 24-48 method Observations QC with BG check and QC-VAR Global Model Uniform grid Resolution of.9º (~100 km) 28 eta levels Kuo convection scheme Sundqvist stratiform scheme Force-restore surface module with climatogical soil moisture 10 day forecasts at 00Z and 6 day forecasts at 12Z. Cut-off of T+3h00 Regional Model Variable resolution grid Resolution of.22º (~24 km) 28 eta levels Fritsch-Chappell scheme Sundqvist stratiform scheme ISBA surface module with soil moisture pseudo-analysis (error feedback, no data) 48-hour forecasts (00Z -12Z) Cut-off of T+1h40

Upper air soundings radiosonde pilot dropsonde Observations for 3D analyses land stations ships aircrafts temperature moisture winds pressure temperature moisture pressure winds Surface observations synoptic land stations ships fixed buoys drifting buoys Satellite NOAA ATOVS circumpolar radiance amsu-a & amsu-b GOES imager geostationary radiance Aircrafts ACARS / AMDAR AIREP AMVs geostationary (METEOSAT & GOES) derived winds aircrafts temperature winds

Operational Verification

Observing System Experiments Series of experiments with the exclusion of a type of observation in order to evaluate the importance of the impact of various observation systems in the NWP suite Two 6 weeks periods: Winter Period: 2001121800 to 2002012712 Summer Period: 2002061700 to 2002073112 6-day forecasts every 12 hours (00UTC and 12UTC) from final analyses

OSE Results Winter period, impact of the removal of TOVS vs Radiosondes of upper-air network Anomaly correlation Geopotential Heights 500 hpa

OSE Results Summer period, impact of the removal of TOVS vs Radiosondes of upper-air network Anomaly correlation Geopotential Heights 500 hpa

Reception time of BUFR aircrafts observations in CMC database Period 00 UTC, from 01 September 2003 to 15 September 2003 6-hour validity period Synoptic time T+1h30 T+3h00 T+6h00

Reception time of RAOBS observations in CMC database Period 12 UTC, from 01 September 2003 to 15 September 2003 6-hour validity period Synoptic time T+1h30 T+3h00 T+6h00

Reception time of AMSU-A ATOVS observations in CMC database Period 00 UTC, NOAA-15, from 01 September 2003 to 15 September 2003 6-hour validity period Synoptic time T+1h30 T+3h00 T+6h00

Reception time of AMSU-A ATOVS observations in CMC database Period 06 UTC, NOAA-15, from 01 September 2003 to 15 September 2003 6-hour validity period Synoptic time T+1h30 T+3h00 T+6h00

Reception time on AMSU-A ATOVS observations in CMC database Period 00 UTC, NOAA-16, from 01 September 2003 to 15 September 2003 6-hour validity period Synoptic time T+1h30 T+3h00 T+6h00

Reception time of AMSU-A ATOVS observations in CMC database Period 12 UTC, NOAA-17, from 01 September 2003 to 15 September 2003 6-hour validity period Synoptic time T+1h30 T+3h00 T+6h00

Example of NOAA Satellites AMSU-A ATOVS coverage after thinning, T+1h40 observation cut-off time, 24 September 2003, 12 UTC

Example of NOAA Satellites AMSU-A ATOVS coverage after thinning, T+3h00 observation cut-off time, 24 September 2003, 12 UTC

Example of NOAA Satellites AMSU-A ATOVS coverage after thinning, T+9h00 observation cut-off time, 24 September 2003, 12 UTC

Impact of cut-off time in a 3DVar assimilation cycles Experiments: 6-hourly assimilation cycles with various cut-off times and 6-day forecasts run every 12 hours (00 UTC and 12 UTC) during a 5-week verification period from 2003083100 to 2003100412 - G0: cut-off time: T+1h40 at 00 & 12 UTC et T+1h20 at 06 & 18 UTC. - G1: cut-off time: T+3h00 at 00 & 12 UTC et T+2h00 at 06 & 18 UTC. *G2: cut-off time: T+9h00 at 00 & 12 UTC and T+6h00 at 06 & 18 UTC. - G3: cut-off time: T+24h00 at 00, 06, 12 and 18 UTC. OPS: operational forecasts, FG from G2 with analysis at T+3h00

Impact of observational data cut-off time in the assimilation cycle Anomaly correlation Red line: operational cycle, T+9h00 Blue line: rapid update, T+3h00 Green line: early, T+1h40

Impact of observational data cut-off time in the assimilation cycle Anomaly correlation Red Line: T+24h00 cycle Blue line: operational cycle, T+9h00 Green line: operational forecasts from T+3h00 analyses

RMSE of Temperature 24-hour forecasts over the Southern Hemisphere Verification against analyses

RMSE of Wind Speed 24-hour forecasts over the Tropics Verification against analyses

Global System Now: - Uniform resolution of 100 km (400 X 200 X 28) - 3D-Var at T108 on model levels, 6-hr cycle, use of raw radiances from AMSUA, AMSUB and GOES 2004: - Resolution to 35 km (800 X 600 X 80) - Top at 0.1 hpa (instead of 10 hpa) with additional AMSUA and AMSUB channels - 4D-Var assimilation, 6-hr time window with 3 outer loops at full model resolution and inner loops at T108 (cpu equivalent of a 5-day forecast of full resolution model) - new datasets: profilers, MODIS winds, QuikScat 2005: - assimilation of AIRS, MSG, MTSAT - revised 4D-Var statistics 2006-07: - Additional datasets: IASI, GIFTS, COSMIC - very large increase in volume of assimilated data

Final Remarks Satellite observations and the upper air network have a large impact in the quality of CMC NWP products Among observing systems in the southern hemisphere, the use of satellite data provides the largest improvement to the forecast quality Operational NWP centers, such as the CMC, must maintain an assimilation cycle with relatively long observations cut-off time as the central part of their NWP suite in order to maximize the quality of their products Planning and investment in timely reception and processing of satellite data is essential to realise the full potential of satellite observing systems in operational NWP suites with short cut-off times