| When was the current long-range forecast system implemented? |
System Name : GloSea6GC3.2 |
|---|---|
| Is it a coupled forecast system? | Yes |
| Is it a Tier-2 forecast system? | No |
| Atmospheric model resolution |
UM: N216L85 |
| Ocean model (if applicable) |
NEMO: |
| Source of atmospheric initial conditions |
Forecasts : KMA NWP Hindcast : ERA-interim |
| Source of ocean initial conditions |
Forecasts : KMA GODAPS2 (Global Ocean Data Assimilation System v2) Hindcasts : UKMO ODA Reanalysis |
| If Tier-2, what is the source of SST predictions? | N/A |
| Hindcast Period | 1993-2016 |
| Ensemble size for the hindcasts | 28 members (from 4 different start dates) |
| How is the hindcast ensemble configured? | Lagged approach, 7 members per start date on the 1st, 9th, 17th, and 25th, of each calendar month. All 7 member share the same initial conditions and differ only due to schemes to represent model uncertainties |
| Ensemble size for the forecast | 84 |
| How is the forecast ensemble configured? | Lagged approach, 4 members per each date on 3weeks (21days) |
| Length of forecasts | 6 months |
| Data Format | GRIB 2 |
| What is the latest date predicted anomalies for the next month/season become available? | 13th of the month |
| How are the forecast anomalies constructed? | Departures from the model climate estimated by the hindcast integrations |
| URL where forecast are displayed | http://www.wmolc.org/~GPC_Seoul |
| Point of Contact | Ms. Juyon Lim (anisse@korea.kr) |
