Variations in seasonal-forecasting skill and predictability during the 15 y
ears (1979-93) of the European Centre for Medium-Range Weather Forecasts (E
CMWF) re-analysis (ERA), have been studied using 120-day ensemble integrati
ons of the ECMWF model. These integrations form part of the European Union
PROVOST (PRediction Of climate Variations On Seasonal to interannual Time-s
cales) project. Observed sea surface temperatures (SSTs) were updated daily
at the model's lower boundary. Two major and three moderate El Nino Southe
rn Oscillation (ENSO) events occurred during the ERA period. Results are in
terpreted as giving an upper bound on the predictive skill of a coupled oce
an-atmosphere system as a function of season, location, and state of ENSO.
The model systematic error was found to be comparable with a typical amplit
ude of interannual variation. When standardized by the corresponding ERA an
omaly variance, systematic error appears to be largest in boreal spring in
the northern extratropics, and in boreal summer in the tropics.
Ensemble-mean skill scores were found to be positive overall. Apart from th
e northern winter season, the ensemble-mean skill for months 2-4 drops sign
ificantly when compared with months 1-3. The interannual variation of skill
scores is much larger for the European region than for the hemispheric dom
ain. Over the northern hemisphere, skill is much higher when only ENSO year
s are considered; for Europe, the enhancement in skill for ENSO years is mu
ch weaker.
Estimates of intrinsic predictability were made for each year of the datase
t. These estimates, defined both by a t-test and variance ratio, indicate g
enerally high predictability in years when ENSO was strong. Apart from nort
hern winter, the predictability estimates also showed a systematic drop bet
ween months 1-3 and months 2-4. It is therefore concluded that the fall in
skill scores between months 1-3 and 2-4 indicates more a weakening of the i
mpact of initial conditions (ICs) than, say, an increase in the effects of
model error. In order to study this further, the relative impacts of SSTs a
nd ICs, including land surface ICs, on interannual variation of precipitati
on have been examined in an additional set of experiments. Overall, SSTs ha
ve a dominant role, though the impact of ICs is not negligible.
The predictability of tropical and extratropical precipitation is also disc
ussed. The level of skill for precipitation in the extratropics is generall
y lower than in the tropics. However, within the tropics there are regions
where the precipitation exhibits chaotic behaviour and is correspondingly l
ess predictable.