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Environment Canada Canadian Meteorological Centre Environnement Canada Centre météorologique canadien Meteorological Service of Canada Status Report Montréal, Canada, May 26-28, 2004 Gilles Verner Chief, Data Assimilation and Quality Control Canadian Meteorological Centre 17 th NOAM-Europe Data Exchange Meeting

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Environment CanadaCanadian Meteorological Centre

Environnement CanadaCentre météorologique canadien

Meteorological Service of Canada Status Report

Montréal, Canada, May 26-28, 2004

Gilles VernerChief, Data Assimilation and Quality Control

Canadian Meteorological Centre

17th NOAM-Europe Data Exchange Meeting

Environment CanadaCanadian Meteorological Centre

Environnement CanadaCentre météorologique canadien

Outline

• Current status:– Canadian Forecast System

– Telecoms and Computers

– NWP System at CMC

– MSC Observing Networks and Canadian AMDAR

• Changes to NWP System since last meeting– Results from AMSU-B / GOES radiances

– Results from 15-km regional GEM

– Results from new OSE’s

• Future Plans and Requirements for Data

• Part II presented by Godelieve Deblonde

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MSC Forecast Offices and Satellite Reception Facilities

Each MSC Officehas a GOES Direct Readout Station.

CMC has 3 GOESReadout Stations.

MSC operates 3 HRPTStations: Halifax, Gander and Edmonton.Data from a non-MSCNorthern station is alsoavailable (Resolute).CMC has DOMSAT system for AVHRR-GAC (TeraScan)

Environment CanadaCanadian Meteorological Centre

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MSC Forecast Offices and Satellite Reception Facilities

Each MSC Officehas a GOES Direct Readout Station.

CMC has 3 GOESReadout Stations.

MSC operates 3 HRPTStations: Halifax, Gander and Edmonton.Data from a non-MSCNorthern station is alsoavailable (Resolute).CMC has DOMSAT system for AVHRR-GAC (TeraScan)

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CMC Computer Center ConfigurationCMC Computer Centre Configuration

2004/03

6x ea

Supercomputing Cluster

SGIO3000's40 PEs

(MIPS R12K)

O2000 4 xR10K PEs

1.2 TB14x SCSIfrom OSS

Climate Archive

HPModel 30 &

60 RAID0.2 TB?

3x

1000 Mb/s switched128ports. Each host has links to

ops & dev net

SGIO300:8 PEs

Central File Server145 TB

4 DST drives20 MB/s ea.

LSI (1 TB 4X FC)

10x FCdual

attach

LSI11TB

Front Ends

FC Hubs 32 ports

Data Acquisition& Distribution

opsnet switched(1000+100+10)

CriticalWorkstations

devnet switched(1000+100+10)

Dev HPpairs

NationalProduct

DistributionServerMC/SG

2 x HP K370

SmallerHP pairs

PC's & WksNT/OTServers

2 x o200Monitoring

Servers

routers

8 x Front-End3 x Back-End

2 Data4 Climate

2 x Greenlane

DMZ nets (10)

router

AWWS2xHP

L-series

InternetServers

100 UNIX &150 MSdesktops

3x o200WrkGrpServers

Satnet Tx

PC's, Wks.&

Tandem

F820.05 TB

NASO3000 18 xR14K PEs

ASEPLinuxCluster

17 DL380

IBM SP -928 PE &2.19TB

LSI (8.67 TB FC)

8x

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Telecommunications

• GTS link CMC - NWS: upgraded from 64 kbps to T1 during 2003

• Upgrade was done for exchange of NWP model output (for EPS) and Canadian Radar data

• Former NAIL link between Ice Centres (CIS - NIC) removed

• Link UKMO-CMC still active (Meteosat - GMS - GOES)

• Eumetsat - CMC link for EARS

• Internal MSC links upgraded (radar, hrpt, NWP)

