## What Is the Holt-Winters Method?

Holt-Winters is a model of time series behavior. Forecasting always requires a model, and Holt-Winters is a way to model three aspects of the time series: a typical value (average), a slope (trend) over time, and a cyclical repeating pattern (seasonality). Time series anomaly detection is a complicated problem with plenty of practical methods. It’s easy to get lost in all of the topics it encompasses. Learning them is certainly an issue, but implementing them is often more complicated. A key element of anomaly detection is forecasting—taking what you know about a time series, either based on a model or its history, and making decisions about values that arrive later. You know how to do this already. Imagine someone asked you to forecast the prices for a certain stock, or the local temperature over the next few days. You could draw out your prediction, and chances are it’s a pretty good one. Your brain works amazingly well for problems like this, and our challenge is to try to get computers to do the same. If you take an introductory course on time series, you’ll learn how to forecast by fitting a model to some sample data, and then using the model to predict future values. In practice, especially when monitoring systems, this approach doesn’t work well, if at all! Real systems rarely fit mathematical models. There’s an alternative. You can do something a lot simpler with exponential smoothing.## Holt-Winters Triple Exponential Smoothing Formula Explained

The Holt-Winters method uses exponential smoothing to encode lots of values from the past and use them to predict “typical” values for the present and future. Exponential smoothing refers to the use of an exponentially weighted moving average (EWMA) to “smooth” a time series. If you have some time series*x*, you can define a new time series

_{t}*s*

_{t}_{ }that’s a smoothed version of

*x*.

_{t}*s _{t}*=

*αx*+(1−

_{t}*α*)

*s*−1

_{t}*xt*, and another for its

*slope*. The terms

*level*and

*trend*are also used.

*s _{t}*=

*αx*+(1−

_{t}*α*)(

*s*−1+

_{t}*b*−1)

_{t}*b _{t}*=

*β*(

*s*−

_{t}*s*−1)+(1−

_{t}*β*)

*b*−1

_{t}*m*time steps in the future. The formula for the

*m*-step-ahead forecast,

*F*

_{t}_{+m}, is:

*F _{t}*

_{+m}=

*s*+

_{t}*mb*

_{t}*L*, which depends on the period of the seasonality and has to be known in advance.The three aspects of the time series behavior—value, trend, and seasonality—are expressed as three types of exponential smoothing, so Holt-Winters is called triple exponential smoothing. The model predicts a current or future value by computing the combined effects of these three influences. The model requires several parameters: one for each smoothing (ɑ, β, γ), the length of a season, and the number of periods in a season.

## Holt-Winters Forecasting Example

The hardest parts of Holt-Winters forecasting are understanding how the model works and choosing good parameters. To tackle the first, we’ll walk through an example model by doing Holt-Winters “by hand.” The usual way to explain Holt-Winters is by showing a bunch of complicated equations with Greek letters and subscripts. We’ll skip the math and show how it works, which is a lot simpler. We’re going to be working with this time series:*relative to the average*of those five points? The average of (0+1+0+0+0)/5 is 0.2, which we’ll draw on the plot as a horizontal line:Holt-Winters has a trend component. If we set its parameter to zero, Holt-Winters ignores the trend (slope), so the model simplifies. Now, it’s just a bunch of values relative to the average. In our plot, the values relative to 0.2 are [-0.2, 0.8, -0.2, -0.2, -0.2]. If we did Holt-Winters without trend, that’s the type of model we’d build. Here’s what the Holt-Winters function in R gives, with some annotations in blue I added manually:Forecasting with trend is just an enhancement of this. Instead of using a fixed average as the foundation, you have to incorporate the slope of the line. Here’s a model with a trend:

## What Is Seasonality in Forecasting?

Seasonality refers to a periodic pattern or a fixed length of time containing the full repetition. However, seasonality can be confusing. You might think your data repeats daily (there’s a peak at 2 p.m. every day), but if the weekend has different behavior (there’s no peak at 2 p.m. on Sunday) then your season is really a week, not a day. Within the season, there are periods, which is the granularity of prediction. If you want to model a value for every hour of every day within a week, your season is 168 hours long and your period is 1 hour. You already know, by definition, the example series repeats itself every five points, i.e., the season is five periods. What if you didn’t know what the season is for a time series? How can you figure it out? What are the consequences of being wrong? The right seasonality is crucial to Holt-Winters forecasting. To illustrate this, let’s see what happens when you use a season of six periods, one greater than the actual season of five periods: The forecast, which is the red line in the chart, becomes less accurate and turns into garbage. To get good results, you need to give the model good parameters. This is the second challenge with Holt-Winters forecasting.## Determining Optimal Parameters for Holt-Winters Formula Calculations

Picking the seasonality is a hard problem. General-purpose forecasting is hard because it has to be ready to use on any dataset, which might have any combination of values, trend, and seasonality. It might not even have some of those components. These are usually unknowns unless you’re manually inspecting the data and customizing the model for it. At SolarWinds, we needed forecasting functionality that just works, without any assumptions or knowledge of the data’s characteristics. There are various approaches to this: machine learning, Fourier analysis, and so on. Our solution to this problem is to try lots of different combinations of things, using techniques like Nelder-Mead optimization to pick the winners. This takes advantage of computers being fast at simple things, so we formulate the problem simply: can I quantify how good a forecast is, and can I compare forecasts? Then we try different combinations of parameters and see what wins. Let’s quantify how good a forecast is. The last forecast was bad, but*how bad?*The usual way to quantify the accuracy of a forecast is to calculate the differences between the predicted values and the actual values. The blue arrows in the following chart represent how far off the prediction was from the actual value. To quantify overall accuracy, you can combine these differences into a single value by taking the average or the sum of squared values. The result is a value that’s smaller if the forecast is better, and larger if the forecast is worse. This gives you a good way to compare forecast results. Our forecasting code tries lots of combinations (lots!) with different parameters and picks the ones that generate the lowest combined error score. To illustrate this, here are a bunch of forecasts on the same time series, trying out different frequencies.

## Holt-Winters Forecasting Method for Database Anomaly Detection

Holt-Winters forecasting is surprisingly powerful despite its simplicity. It can handle lots of complicated seasonal patterns by simply finding the central value, then adding in the effects of slope and seasonality. The trick is giving it the right parameters. This is a hard problem, but we’ve found numerical optimization can pick good values quickly. This solution is simple to build and understand, which is valuable for our purposes. If you’re interested in exploring further, here are some other resources:- https://www.otexts.org/fpp/7/5
- https://grisha.org/blog/2016/01/29/triple-exponential-smoothing-forecasting/
- http://www.itl.nist.gov/div898/handbook/pmc/section4/pmc435.htm