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How do we describe patterns in data over time and forecast future values?

Analyse time series using smoothing and trend lines, then forecast future values.

Trend, seasonal and irregular components, moving-average smoothing, seasonal indices, and trend-line forecasting in TCE Mathematics Applications.

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What this dot point is asking

A time series is data recorded in time order, such as monthly sales or quarterly rainfall. The goal is to see through the wobble and describe the underlying movement, then project it forward.

Smoothing with moving averages

A moving average replaces each value with the average of itself and its neighbours, which smooths out short-term fluctuations and reveals the trend. The number of points averaged is the order. For an odd order (e.g. 3 or 5), the smoothed value lines up directly with a data point. For an even order (e.g. 4 for quarterly data), you must centre the average so it lines up with a time point.

Seasonal indices

A seasonal index measures how a particular season compares with the average. An index of 1.201.20 means that season runs 20%20\% above the average; 0.850.85 means 15%15\% below. For data with nn seasons, the indices must add to nn (for example, four quarterly indices sum to 44, and average to 11).

Deseasonalising strips out the seasonal pattern so the underlying trend is clear. You fit a trend line to the deseasonalised data, forecast along it, then reseasonalise by multiplying back by the relevant index.

Trend-line forecasting

Once you have a trend line (often a least-squares line fitted to time tt on the horizontal axis), substitute the future time value to forecast. As with regression, forecasting far beyond the data is extrapolation and grows less reliable the further out you go.

Calculating seasonal indices from data

To find seasonal indices yourself, average each season's values, divide each seasonal average by the overall average of all the data, and the results are the indices. They must sum to the number of seasons (4 for quarterly, 12 for monthly), so if they do not, scale them: multiply each by the number of seasons divided by their current sum. This forces the average index to 1, which is the property that makes deseasonalising and reseasonalising consistent.

A complete forecast answer states the trend equation, shows the deseasonalising and reseasonalising steps where seasons apply, checks that seasonal indices sum to the number of seasons, and comments on reliability if the forecast reaches well beyond the data.

Exam-style practice questions

Practice questions written in the style of TASC exam questions on this dot point, with worked answer explainers. The year tag is the paper they imitate, not the source.

TCE 20243 marksA graph shows actual and deseasonalised power costs for a household, with a regression line for the deseasonalised data. a) What long-term trend does the regression line suggest? b) i. To convert a deseasonalised prediction to actual, what is the final step? ii. When would a smoothing process such as 3- or 5-point averaging be used instead of deseasonalising?
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a) (1 mark) The regression line of the deseasonalised data has a slight positive slope, so the long-term trend is a small steady increase in power costs (accept a comment that there is little or no increase, since the rise is very gradual).

b) i. (1 mark) Multiply the deseasonalised prediction by the seasonal index for that season: actual == deseasonalised ×\times index. This puts the seasonal variation back in (reseasonalise using D=AID = \frac{A}{I} rearranged to A=D×IA = D \times I).

b) ii. (1 mark) Moving-average smoothing is used when the data has no clear repeating seasonal pattern (or the period is unknown or irregular), so seasonal indices cannot be calculated. Smoothing just removes random fluctuation to reveal the underlying trend.

TCE 20243 marksA table shows rainfall on Tasmania's east coast in 2023. a) Complete the 3-point moving-average row (two values missing). b) Add your values to the graph. c) The line of best fit for the smoothed data is R=0.006M+30.1R = 0.006M + 30.1, where MM is months since December 2022. Add (2,30.1)(2, 30.1) and (11,30.2)(11, 30.2) and draw the line.
Show worked answer →

a) (1 mark) A 3-point moving average replaces each value with the mean of it and its two neighbours. The January value cannot be found (no value before it), so the first computed average is for February: 3+54+193=25\frac{3 + 54 + 19}{3} = 25 (given). The missing entries are found the same way, for example the November average =62+22+293=38= \frac{62 + 22 + 29}{3} = 38 (round to whole numbers to match the table).

b) (1 mark) Plot the two computed averages at their correct months, joining the smoothed series.

c) (1 mark) Plot (2,30.1)(2, 30.1) and (11,30.2)(11, 30.2), rule a straight line through them and extend it. The almost flat line shows a very slight upward trend in smoothed rainfall.

TCE 20233 marksA table shows quarterly power costs, with deseasonalising almost complete. The regression line for the deseasonalised data is D=1.0459x+516.33D = 1.0459x + 516.33 where xx is the season number. Predict the actual power cost for Spring 2024 (Spring index 0.9520.952).
Show worked answer →

(3 marks) Work in three steps.

  1. Find the season number xx for Spring 2024. The data runs from Summer 2021 (x=1x = 1), so Spring 2024 is x=16x = 16.

  2. Substitute into the trend line for the deseasonalised prediction: D=1.0459(16)+516.33=16.73+516.33=533.07D = 1.0459(16) + 516.33 = 16.73 + 516.33 = 533.07.

  3. Reseasonalise by multiplying by the Spring index: actual =533.07×0.952=$507.48= 533.07 \times 0.952 = \$507.48 (about $507\$507). The final answer must be the actual cost in dollars, not the deseasonalised value.

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