• Internet still used for access to Nesdis data; CMC internet access upgraded during 2003 (100 mbps and 2 independent ISP)

• Funding for high speed link (T1+) with Nesdis approved

OPERATIONAL RUNS: MAIN COMPONENTS

GEM modelGlobal (100km) : 0-10/15 days Regional (15km) : 0-48 hoursHIMAP (10km) : 0-24 hours

air quality (CHRONOS)

Environmental EmergencyTransport model (CANERM)

Trajectory model

monthly and seasonalforecasts

global assimilation cycle

3D Var Analysis (data collection and

assimilation)

Models,6-hour forecast

(trial field)

Wave model (WAM)

regional data assimilation

ensemble forecasts(16 members)

surface analysis

CMC Operational Models

Global Model Regional 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

• Variable resolution grid• Resolution of .1375º (~15 km) • 58 eta levels• Kain-Fritsch 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+1h35

• 3D-Var assimilation on model η levels (T108)• Background errors from 24-48 method• Observations QC with BG check and QC-VAR• GEM model (global, regional, meso)

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575 X 641 grid (66% in 15-km uniformarea)

Regionalmodel

CMC Operational Models (cont.)

Mesoscale model Global ensemble

• GEM variable grid (HiMAP)• Resolution of .09º (~10 km) L35• Kain-Fritsch convection scheme• Sundqvist condensation scheme• ISBA surface module• No assimilation cycle (started from 6hr regional)• 30 hour forecasts at 06/18Z

• Perturbed analyses from perturbed assimilation cycles• Resolution of ~150 km (1.2º for GEM and T149 for SEF)• 16 members• Multi model approach with different physics options• 10 day forecasts at 00Z

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Observations for 3D-Var analysesTYPE

FORMAT / INSTRUMENT

PLATFORM VARIABLES

Upper-air soundings

• radiosonde

• pilot

• dropsonde

(profiler)

• land stations

• ships

• aircraft (dropsonde)

• temperature

• moisture

• winds

• sfc pressure

Surface observations • synoptic

• land stations

• ships

• fixed buoys

• drifting buoys

• temperature

• moisture

• sfc pressure

• winds (marine)

Satellite • NOAA ATOVS

amsu-a & amsu-b

• circumpolar (NOAA series)

(Aqua, amsu-a) • radiance

• GOES imager• geostationary (GOES-W)

(GOES-E)• radiance

• AMVs

( IR, WV, VI channels)

• geostationary

(GOES-E/W/P, METEOSAT-5/7)

(circumpolar, Terra & Aqua)

• derived winds

Aircrafts• BUFR / AMDAR

• AIREP / ADS

• Aircrafts

(single level & profiles)

• temperature

• winds

Network now completed!

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Canadian AMDAR Programme Business Case and Workshop March-April 2000

Canadian AMDAR Program Implementation Team:– TORs (EC, NC, airlines, WMO, NOAA, Sypher)– Canadian AMDAR s/w’s Specifications - enhanced ARINC 620-4– Data Ownership and Process & Communication Studies– AMDAR Data Control System’s Specifications (ongoing)

Completion of DASH-8’s AMDAR s/w by UASC (Unilink)

• Lobbying airlines to join, including major PR actions

Air Canada Jazz began reporting July 2002: 21 Air Nova DASH-8s and 10 CRJs presently reporting data– probable fleet expansion to Air BC and Air Ontario (2004-05), JAZZ now planning ~65

CRJ and 60 DASH-8 by March 2006 reception and processing of data by CMC; C-ADAS software

• Partnering with First Air for an alternative AMDAR system

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Canadian AMDAR coverage

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Canadian AMDAR coverage - soundings

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Monitoring of Canadian AMDAR - DASH-8 Temp.

