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Table of Contents

Detailed model description

Page containing details for all model configurations available in S2S since the project start => KMA model description

Overview of the model changes

Model version

Implement. date in S2S

Time range

Resolution

Ens. Size

Frequency

Re-forecasts

Rfc period

Rfc frequency

Rfc size

Ocean resolutionActive Sea IceRemarks

GloSea6-GC3.2

01/06/2023 

d 0-60

N216 L85

(0.83° x 0.56°, about 60 km in mid latitudes)

8dailyon the fly1993-2016

4/month

(always on the 1st, 9th, 17th and 25th)

7
yes9 ocean parameters added

GloSea6-GC3.2

22/02/2022

d 0-60

N216 L85

(0.83° x 0.56°, about 60 km in mid latitudes)

4dailyon the fly1993-2016

4/month

(always on the 1st, 9th, 17th and 25th)

3
yes
GloSea5-GC201/09/2020d 0-60

N216 L85

(0.83° x 0.56°, about 60 km in mid latitudes)

4dailyon the fly1991-2016

4/month

(always on the 1st, 9th, 17th and 25th)

3
yes

Nine additional parameters allowing computing MJO indices added since 01/08/2020 to the real-time data and since 01/09/2020 to the reforecasts.

Specific Humidity on pressure level provided since 01/08/2020

GloSea5-GC201/11/2016d 0-60

N216 L85

(0.83° x 0.56°, about 60 km in mid latitudes)

4dailyon the fly1991-2010

4/month

(always on the 1st, 9th, 17th and 25th)

3
yes

Description of the main changes

01-09-2020

Extension of the reforecast period from 1991-2010 to 1991-2016.

01-08-2020

Nine additional parameters allowing computing MJO indices were added  to the KMA outputs starting from 1  August 2020 for the real-time forecasts and from 1 September for the on-the-fly reforecasts:

  • Snow Fall water equivalent
  • Surface net solar radiation
  • Surface net thermal radiation
  • Surface solar radiation downwards
  • Surface thermal radiation downwards
  • Top net thermal radiation
  • Sea surface temperature
  • Total Cloud Cover
  • Specific humidity (on pressure levels)

31-10-2017

In

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Changes:

...

reference to Tennant(2013), the soil moisture content(SMC) and surface temperature perturbations were added to KMA’s Global Ensemble system. It should improve predictive performance of the surface variations that have a smaller spread than the upper level one. Together with SST perturbation, it helps improving the spread of surface temperature and moisture.
References: Tennant. W, 2013: New schemes to perturb sea-surface temperature and soil moisture content in MOGREPS. Q.J.R.Meteorol. Soc., 140, 1150-1160