## 15.4 Forecasts combinations in ADAM

When it comes to achieving as accurate forecasts as possible in practice, the best and the most robust (in terms of not failing) approach is producing combined forecasts. The primary motivation for combining is that there is no one best forecasting method for everything – methods might perform very well in some conditions and fail in others. It is typically not possible to say which of the cases you face in practice. Furthermore, the model selected on one sample might differ from the model chosen for the same sample but with one more observation. Thus there is a model uncertainty (as defined by Chatfield, 1996), and the safer option is to produce forecasts from several models and then combine them to get the final forecast. This way, the potential damage from an inaccurate forecast hopefully will be reduced.

There are many different techniques for combining forecasts. The non-exhaustive list includes:

**Simple average**, which works fine as long as you do not have exceptionally poorly performing methods;**Median**, which produces good combinations when the pool of models is relatively small and might contain those that produce very different forecasts from the others (e.g. explosive trajectories). However, when a big pool of models is considered, the median might ignore vital information and decrease accuracy, as noted by Jose and Winkler (2008). Stock and Watson (2004) conducted an experiment on macroeconomic data, and medians performed poorer than the other approaches (probably because of the high number of forecasting methods), while median-based combination worked well for Petropoulos and Svetunkov (2020), who considered only four forecasting approaches;**Trimmed and/or Winsorized mean**, which drop extreme forecasts, when calculating the mean and, as was shown by Jose and Winkler (2008), work well in case of big pools of models, outperforming medians and simple average;**Weighted mean**, which assigns weights to each forecast and produces a combined forecast based on them. While this approach sounds more reasonable than the others, there is no guarantee that it will work better because the weights need to be estimated and might change with the sample size change or a pool of models. Claeskens et al. (2016) explain why the simple average approach outperforms weighted averages in many cases: it does not require estimation of weights and thus does not introduce as much uncertainty. However, when done smartly, combinations can be beneficial in terms of accuracy, as shown, for example, in Kolassa (2011) and Kourentzes, D. Barrow, et al. (2019).

The forecast combination approach implemented in ADAM is the weighted mean, based on Kolassa (2011), who used AIC weights as proposed by Burnham and Anderson (2004). This approach aims to estimate all models in the pool, calculate information criteria (IC) for each of them (see discussion in Section 13.4 in I. Svetunkov, 2022a) and then calculate weights for each model. Those models with lower ICs will have higher weights, while the poorly performing ones will have higher ones. The only requirement of the approach is for the parameters of models to be estimated via likelihood maximisation (see Section 11.1). It is not important what model is used or what distribution is assumed, as long as the models are initialised (see discussion in Section 11.4) and constructed in the same way and the likelihood is used in the estimation.

When it comes to prediction intervals, the correct way of calculating them for the combination is to consider the joint distribution of all forecasting models in the pool and take quantiles based on that. However, Lichtendahl et al. (2013) showed that a simpler approach of averaging the quantiles works well in practice. This approach implies producing prediction intervals for all the models in the pool and then averaging the obtained values. It is fast and efficient in terms of getting well-calibrated intervals.

In R, `adam()`

function supports the combination of ETS models via `model="CCC"`

or any other combination of letters, as long as the model contains “C” in its name. For example, the function will combine all non-seasonal models if `model="CCN"`

is provided. Consider the following example on Box-Jenkins sales series:

In the code above, the function will estimate all non-seasonal models, extract AICc for each of them and then calculate weights, which we can extract for further analysis:

```
## ANN MAN AAdN MMN AMdN MNN AAN MAdN AMN MMdN
## 0.000 0.013 0.252 0.010 0.512 0.000 0.072 0.031 0.049 0.059
```

As can be seen from the output of weights, the level models ETS(A,N,N) and ETS(M,N,N) were further away from the best model and, as a result, got weights very close to zero.

The fitted values are combined from all models, the residuals are equal to \(e_t = y_t -\hat{y}_t\), where \(\hat{y}_t\) is the combined value. The final forecast together with the prediction interval can be generated via the `forecast()`

function (Figure 15.2):

What the function does, in this case, is produces forecasts and prediction intervals from each model and then uses original weights to combine them. Each model can be extracted and used separately if needed. Here is an example with ETS(A,Ad,N) model from the estimated pool:

As can be seen from the plots in Figures 15.2 and 15.3, due to the highest weight, ETS(A,Ad,N) and ETS(C,C,N) models have produced very similar point forecasts and prediction intervals.

Alternatively, if we do not need to consider all ETS models, we can provide the pool of models, including a model with “C” in its name. Here is an example of how pure additive non seasonal models can be combined:

The main issue with the combined ETS approach is that it is computationally expensive due to the estimation of all models in the pool and can also result in high memory usage. As a result, it is recommended to be smart in deciding which models to include in the pool.

### 15.4.1 Other combination approaches

While `adam()`

supports IC weights combination of ETS models only, it is also possible to combine ARIMA, regression models and models with different distributions in the framework. Given that all models are initialised in the same way and that the likelihoods are calculated using similar principles, the weights can be calculated manually using the formula from Burnham and Anderson (2004):
\[\begin{equation}
w_i = \frac{\exp\left(-\frac{1}{2}\Delta_i\right)}{\sum_{j=1}^n \exp\left(-\frac{1}{2}\Delta_j\right)},
\tag{15.1}
\end{equation}\]
where \(\Delta_i=\mathrm{IC}_i -\min_{i=1}^n \left(\mathrm{IC}_i\right)\) is the information criteria distance from the best performing model, \(\mathrm{IC}_i\) is the value of information criterion of model \(i\) and \(n\) is the number of models in the pool. For example, here how we can combine the best ETS with the best ARIMA and the ETSX(M,M,N) model in the ADAM framework, based on BICc:

```
# Prepare data with explanatory variables
BJsalesData <- cbind(as.data.frame(BJsales),
xregExpander(BJsales.lead,c(-5:5)))
# Apply models
adamPoolBJ <- vector("list",3)
adamPoolBJ[[1]] <- adam(BJsales, "ZZN",
h=10, holdout=TRUE,
ic="BICc")
adamPoolBJ[[2]] <- adam(BJsales, "NNN",
orders=list(ar=3,i=2,ma=3,select=TRUE),
h=10, holdout=TRUE,
ic="BICc")
adamPoolBJ[[3]] <- adam(BJsalesData, "MMN",
h=10, holdout=TRUE,
ic="BICc",
regressors="select")
# Extract BICc values
adamsICs <- sapply(adamPoolBJ,BICc)
# Calculate weights
adamsICWeights <- adamsICs - min(adamsICs)
adamsICWeights[] <- exp(-0.5*adamsICWeights) /
sum(exp(-0.5*adamsICWeights))
names(adamsICWeights) <- c("ETS","ARIMA","ETSX")
round(adamsICWeights,3)
```

```
## ETS ARIMA ETSX
## 0.524 0.424 0.052
```

These weights can then be used for the combination of the fitted values, forecasts and prediction intervals:

```
adamPoolBJForecasts <- vector("list",3)
# Produce forecasts from the three models
for(i in 1:3){
adamPoolBJForecasts[[i]] <- forecast(adamPoolBJ[[i]],
h=10, interval="pred")
}
# Produce combined conditional means and prediction intervals
finalForecast <- cbind(sapply(adamPoolBJForecasts,
"[[","mean") %*% adamsICWeights,
sapply(adamPoolBJForecasts,
"[[","lower") %*% adamsICWeights,
sapply(adamPoolBJForecasts,
"[[","upper") %*% adamsICWeights)
# Give the appropriate names
colnames(finalForecast) <- c("Mean", "Lower bound (2.5%)",
"Upper bound (97.5%)")
# Transform the table in the ts format (for convenience)
finalForecast <- ts(finalForecast,
start=start(adamPoolBJForecasts[[i]]$mean))
finalForecast
```

```
## Time Series:
## Start = 141
## End = 150
## Frequency = 1
## Mean Lower bound (2.5%) Upper bound (97.5%)
## 141 257.6468 254.8652 260.4381
## 142 257.6975 253.3268 262.0589
## 143 257.7544 251.8519 263.6948
## 144 257.8022 250.3469 265.2919
## 145 257.8509 248.8261 266.9842
## 146 257.9014 247.2107 268.6252
## 147 257.9537 245.7223 270.3505
## 148 257.9849 244.0379 271.9369
## 149 258.0267 242.4063 273.7741
## 150 258.0741 240.7081 275.5665
```

In order to see how the forecast looks like, we can plot it via `graphmaker()`

function from `greybox`

:

```
graphmaker(BJsales, finalForecast[,1],
lower=finalForecast[,2], upper=finalForecast[,3],
level=0.95)
```

Figure 15.4 demonstrates the slightly increasing trajectory with expanding prediction interval. The point forecast (conditional mean) corresponds to the trajectory observed on the last several observations, just before the forecast origin. The future values are inside the prediction interval, so overall, this can be considered as a reasonable forecast.

### References

• Burnham, K.P., Anderson, D.R., 2004. Model Selection and Multimodel Inference.. Springer New York. https://doi.org/10.1007/b97636

• Chatfield, C., 1996. Model uncertainty and forecast accuracy. Journal of Forecasting. 15, 495–508. https://doi.org/10.1002/(SICI)1099-131X(199612)15:7<495::AID-FOR640>3.3.CO;2-F

• Claeskens, G., Magnus, J.R., Vasnev, A.L., Wang, W., 2016. The forecast combination puzzle: A simple theoretical explanation. International Journal of Forecasting. 32, 754–762. https://doi.org/10.1016/j.ijforecast.2015.12.005

• Jose, V.R.R., Winkler, R.L., 2008. Simple robust averages of forecasts: Some empirical results. International Journal of Forecasting. 24, 163–169. https://doi.org/10.1016/j.ijforecast.2007.06.001

• Kolassa, S., 2011. Combining exponential smoothing forecasts using Akaike weights. International Journal of Forecasting. 27, 238–251. https://doi.org/10.1016/j.ijforecast.2010.04.006

• Kourentzes, N., Barrow, D., Petropoulos, F., 2019. Another look at forecast selection and combination: Evidence from forecast pooling. International Journal of Production Economics. 209, 226–235. https://doi.org/10.1016/j.ijpe.2018.05.019

• Lichtendahl, K.C., Grushka-Cockayne, Y., Winkler, R.L., 2013. Is It Better to Average Probabilities or Quantiles? Management Science. 59, 1594–1611. https://doi.org/10.1287/mnsc.1120.1667

• Petropoulos, F., Svetunkov, I., 2020. A simple combination of univariate models. International Journal of Forecasting. 36, 110–115. https://doi.org/10.1016/j.ijforecast.2019.01.006

• Stock, J.H., Watson, M.W., 2004. Combination forecasts of output growth in a seven-country data set. Journal of Forecasting. 23, 405–430. https://doi.org/10.1002/for.928

• Svetunkov, I., 2022a. Statistics for business analytics. https://openforecast.org/sba/ (version: 31.03.2022)