August 02

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Monitoring of Canadian AMDAR - DASH-8 Wind

August 02

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Monitoring of Canadian AMDAR - CRJ Wind/TT

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Canadian AMDAR - Status

• Current sensor on DASH-8 is flush mounted on wing, next to hydraulic lines (non standard)

• AC Jazz Temp probes to be replaced (2 probes) on forward part of fuselage, should fix the Temp bias problem: target is end of 2004

• Monitoring by CMC helped JAZZ to explain a long standing issue related to their FMS generating unneeded steering commands in light wind situations

• First Air: have selected the NASA TAMDAR system for provision of data, test flight with TAMDAR to occur this Summer

• If evaluation of TAMDAR is conclusive, 8 First Air aircraft to start reporting in early to mid 2005.

• All (good) data to be on GTS: IUAA01 CWAO and IUAB01 CWAO, beginning soon with data from CRJ.

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First Air Route (http://www.firstair.ca/images/FA-ROUTE.gif)

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Other Canadian observations

• Canadian AMDAR on GTS soon, using BUFR code

• “Synoptic” observations from CTBTO network, using SYNOP MOBIL code, header: SNCN19 CWAO. Observations every 10-min, 10 stations for now but should increase, received at CMC by e-mail.

• Canadian radar data - will be available centrally at CMC, once NRP (National Radar Processor) becomes operational, in about 1 year

• Forestry and Road weather stations in British Columbia - data received at CMC, in old SA format. Data redistribution restrictions currently apply…should eventually be available in BUFR

• Co-operative network in Quebec (Province, Hydro-Quebec, etc), received at CMC, also redistribution restrictions…eventually in BUFR

• Montreal mesonet, including research wind profiler: under installation but operated by Universities, data not yet available and redistribution restrictions may apply…should be provided to USA profiler hub

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Changes to CMC NWP System since last meeting

Major conversion to IBM machine during 2003 – completed by January 04

New satellite data, implemented June 19, 2003: AMSUB + GOES• 4 AMSU-B channels (ch 2-5)

• GOES 6.7 micron channel (tested GOES 8/10 but 8 replaced by 12, culd implement GOES-10 only)

• last level of moisture analyses raised from 300 to 70 hPa

• impacts mostly on moisture fields and precipitation

• implementation in global system only, due to IBM conversion

•note: loss of NOAA-17 AMSUA data on October 28, 2003

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Average 250 mb (T-Td) analysis increments forAverage 250 mb (T-Td) analysis increments forthe 22 Dec 01 to 31 Jan 02 assimilation periodthe 22 Dec 01 to 31 Jan 02 assimilation period

GOES - CONTROL AMSUB - CONTROL

• AMSUB and GOES have similar average (quite large!!) corrections at 250 mb for T-Td

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ATOVS available for Reg ATOVS available for GlobATOVS available for Reg ATOVS available for Glob

GOES available for RegGOES available for Reg

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AMSU-B+GOES OPE

Results:48h forecast verification

over S. HemisphereAug-Sep 2002

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Verification of 24-48 hr

precipitation NOAM

Dec 02-Jan 03

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Cross Validation with SSM/I - IWV

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Operational WMO Verification

3D-Var GEM3D-Var levels

TOVS 1d

TOVS 1b

3D-VarT,ps

AMSU-BGOES rad

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Changes to CMC NWP System since last meeting

New GEM regional model evaluated in parallel during last 3 months

• MPI code

• 15 km, 58 levels (575 x 641 grid)

• Minimum resolution of 350 km

• Sundqvist condensation scheme

• Kain-Fritsch convection scheme

• Moist TKE (Turbulence en air saturé)

• Ktrans Shallow convection

• Very good results for mass/wind and PCPN

• 8x more cpu than previous regional model (24km, 28 levels)

• Incorporates AMSUB and GOES radiance data (as in global)

