Lewis Fry Richardson served as a driver for the Friends' Ambulance Unit in the Champagne district of France from September 1916 until the Unit was dissolved in January 1919 following the cessation of hostilities. For much of this time he worked near the front line, and during the Battle of Champagne in April 1917 he came under heavy shelling (Ashford, 1985). It is a source of wonder that in such appallingly inhuman conditions he had the buoyancy of spirit to carry out one of the most remarkable and prodigious calculational feats ever accomplished. During the intervals between transporting wounded soldiers back from the front he worked out by manual computation the changes in the pressure and wind at two points, starting from an analysis of the condition of the atmosphere at 0700 UTC on 20 May 1910. Richardson described his method of solving the equations of atmospheric motion and his sample forecast in what has become the most famous book in meteorology, his Weather Prediction by Numerical Process (Richardson, 1922). The unrealistic values which he obtained are a result of inadequacies and imbalances in the initial data, and do not reflect any flaw in his method, which is essentially the way numerical forecasts are produced today.
How long did it take Richardson to make his forecast? And how many people would be required to put the method to practical use? The answers to these two questions are contained in § 11/2 of his book, but are expressed in a manner which has led to some confusion. On p. 219 under the heading The Speed and Organization of Computing Richardson wrote
Now to the question of the resources required to realize Richardson's dream of practical forecasting. Quoting again from p. 219 of the book:
So where did Richardson come by the figure of 3200 chequers to cover the globe? The error is inescapable but is not, I believe, a numerical slip. Richardson intimated that the weather in the tropics was sufficiently steady for variations to be neglected. But in such a case the global forecasting problem falls neatly into two parts and it is natural to consider each hemisphere separately. The Northern hemisphere can be covered by 3200 pairs of columns. Assuming with Richardson that the values at 1200 pairs may be prescribed and assigning 32 individuals to each of the remaining pairs, one finds that 32×2000 = 64,000 souls are needed to race the weather for the extra-tropical Northern hemisphere.
If this is what Richardson intended, his uncharacteristic error was not an arithmetical howler but a lapse of expositional precision. For his staggering figure of 64,000 is clearly stated to refer to the whole globe. Later in the paragraph he speaks of a forecast-factory for the whole globe (in fact, the word globe occurs five times on p. 219). In his wonderful fantasy of a theatre full of computers, the tropics in the upper circle are treated on an equal footing with the temperate and frigid zones. Given that Richardson's assumption of constancy of tropical weather was over-optimistic, a full complement of 32 computers for each pair of columns in his forecast-factory for the whole globe would have provided work for 204,800 people.
Even this vast multitude could compute the weather only as fast as it was evolving. To obtain useful and timely predictions, the calculations would need to go several times faster than the atmosphere. Allowing for a speed-up factor of five, the establishment of a practical forecast-factory would have reduced the ranks of the unemployed by over a million.
Ashford, Oliver M., 1985: Prophet-or Professor? The Life and Work of Lewis Fry Richardson. Adam Hilger, Bristol and Boston, xiv+304 pp.
Richardson, Lewis F., 1922: Weather Prediction by Numerical Process. Cambridge University Press, xii+236 pp. Reprinted by Dover Publications, New York, 1965, with a New Introduction by Sydney Chapman, xvi+236 pp.