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| Medium-Range High-Resolution Forecast |
Medium-Range Ensemble Forecast |
Long-Range Forecast |
Operational forecasts
ECMWF produces a suite of operational forecasts for various lead times:
- Medium-range forecast: comprises the high-resolution and the ensemble forecasts of weather, at the space and time-scales represented by the relevant model, up to 10 and 15 days ahead, respectively, and the associated uncertainty.
- Extended-range (monthly) forecast: comprises ensembles of individual forecasts and post-processed products of average conditions (e.g. weekly averages) up to 1 month ahead, and the associated uncertainty.
- Long-range (SEAS) forecast: comprises ensembles of individual forecasts and post-processed products of average conditions (e.g. monthly averages) up to 13 months ahead, and the associated uncertainty.
In addition re-forecasts are calculated operationally using the current system configuration but applied to the weather over past decades:
- Re-forecasts: comprise forecasts run for past decades necessary to estimate the model climate and the level of skill and to generate some of the operational products.
These forecasts are produced using the ECMWF Integrated Forecasting System (IFS).
Component models
There are five component models of the IFS.
- Atmospheric model with various configurations suited to the space scale and time range of the required forecasts. The current configurations for High Resolution (HRES), Ensemble (ENS) and Boundary Conditions (BC) are given in Table 1a.
- Ocean wave model is a version of the WAve Model (WAM) model which has been further developed in house. It is coupled to the atmospheric model or run as a standalone model in the Limited-Area Wave (LAW) configuration.
- Ocean model is a version of the NEMO (Nucleus for European Modelling of the Ocean) model.
- Process models are used to describe, for example, land-surface processes, surface ocean waves, and sea-ice.
- Perturbation models are used to simulate the effect of uncertainties in the observations, initial conditions, surface boundary conditions, and modelled processes. These produce perturbations for use in ensemble forecasts.
Component analyses
In addition, there are five components for analysing the state of the atmosphere and oceans.
- 4DVAR (4-Dimensional Variational analysis) provides a detailed estimate of the current state of the atmosphere computed utilising as optimally as possible observations and prior information about the Earth-system using ECMWF’s highest resolution model.
- EDA (Ensemble of Data Assimilations) provides an ensemble of estimates of the current state of the atmosphere and its uncertainty. The EDA estimate of the analysis uncertainty can be used as an approximation of the 4DVAR uncertainty. The current configuration of EDA is given in Table 1a.
- ORTA (Ocean Real-Time Analysis) provides an estimate of the ocean initial state and its uncertainty. The current configuration of ORTA is given in Table 1c.
- ERA (ECMWF Reanalysis) provides consistent estimates of the state of the atmosphere generated using a fixed, lower-resolution version of 4DVAR for the past decades. The latest ERA product, ERA-Interim, covers the period since 1979 and is continued in real time to support climate monitoring. ERA-Interim is also used to define the atmospheric initial conditions of the re-forecasts.
- ORA (Ocean Reanalysis) is the equivalent of ERA for the oceans.
Key characteristics of the forecasting system
Table 1a: Key characteristics in 2012 of the operational configurations of the ECMWF IFS
|
Forecast/Analysis |
Number of members |
Horizontal resolution |
Vertical levels and
pressure at model top (hPa) |
Perturbation models |
IFS cycle |
HRES |
Forecast
0–10 days |
1 |
T1279/16 km |
91/0.01 |
No |
Latest |
ENS |
Forecast
0–10 days |
51 |
T639/32 km |
62/0.5 |
Yes (in analysis and model physics) |
Latest |
| ENS |
Forecast
10–32 days |
51 |
T319/64 km |
62/0.5 |
Yes (in analysis and model physics) |
Latest |
4DVAR |
Analysis |
1 |
T1279/16 km
(T255 inner loops) |
91/0.01 |
No |
Latest |
EDA |
Analysis |
11 |
T399/50 km (T159 inner loops) |
91/0.01 |
Yes (in observations and model physics) |
Latest |
SEAS |
Forecast
0–13 months |
51 |
T255/80 km |
91/0.01 |
Yes (in analysis and model physics) |
2011 version |
ERA |
Analysis |
1 |
T255/80 km |
60/0.1 |
No |
2006 version |
BC |
Forecast
0–90 hours, hourly output |
1 |
T1279/16 km |
91/0.01 |
No |
Latest |
Table 1b: Key characteristics in 2012 of the ENS and SEAS re-forecasts
|
Forecast/Analysis |
Number of members |
Horizontal resolution |
Vertical levels |
Top of the Atmosphere |
Perturbation models |
IFS cycle |
Number of years |
ENS |
Forecast
0–10 days |
5 run once a week |
32 km |
62 |
0.5 hPa |
Yes (in analysis and model physics) |
Latest |
Most recent 20 |
| ENS |
Forecast
10–32 days |
5 run once a week |
64 km |
62 |
0.5 hPa |
Yes (in analysis and model physics) |
Latest |
Most recent 20 |
SEAS |
Forecast
0–13 months |
15 run once a month |
80 km |
91 |
0.01 hPa |
Yes (in analysis and model physics) |
2011 version |
30
(1981–2010) |
Table 1c: Key characteristics in 2012 of the ocean component models of the ECMWF IFS
|
Forecast/Analysis |
Number of members |
Horizontal resolution |
Vertical levels |
Model cycle
|
NEMO |
Forecast
0–13 months |
51 |
1° |
42 |
Latest |
ORA-ORTA |
Analysis |
5 |
1° |
42 |
Latest |
Table 1d: Key characteristics in 2012 of the ocean-wave component
|
Forecast/Analysis |
Domain |
Number of members |
Horizontal resolution |
Number
of
directions |
Number
of frequencies |
LAM WAM |
Analysis +
forecast
0–5 days |
Limited:
5°N-90°N,
98°W-54°E |
1 |
11 km |
36 |
36 |
WAM HRES |
Analysis and
forecast
0–10 days |
Global |
1 |
28 km |
36 |
36 |
WAM
ENS |
Forecast
0–10 days |
Global |
51 |
55 km |
24 |
30 |
WAM
ENS |
Forecast
10–32 days |
Global |
51 |
55 km |
12 |
25 |
WAM SEAS |
Forecast
0–13months |
Global |
51 |
111 km |
12 |
25 |
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