• Implemented May 18, 2004

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Results Results fromfrom

PAR run:PAR run:Oper 24-Oper 24-

km vs new km vs new 15-km 15-km GEM;GEM;NOAMNOAM

mid-feb to mid-feb to mid-apr mid-apr

0404

GZ500 UV250

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Results Results fromfrom

PAR run:PAR run:Oper 24-Oper 24-

km vs new km vs new 15-km 15-km GEM;GEM;NOAMNOAM

mid-feb to mid-feb to mid-apr mid-apr

0404

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Implementations planned 2004-05

• Assimilation: new datasets– AMSUA (AQUA), GOES-12, Profilers, MODIS winds Spring 2004– Stratos AMSU-A channels + AMSU-B (raised model top) 2005 +– IR channels (GOES 10-12; METEOSAT, MTSAT and AIRS)– IWV from SSM/I and SSM/IS (eventually from sfc-GPS)– Sfc winds (QuikScat, SSM/IS)

• Global 4D-Var Fall 2004

• Improved GEM Global model Mid 2005

• EnKF (using 3D/4D operators) for EPS and flowdependent statistics Mid 2004

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Difference in RMS of 24-hours Forecast errors, verified against Control analyses done with all the observations:

No Polar Winds – Polar Winds exp., 500 hPa wind vector (m/s), 2003110800-2004012512

Impact of MODIS Polar Winds

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Anomaly correlation, GZ 500 hPaNorthern Hemisphere: Control, No SAT and NOUA

Winter 02 exp Winter 03 exp

17 dec 01 – 27 jan 02 | 8 nov – 31 dec 03

OSE without AMSUB/GOES

OSE with AMSUB/GOES/MODIS

New OSE’s

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Anomaly correlation, GZ 500 hPaSouthern Hemisphere: Control, No SAT and NOUA

17 dec 01 – 27 jan 02 | 8 nov – 31 dec 03

OSE without AMSUB/GOES

OSE with AMSUB/GOES/MODIS

Winter 02 exp Winter 03 exp

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Anomaly correlation, GZ 500 hPaNorth America: Control, No SAT and NOUA

17 dec 01 – 27 jan 02 | 8 nov – 31 dec 03

OSE without AMSUB/GOES

OSE with AMSUB/GOES/MODIS

Winter 02 exp Winter 03 exp

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Global 4D-Var assimilation cycle

• 6h window with 45 min time step.

• 4D data thinning. Spatial data selection is done for each 45 min time bin.

• Incremental analysis performed at T108.

• GEM tangent-linear and adjoint models on 240 x 120 grid.

• 2 outer loops: 40 inner loops : adiabatic physics (vertical diffusion) 30 inner loops : improved physics (SGO, large scale condensation,

convection)

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Recent 4D Results: 20 Jun – 28 Aug 03

4D-Var

OPS-3D

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Improved Global GEMImproved Global GEM

Numerics / Dynamics

• 800 x 600 x L58 (i.e., 33 km at 49o)

• Timestep of 15 min

• Numerical poles at geographical poles

• 6 horizontal diffusion on momentum variables

• Modified sponge layer at model top

• Filtered orography from USGS

Physics

• Constant thermodynamic roughness over water surfaces

• No vertical smoothing on net radiational fluxes

• Bougeault-Lacarrere mixing length for the vertical diffusion

• MoisTKE for boundary-layer clouds

• Shallow convection with Kuo Transient

• Deep convection with Kain-Fritsch

• Grid-scale condensation with a modified Sundqvist scheme (consun)

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Priorities for Satellite Data

• ATOVS: Improved access to Level 1B data (new link with Nesdis), Canadian HRPT data (processing with AAPP) for regional model (cut-off of T+90 min.) and EARS

• SSM/IS

• QuikScat and Envisat (AATSR), both now received, tests underway

• MODIS Products (Winds, SST, LAI, Cloud), winds now tested. A more “operational like” status of NOAA wind product would be very useful.

• METEOSAT and GOES-9 Imagery (MTSAT) (CSR product)

• High Density AMV for GOES9/MTSAT, GOES 9 soon in parallel

• AIRS (assimilation now being tested)

• METOP (IASI,…)