The Sunday Telegraph

‘Average’ conditions? They are anything but

Typical rainfall and sunshine means one thing to meteorolog­ists and another to readers

- Comment by PHILIP EDEN, past vice-president of theroyal Meteorolog­ical Society

“AVERAGE” IS one of the most sloppily used words in weather reports in the news media.

I, too, have to plead guilty to being less than rigorous in my own use of the word.

One of the difficulti­es is that the correct use of statistica­l terms might keep a mathematic­ian happy but it would leave most other readers cold. It can also get very repetitive.

Apart from its general meaning of “typical”, average is also a synonym for the arithmetic mean. Often shortened to “mean”, this is what you get when you add up a set of measuremen­ts and divide by the number of measuremen­ts. For instance, to discover the mean maximum temperatur­e for December 2011, one adds together each daily maximum during the month and divides by 31.

Another word which can be misleading is “normal”. Too-clever-by-half correspond­ents upbraid me for writing loosely about “normal rainfall” and “normal sunshine”, suggesting – usually with a touch too much sarcasm – that I might like to write a column about abnormal sunshine.

There are, though, secondary meanings: in the scientific study of climate, “normal” refers specifical­ly to the mean value over a 30year period of any meteorolog­ical element at a particular site.

The arithmetic mean provides a good summary of a set of measuremen­ts when they cluster evenly around a particular value. Unfortunat­ely, not all meteorolog­ical elements do this. The distributi­on may be skewed – with a cluster towards one extremity and stragglers towards the other, or there may be more than one cluster, and so on. When this happens statistici­ans may look at the median and the mode as well as the mean. The median is defined as that value which has half of the measuremen­ts above it and half below; the mode is the value which occurs most frequently in the set of measuremen­ts.

Let us look at an example. The number of days with a snow-cover in the Januaries of the 1960s in Bedfordshi­re were, respective­ly, 3, 0, 9, 31, 2, 3, 10, 0, 13, and 0. For this strongly skewed set of observatio­ns the mean is 7.1, the median is 3, and the mode is 0. Each of these figures shows up a different characteri­stic of the set, and taken together they tell us a great deal more than does the mean itself.

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