1. Forecast system version

Identifier code: GEM5.2-NEMO

First operational forecast run: 30 June 2024

2. Configuration of the forecast model

Is the model coupled to an ocean model?  Yes

Coupling frequency:  30 minutes

2.1 Atmosphere and land surface

ModelGEM5.2 (atmosphere), ISBA (land)
Horizontal resolution and grid283×190 Yin-Yang grid (~110 km)
Atmosphere vertical resolution85 levels
Top of atmosphere0.1 hPa
Soil levels

2

Layer 1: 0 - 10 cm 
Layer 2: 10 - 280 cm

Time step30 minutes

Detailed documentation:

Diro, G. T. et al. 2024: The Canadian Seasonal to Interannual Prediction System version 3.0 (CanSIPSv3,0). Canadian Meteorological and Environmental Prediction Centre technical note, Environment and Climate Change Canada, https://collaboration.cmc.ec.gc.ca/cmc/cmoi/product_guide/docs/tech_notes/technote_cansips-300_20240611_e.pdf

2.2 Ocean and cryosphere

Ocean modelNEMO3.6
Horizontal resolutionORCA1
Vertical resolution50 levels
Time step30 minutes
Sea ice modelCICE6
Sea ice model resolutionORCA1
Sea ice model levels5 ice-thickness categories
Wave modelN/A
Wave model resolutionN/A

Detailed documentation:

Diro, G. T. et al. 2024: The Canadian Seasonal to Interannual Prediction System version 3.0 (CanSIPSv3,0). Canadian Meteorological and Environmental Prediction Centre technical note, Environment and Climate Change Canada, https://collaboration.cmc.ec.gc.ca/cmc/cmoi/product_guide/docs/tech_notes/technote_cansips-300_20240611_e.pdf

3. Boundary conditions - climate forcings

Greenhouse gasesObserved annual globally averaged values for CO2, N2O, CH4, CFC11 and CFC12 assembled from several sources including the WMO Greenhouse Gas Bulletin https://wmo.int/publication-series/greenhouse-gas-bulletin
OzoneMonthly climatological latitude and height dependent climatologies based on Fortuin and Kelder (1998)
Tropospheric aerosolsN/A
Volcanic aerosolsN/A
Solar forcingN/A

Detailed documentation:

Fortuin J. P. F. and H. Kelder, 1998: An ozone climatology based on ozonesonde and satellite measurements. Journal of Geophysical Research103, 31709-31734, doi:10.1029/1998JD200008

4. Initialization and initial condition (IC) perturbations

4.1 Atmosphere and land


HindcastForecast
Atmosphere initialization
ERA5ECCC GEPS
Atmosphere IC perturbationsRandom isotropic perturbationsEnsemble Kalman Filter

Land Initialization

Off-line ISBA-based Surface Prediction System (SPSv6.2)

forced by 1-hourly lowest-level ERA5 fields

ECCC GDPS output adjusted to hindcast climatology
Land IC perturbationsNoneNone
Soil moisture initialization

Off-line ISBA-based Surface Prediction System (SPSv6.2)

forced by 1-hourly lowest-level ERA5 fields

ECCC GDPS output adjusted to hindcast climatology
Snow initialization

Off-line ISBA-based Surface Prediction System (SPSv6.2)

forced by 1-hourly lowest-level ERA5 fields

ECCC GDPS output with prescribed climatological snow over Tibetan Plateau
Unperturbed control forecast?NoneNone

Detailed documentation:

Gauthier, P., et al. 1999: Background-error statistics modelling in a 3D variational data assimilation scheme: Estimation and impact on the analyses. Proc. ECMWF Workshop on Diagnosis of Data Assimilation Systems, Reading, United Kingdom, ECMWF, 131–145, 

https://www.ecmwf.int/sites/default/files/elibrary/1999/9500-background-error-statistics-modelling-3d-variational-data-assimilation-scheme-estimation-and.pdf 

Houtekamer, P.L., et al. 2009: Model Error Representation in an Operational Ensemble Kalman Filter. Monthly Weather Review, 137, 2126-2143, https://doi.org/10.1175/2008MWR2737.1


4.2 Ocean and cryosphere


HindcastForecast
Ocean initializationORAS5CCMEP GIOPS analysis
Ocean IC perturbationsNoneNone
Unperturbed control forecast?NoneNone

Detailed documentation:

 

5. Model Uncertainties perturbations:

Model dynamics perturbationsNone
Model physics perturbations
  • Stochastic perturbation of 17 parameters (SPP).
  • Modified parameter values and ranges are based on simulated climatology and variability (e.g., tropical waves) and forecast skill

If there is a control forecast, is it perturbed?

No control forecast

Detailed documentation: 

Diro, G. T., et al. 2024: The Canadian Seasonal to Interannual Prediction System version 3.0 (CanSIPSv3,0). Canadian Meteorological and Environmental Prediction Centre technical note, Environment and Climate Change Canada, https://collaboration.cmc.ec.gc.ca/cmc/cmoi/product_guide/docs/tech_notes/technote_cansips-300_20240611_e.pdf

McTaggart-Cowan, R., et al. 2022: Using stochastically perturbed parameterizations to represent model uncertainty. Part I: Implementation and parameter sensitivity. Monthly Weather Review, 150, 2829-2858, https://doi.org/10.1175/MWR-D-21-0315.1

McTaggart-Cowan, R., et al. 2022: Using stochastically perturbed parameterizations to represent model uncertainty. Part II: Comparison with existing techniques in an operational ensemble. Monthly Weather Review, 150, 2859-2882, https://doi.org/10.1175/MWR-D-21-0316.1

6. Forecast system and hindcasts

Forecast frequency12-month forecast is produced on the last day of each month
Forecast ensemble size20 (ensemble members 1-10 initialized at 00Z on last day of month, 11-20 at 00Z on 5th to last day of month)
Hindcast years1980-2023
Hindcast ensemble size20 (ensemble members 1-10 initialized at 00Z on first day of month, 11-20 at 00Z on 5th to last day of previous month)
On-the-fly or static hindcast set?static

7. Other relevant information

A significant update between GEM5-NEMO (based on the GEM5.1 AGCM) and GEM5.2-NEMO is that adjustments to the parameterization of non-orographic gravity waves in the tropics in GEM5.2-NEMO has enabled the model to simulate a realistic Quasi-Biennial Oscillation. 

Horizontal interpolation from the native model grids to the C3S 1x1-degree grid: bilinear interpolation with filling/masking for land-only and ocean-only fields

Vertical interpolation pressure levels: 

  • For temp/phi near the surface, log-linear interpolation (linear in ln(eta)) with the lapse rate of 6.5e-3 deg/m
  • For remaining variables near the surface and all variables near the top, constant extrapolation, i.e. keep same value from the closest model level

8. Where to find more information

https://weather.gc.ca/saisons/index_e.html

https://climate-scenarios.canada.ca/?page=seasonal-forecasts 

https://collaboration.cmc.ec.gc.ca/cmc/cmoi/product_guide/docs/tech_notes/technote_cansips-300_20240611_e.pdf