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Table of Contents
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1. Forecast system version

System name: GloSea5-GC2Identifier code: SEAS5

First operational forecast run: 1 November 20173 February 2015

2. Configuration of the forecast model

Is the model coupled to an ocean it a coupled model ?  Yes from day 0: Atmosphere, land, ocean and sea-ice.

Coupling frequency: 1 hour3-hourly coupling between atmosphere-land and ocean--sea-ice.

The coupled model Global Coupled 2 (GC2) is described in Williams et al, 2015.

2.1 Atmosphere and land surface

Model

Met Office Unified Model

(UM) - Global Atmosphere 6.0

Joint UK Land Environment Simulator (JULES) - Global Land 6.0

IFS Cycle 43r1

Horizontal resolution and grid

Dynamics:TCO319 Cubic octahedral grid

Physics: O320 Gaussian grid (36 kmN216: 0.83 degrees x 0.56 degrees (approx 60km in mid-latitudes)
Atmosphere vertical resolutionL91 (0.01 hPa)85 levels
Top of atmosphere85km
Soil levels

4

Level 1 : 0 - 0.1 m

Level 2 : 0.

01 hPa (approx. 80 km)
Soil levels

1 - 0.35

Level 3 : 0.35 - 1.0 m

Level 4 : 1.0 - 3.0 m

4

Time step20 15 minutes

Detailed documentation: IFS cycle 43r1 documentation

...

JULES documentation

Global Atmosphere 6.0 & Global Land 6.0: Walters et al, 2017

 

2.2 Ocean and cryosphere

Ocean model

NEMO v3.4 - Global Ocean 5.0

Horizontal resolutionORCA 0.25
Vertical resolutionL75
Time step1 hour22.5 minutes
Sea ice modelLIM2CICE v4.1 - Global Sea-Ice 6.0
Sea ice model resolutionORCA 0.25
Sea ice model levelsN/A5 categories + open water
Wave modelECMWF wave modelN/A
Wave model resolution0.5 degreesN/A

Detailed documentation: NEMO documentation and IFS cycle 43r1 documentation, CICE documentation

Global Ocean 5.0: Megann et al, 2014

Global Sea Ice 6.0: Rae et al, 2015.

3. Initialization and initial condition (IC) perturbations

3.1 Atmosphere and land


Re-forecastHindcastForecast
Atmosphere initialization
ERA-InterimECMWF OperationsMet Office Global Hybrid 4D-VAR
Atmosphere IC perturbationsEnsemble data assimilation and leading singular vectors applied to upper air variablesNoneNoneEnsemble data assimilation and leading singular vectors applied to upper air variables

Land Initialization

Climatology/ERA-Interim land (43r1)Climatology/Met Office Global Hybrid 4D-VARECMWF Operations
Land IC perturbationsEnsemble data assimilation applied to some land fieldsNoneNoneEnsemble data assimilation applied to some land fields
Soil moisture initializationERA-Interim landClimatologyClimatologyECMWF operations
Snow initializationERA-Interim landECMWF operationsMet Office Global 4D-VAR
Unperturbed control forecast?YesNoYesNo

Detailed documentation: IFS cycle 43r1 documentation and SEAS5 user guide

More DA details?

Data assimilation method for control analysis: 4D Var (atmosphere) and 3DVAR (ocean/sea-ice)

Horizontal and vertical resolution of perturbations:  T42L91 SVs+ T399L137 EDA perturbations

Met Office Global Hybrid 4D-VAR: Clayton et al, 2013 Perturbations in +/- pairs: Yes


3.2 Ocean and cryosphere


Re-forecastHindcastForecast
Ocean initializationORAS5GloSea Ocean Sea-Ice Analysis (GS-OSIA)Forecast Ocean Assimilation Model (FOAM)ORTA5
Ocean IC perturbations Yes - generated through perturbations to assimilated observations and surface forcingNoNoYes - generated through perturbations to assimilated observations and surface forcing
Unperturbed control forecast?NoNo

Detailed documentation: ECMWF ocean reanalysis documentation and SEAS5 user guide

Ocean data assimilation details? Source and treatment of SST? (Other data sources - altimetry?)

The GS-OSIA and th e 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-interim) 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 . Details of the GS-OSIA can be found in MacLachlan et al, 2015 .


4. Model uncertainties

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perturbations:

Model dynamics perturbationsNoNone
Model physics perturbations3-lev SPPT and SPBSAtmosphere stochastic physics scheme, SKEB2

If there is a control forecast, is it perturbed?

YesNo control

Detailed documentation: IFS cycle 43r1 documentation:

SKEB2: Bowler et al, 2009

5. Forecast system and

...

Note, the ECMWF seasonal forecasts cover two time ranges: the long range (LR) forecasts out to 7 months, and annual range (AR) forecasts out to 13 months. The model used for these forecasts is identical, but they have different numbers of forecast members.

hindcasts


Forecast frequencydaily
Forecast frequency

monthly (LR)

quarterly (AR)Re-forecast years36 (1981-2016)Re-forecast ensemble size

25 (LR)

15 (AR)

Forecast ensemble size

51 (LR)

15 (AR)

2 per day
Hindcast years23 (1993-2015)
Hindcast ensemble size7 per start date
Hindcast start dates1, 9, 17, 25 of each month
On-the-fly or static
re-forecast
hindcast set?
staticCalibration (bias correction) period1993-2016
on-the-fly


6. Where to find more information

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ECMWF seasonal forecast documentation page


GloSea5 system:

Model description references:

Initialisation references:

...