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Production suite overview

MSC - EC - GC
 

Timelines of Numerical Weather Prediction

Historical changes of models and analyses

2005

January 12
Data assimilation in the Ensemble Forecast System: Optimum Interpolation is replaced by the Ensemble Kalmann Filter method
March 15
4D-Var analysis implemented in the Global data assimilation system.

2004

May 18
New GEM regional model at 15 km.  Bring satellite data assimilation in regional analysis to same level as in global analysis

2003

Febuary 24-28
New GCM II model for seasonal forecasts
September
Public access to model output in GRIB format via Weatheroffice

2001

January 11
Implementation of a new regional analysis on "eta" coordinates. Addition of TOVS and ACARS/AMDAR data

2000

June 14
Implementation of a new global analysis on "eta" coordinates. The 3D-Var data assimilation is performed directly on the GEM model 28 eta vertical levels. Implementation of new GEM version to increase the level of activity in the model.
September 27
Improvements to the global analysis: addition of TOVS and ACARS/AMDAR data

1998

January 22
Improvements of the operational force-restore land-surface scheme
March 11
New snow analysis
September 15
Regional GEM's hor. resolution increases from 35km to 24 km. The number of vertical levels stays 28. Improvements of some parametrizations of the physics processes.
October 14
The SEF model (T199/21L) is replaced by the GEM model - global configuration. The global GEM resolution is 0.9º and 28 levels.

1997

February 24
The RFE model is replaced by GEM regional. No regional analysis cycle. The regional GEM model is initialized with the global analysis on 16 pressure levels.
June 10
The regional GEM model is initialized with the global analysis on 21 sigma levels instead of the analysis on pressure levels
June 18
The OI is replaced by the 3D-VAR scheme.
September 24
Re-introduction of the regional analysis cycle. (with 12-hour spin-up). The resulting regional analyses are used to initialize the regional GEM.
November
Installation of the experimental GEM 15 km run (HIMAP)

1995

June 14
Global SEF model with increased resolution from T119 to T199L21
July 26
A new surface layer treatment in EFR as well as a soil humidity analysis that compensates for the surface humidity biases of the model (error feedback of the surface dew point forecast)
August 9 & 30
Two versions of HUMSAT were implemented in quick succession
September 19
Improved snow analysis (changes to the albedo calculation over snow)
December 13
Increase of the resolution of the RFE model: from 50km/25levels to 35km/28 levels

1994

July 21
New sea surface temperature analysis running once a day based on the analysis of anomalies with respect to climatology. New climatology fields were implemented at the same time
September 21
New 3-D upper air objective analysis was implemented (versus previous split horizontal and vertical scheme): includes additional level at 925 hPa and improved treatment of SATEMS. Temperature are diagnosed for the height analyses

1993

June 16
New higher resolution global system with HUMSAT. Model increased from T79 to T119 with the same number of vertical levels (21). Physics is considerably changed with KUO, shallow convection and new radiation scheme
November 3
New 50km/25 level EFR with new physics package (similar to Spectral SEF except for minor differences). Output is kept on a variable grid. HUMSAT is used in the regional assimilation cycle

1992

March 18
New ice analysis based on SSM/I data; new snow depth analysis on 400x200 global gaussian grid. Optimized spectral model about 12% more efficient. Changes in the warming in the upper stratosphere; new analysis of humidity when temperatures are below 0C.
Dec 16
New NEC SX-3/44 replaces Cray. EFR 100km has increased levels to 23 and a slightly modified physics package (including a new radiation and shallow convection). A regional analysis with a 12-h spin-up was implemented.

1991

March 12
Global spectral model (SEF T79/21 levels) replaces the spectral hemispheric model; new global data assimilation system; global surface mean sea level and surface air temperature analyses
August 1
New spectral model that removes warm west coast bias

1990

March
Reduced bias in EFR installed on XMP-416
July 4
New sea surface temperature on 400X200 on global gaussian grid
November 8
Changes to the trial field model as well as the spectral forecast model to correct a problem with levels below the surface

1989

January 25
New OA with new horizontal and vertical correlation functions statistics

1988

Febuary 23
Improved vertical resolution of EFR to 19 levels
June 15
Global OA operated in hemispheric mode. Analysis of residuals
October 31
Trial field model is the spectral T89/20L model
Dec 7
100km resolution EFR model with microtasking

1987

Febuary 11
Optimization of the EFR (10% faster)
April 12
Conversion to XMP-28 with 152.4KM resolution and implicit non-linear normal mode initialization
July 21
OA improvements: extended search of best 24 in nearest 40 observations on 180x45 gaussian grid
October 27
Code optimization and improvements to the treatement of water vapour fluxes and virtual temperature

1986

Febuary 20
More efficient global code - highly vectorized
April 22
Operational implementation of the EFR model (Regional Finite Element/Éléments Finis Régionaux) at 190km resolution, 15 vertical levels and spectral normal mode intialization
October 23
Expansion of core window of EFR;
reduction in maximum grid length spacing to 228.6km
Dec. 17
Spectral model improvements. Installed on Cray XMP-28, later in 1987

1985

April
Improved V9 spectral on 130X32 gaussian grid

1984

June
Spectral model with triangular 59 (T59) truncation and 15 levels (15L) in the vertical installed on the Cray 1S

1983

May
Improved version 9 of the spectral model

1981

Fall
Spectral R29 13L model (gaussian grid 96X32)
New objective analysis was introduced. Normal mode initialization

1978

January
Optimal interpolation (OI) used in an objective analysis on a gaussian grid
December
Spectral R29 10L model, version 8 physics

1977

March
Spectral R29 5L model
V7 physics

1976

Febuary 18
Spectral model, 20 waves, with rhomboidal truncation (R20) and 5 levels (5L) in the vertical. Featured version 6 (V6) physics.

