1. Forecast system version

System name: GloSea6-GC5.1

First operational forecast run: 3 March 2026

2. Configuration of the forecast model

Is it a coupled model?  Yes: Atmosphere, land, ocean and sea-ice.

Coupling frequency:  Hourly coupling between atmosphere-land and ocean-sea-ice.

The coupled model Global Coupled 5.1 (GC5.1) is described in Xavier et al., 2023.

2.1 Atmosphere and land surface

Model

Met Office Unified Model (UM) - Global Atmosphere and Land 9.1

Horizontal resolution and gridN216: 0.83 degrees x 0.56 degrees (approx 60km in mid-latitudes)
Atmosphere vertical resolution85 levels
Top of atmosphere85km
Soil levels (layers)

4

Layer 1 : 0 - 0.1 m
Layer 2 : 0.1 - 0.35 m
Layer 3 : 0.35 - 1.0 m
Layer 4 : 1.0 - 3.0 m

Time step15 minutes

Detailed documentation:

JULES documentation 

2.2 Ocean and cryosphere

Ocean model

NEMO v4.0.4 - Global Ocean Sea Ice 9.0

Horizontal resolutionORCA 0.25
Vertical resolutionL75
Time step30 minutes
Sea ice model

SI3 - Global Ocean Sea Ice 9.0

Sea ice model resolutionORCA 0.25
Sea ice model levels5 categories + open water
Wave modelN/A
Wave model resolutionN/A

Detailed documentation: NEMO documentation

GOSI9: Guiavarc'h et al, 2025.

3. Boundary conditions - climate forcings


Greenhouse gasesCO2, CH4, N2O, CFC12, HCFC134a - SSP2-4.5
OzoneCMIP6.  Zonal mean climatology 1993-2014.
Tropospheric aerosolsDerived from climatology of Model with full aerosol scheme
Volcanic aerosolsBackgroud aerosol
Solar forcingCMIP6


Detailed documentation:

4. Initialization and initial condition (IC) perturbations

4.1 Atmosphere and land


HindcastForecast
Atmosphere initialization
ERA-5Met Office Global Hybrid 4D-VAR
Atmosphere IC perturbationsNoneNone
Soil moisture & temperature  initializationMet Office JULES-ERA5 analysisMet Office JULES-ERA5 analysis
Snow initialization

 Met Office JULES-ERA5 analysis

Met Office JULES-ERA5 analysis
Unperturbed control forecast?NoNo

Detailed documentation:

Met Office Global Hybrid 4D-VAR: Clayton et al, 2013

ERA5: Hersbach et al., 2020 


4.2 Ocean and cryosphere


HindcastForecast
Ocean initializationGloSea Ocean Sea-Ice Analysis (GS-OSIA)Forecast Ocean Assimilation Model (FOAM)
Ocean IC perturbationsNoNo
Unperturbed control forecast?NoNo

Detailed documentation:

The GS-OSIA and the FOAM system both use the Nucleus for European Modelling of the Ocean data assimilation system (NEMOVAR). This is a 3d-VAR data assimilation scheme. The GS-OSIA uses different surface forcing (ERA-5) and observation sets as it is a historical analysis. FOAM uses surface forcing from the Met Office Global NWP model and real-time observations.

The common NEMOVAR system is described in Blockley et al, 2014. 


5. Model uncertainties perturbations:

Model dynamics perturbationsNone
Model physics perturbationsAtmosphere stochastic physics scheme, SKEB2

If there is a control forecast, is it perturbed?

No control

Detailed documentation:

SKEB2: Bowler et al, 2009

6. Forecast system and hindcasts


Forecast frequencydaily
Forecast ensemble size2 per day
Hindcast years24 (1993-2016)
Hindcast ensemble size7 per start date
Hindcast start dates1, 9, 17, 25 of each month
On-the-fly or static hindcast set?on-the-fly

7. Other relevant information

Interpolation details
Horizontal Interpolation

Atmosphere: area weighted regrid from N216 to 1x1 degree.

Ocean: uses a two-stage regrid.

  1. Area weighted regrid fom ORCA025 grid to N216 grid (using same weights as used in model coupling)
  2. Area weighted regrid from N216 to 1x1 degree
Vertical interpolation

Atmosphere: linear interpolation from the model hybrid height grid onto pressure levels.

8. Where to find more information

GloSea system:

Model description references:

Initialisation references:

Forcing references: