Time Series


Overview

We will primarily deal with the problem of forecasting. We consider the single-variable case, although the following can be easily generalised to multiple variables.
We have training data , and we wish to be able to predict and so on. This is significantly different from our standard supervised learning case, and is closer to the self-supervised case where we have to learn the data distribution—the main difference being that our data is not i.i.d., but correlated with other datapoints over time.
Here our models tend to consist of linear operations, combined with "white noise"/"innovations" terms. Here we assume that this noise is Gaussian, with mean zero and some fixed variance: .
When considering our models we treat this white noise as known—it is simply whatever value we need to close our gap to the linear model. When doing prediction for timestep , we can effectively ignore the noise term as it has expectation zero and we don't know what value will be sampled.

Key Models

Moving Average Model

Notation: MA(q)
Explanation:
Each observation is represented as a sum of the mean of the overall series, its innovation, and a linear combination of the previous innovations.
Model:

Autoregressive Model

Notation: AR(p)
Explanation:
Each observation is represented as a sum of some fixed constant, its innovation, and a linear combination of the previous observations.
Model:

ARMA Model

Notation: ARMA(p, q)
Explanation:
Sum of AR and MA terms to model timeseries ( term "absorbed" into ).
Model:

ARIMA Model

Notation: ARIMA(p, d, q)
Explanation:
ARMA with an added "integrated" term, which replaces the autoregressive terms with -order differences to help de-trend the data.
Note that logging the data first can also help remove exponential trends.
Model:

SARIMA Model

Notation: SARIMA(p, d, q, P, D, Q, m)
Explanation:
Like ARIMA, but includes second set of parameters to model seasonal trend. The parameter determines the number of timesteps for the period.
Note that more simple seasonal differencing methods can also be applied.

Model Fitting

Information on Wikipedia for this appears to vary slightly, so I'm not certain about what exactly is the best approach—hopefully this explanation accounts for that uncertainty.

Coefficient Fitting

This involves fitting the and values. Information on this is inconsistent. For pure MA models it suggests that as the are hard to calculate, non-linear methods must be used. However, in all other cases it suggests that least-squares type approaches can be used.

Order Fitting

This involves fitting the p, d, q variables etc. There are two main approaches to this:
AIC/BIC:
The Akaike and Bayesian information criterion gives us a way of "scoring" a model on the training data by combining likelihood and model complexity. This balances over/under-fitting. They are defined as:
Where is the number of parameters, is the size of the dataset, and is the likelihood of the model on the dataset.
(Partial) Autocorrelation:
Autocorrelation is closely linked to moving-average models. MA(q) is designed so that
  • For a true MA(q) process, the autocorrelation is 0 at lag > q.
  • When modelling a timeseries as MA(q), we set the value of q to equal the point at which all autocorrelations onwards are insignificantly different from zero.
  • We can tell this by plotting the autocorrelation function (ACF; see below)
Fortunately, we have an equivalent for AR(p) models, which are designed so that the partial autocorrelation is 0 at lag > p. We find the ideal value of p in just the same way as q, using a plot of the partial autocorrelation function (PACF).

ACF/PACF Plots

Assume a timeseries data such as the temperature dataset presented here (source for this section).
Initial plot of minimum daily temperature.
Initial plot of minimum daily temperature.
First we will consider the autocorrelation function plot (or correlogram). The correlation between two vectors is their normalised inner product, equal to the cosine angle between them. The ACF plot record this value (y-axis) for the time series compared with increasing lag values (x-axis) of itself. The autocorrelation at lag 0 is therefore 1, and in this case then changes cyclically because of the cyclic nature of the original data.
Autocorrelation of the daily temperature plot.
Autocorrelation of the daily temperature plot.
Same as previous plot, but zoomed in to 50 on the x-axis.
Same as previous plot, but zoomed in to 50 on the x-axis.
For the ACF plot we also record a blue cone representing the confidence interval. Only values outside of this cone are statistically significantly different to 0. Therefore, in this case the ideal value of is the last value on the x-axis that is outside of this cone.
 
The partial autocorrelation function calculates the correlation between the data and a lagged version of the data (like ACF), but with the relationships with intermediate lags removed. This means that the PACF represents just the effect that one particular lag has on the correlation. This is why it tends to drop so much faster than the ACF.
Partial autocorrelation of the daily temperature plot.
Partial autocorrelation of the daily temperature plot.
Once again, we can use the confidence interval to find our ideal value.

Testing Model Properties

Trend

There are two tests that can be used here:
Dickey-Fuller:
  • Null hypothesis: model is not stationary (has a unit root)
  • Alternative hypothesis: model is stationary
KPSS: other way round

Residual Independence

Ljung-Box:
  • Null hypothesis: residuals independently distributed
  • Alternative hypothesis: residuals correlated