1975

mid
A Baroclinic 7 level primitive equation model was installed on Cyber 7600.

1968

September
A Baroclinic 4 level model was installed on an IBM 360-65.
"Kruger" type analysis was being used.

1962

fall
A barotropic model was run on a Bendix machine.
First operational forecast 500hPa chart was done in July 1963.

1950

mid
A barotropic model using the Fjortoff method
late
A barotropic model was run on the IBM 650 at McGill University.
Model was run on an experimental basis only.

Evolution of the CMC's regional forecasting system since 1986

2004

January 7
Conversion to the new IBM supercomputer of the regional and global forecast systems
May 18
15 km Regional model implantation.
New satellite data TOVS and GOES for assimilation. 

2003

June 19
Corrections to TOVS AMUS-B data assimilation for the regional model

2002

December 10
TOVS assimiliation in global and regional models

2001

January 11
Implementation of a new regional analysis on "eta" coordinates. Addition of TOVS and ACARS/AMDAR data
June 7
ATOVS-1B assimilation in global and regional analysis systems
September 11
ISBA surface scheme implantation in the GEM regional
December 11
New data set for 3D-Var assimilation (ACARS,AMDAR, 5 more channels TOVS and SATWINDS of GOES)
New variational quality control scheme

1998

September 15
GEM (24km, 28 levels) / REGIONAL analysis 3D-VAR (12-hour spin-up)
October 14
global GEM (0.9°/28 levels) replaces the SEF model (T199/21 levels>

1997

February 24
GEM (35km, 28 levels) initialized from global analysis OI 3D (without spin-up)
June 18
3D-Var global analysis
GEM initialized from 3D-Var global analysis (no spinup)
September 24
Regional 3D-Var analysis implemented with 12-hour spin-up

1996

December 13
RFE (35km, 28 levels) / REGIONAL analyse OI 3D (12-hour spin-up)

1995

June 14
SEF model T199L21

1994

September 21
3D global analysis

1993

June 16
SEF model T119L21
November 3
RFE (50km, 25 levels) / REGIONAL analysis OI 2D (12-hour spin-up)

1992

December 16
RFE (100km, 23 levels) / REGIONAL analysis OI 2D (12-hour spin-up)

1991

March 12
RFE (100km, 19 levels) / global analysis OI 2D

1988

February 23
RFE (152.4km, 19 levels) / OI hemispherical analysis in 2D
RFE (100km, 19 levels) / OI hemispherical analysis in 2D
global analysis with SEF T79L21 (implemented on Mars 12, 1991)

1987

April 12
RFE (152.4km, 15 levels) / OI hemispherical analysis in 2D

1986

April 22
RFE (190km, 15 levels)/ OI hemispherical analysis in 2D

Evolution of the CMC's global forecasting system since 1950

2005

March 15
4D-Var global analysis is implemented. The analysis fits data along the time axis as well as in the three spatial dimensions.

2004

January 7
Conversion to the new IBM supercomputer of the regional and global forecast systems

2003

June 19
Corrections to TOVS AMUS-B data assimilation for the regional model

2002

December 10
TOVS assimiliation in global and regional models

2001

June 7
ATOVS-1B assimilation in global and regional analysis systems.
December 11
New data set for 3D-Var assimilation (ACARS,AMDAR, 5 more channels TOVS and SATWINDS of GOES)
New variational quality control scheme
Corrections to the global model for better wind treatment in highly mountainous terrain

2000

June 14
Implementation of a new global analysis on "eta" coordinates. Implementation of new GEM version to increase the level of activity in the model.
September 27
Improvements to the global analysis: addition of TOVS and ACARS/AMDAR data

1998

October 14
global GEM model 0.9°/L28

1997

June 18
3D-Var analysis

1995

June 14
global spectral model SEF T199/L21

1994

July 21
3D analysis

1993

June 16
global spectral model SEF T119/L21 with new physic

1991

March 12
global spectral model SEF T79/L21 with global analysis

1985

April
spectral model T59/15L with improved V9 physics version, gaussian grid 130x32

1988

June 15
global objective analysis in hemispheric mode

1984

June
spectral model T59/15L

1983

May
spectral model R29/13L with V9 physics

1981

December
spectral model R29/13L on gaussian grid 96x32

1978

January
Optimal Interpolation analysis
December
spectral model R20/10L with V8 physics

1977

March
spectral model R29/5L with V7 physics

1976

February 18
spectral model R20/5L with V6 physics

1975

September
baroclinic model with 7 levels

1968

September
baroclinic model with 4 levels

1950-1960

barotropic model


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Created : 1997-02-24
Modified : 2005-04-07
Reviewed : 2002-12-18
Url of this page : http://www.msc.ec.gc.ca
/cmc/op_systems/historical_e.html

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