YCC The Beaufort scale

Sir Francis Beaufort

A wind force scale devised in 1805 by (then) Commander Francis Beaufort of the British Navy for observing and classifying wind force at sea. Originally based on the effect of the wind on a full-rigged man-of-war, in 1838 it became mandatory for log entries in all ships in the Royal Navy. Altered to include observations of the state of the sea and phenomena on land as criteria, it was adopted in 1874 by the International Meteorological Committee for international use in weather telegraphy.

The Beaufort scale as originally drawn up made no reference to the speed of the wind, and various attempts, particularly during the 20th century, have been made to correlate the two. An attempt made in 1912 by the International Commission for Weather Telegraphers was interrupted by World War I. In 1921 G.C. Simpson was asked to formulate equivalents, which were accepted in 1926 by the Committee. In June 1939 the International Meteorological Committee adopted a table of values referring to an anemometer at a height of 6 metres (20 feet). This was not immediately adopted by the official weather services of the United States and Great Britain, which used the earlier scale referring to an anemometer at an elevation of 11 metres (36 feet). The Beaufort force numbers 13 to 17 were added by the U.S. Weather Bureau in 1955.

The scale is now rarely used by professional meteorologists, having been largely replaced by more objective methods of determining wind speeds.

Beaufort number name of number wind speed (knots, km/h, m/sec) description of sea surface sea disturbance average wave height
0 calm < 1 knots, < 0.5 m/sec sea like a mirror 0 -
1 light air 1-3 knots, 0.5-1.5 m/sec ripples with appearance of scales are formed, without foam crests 0 -
2 light breeze 4-6 knots, 2.1-3.1 m/sec small wavelets still short but more pronounced; crests have a glassy appearance but do not break 1 0-20 cm
3 gentle breeze 7-10 knots, 3.6-5.1 m/sec large wavelets; crests begin to break; foam of glassy appearance; perhaps scattered white horses 2 30-60 cm
4 moderate breeze 11-16 knots, 5.7-8.2 m/sec small waves becoming longer; fairly frequent white horses 3 1 m
5 fresh breeze 17-21 knots, 8.7-11 m/sec moderate waves taking a more pronounced long form; many white horses are formed; chance of some spray 4 1.8 m
6 strong breeze 22-27 knots, 11-14 m/sec large waves begin to form; the white foam crests are more extensive everywhere; probably some spray 5 3 m
7 moderate gale (or near gale) 28-33 knots, 14-17 m/sec sea heaps up and white foam from breaking waves begins to be blown in streaks along the direction of the wind; spindrift begins to be seen 6 4 m
8 fresh gale (or gale) 34-40 knots, 17-21 m/sec moderately high waves of greater length; edges of crests break into spindrift; foam is blown in well-marked streaks along the direction of the wind 6 5.5 m
9 strong gale 41-47 knots, 21-24 m/sec high waves; dense streaks of foam along the direction of the wind; sea begins to roll; spray affects visibility 6 7 m
10 whole gale (or storm) 48-55 knots, 25-28 m/sec very high waves with long overhanging crests; resulting foam in great patches is blown in dense white streaks along the direction of the wind; on the whole the surface of the sea takes on a white appearance; rolling of the sea becomes heavy; visibility affected 7 9 m
11 storm (or violent storm) 56-63 knots, 29-32 m/sec exceptionally high waves; small- and medium-sized ships might be for a long time lost to view behind the waves; sea is covered with long white patches of foam; everywhere the edges of the wave crests are blown into foam; visibility affected 8 11 m
12-17 hurricane 64 knots, 33 m/sec and above the air is filled with foam and spray; sea is completely white with driving spray; visibility very seriously affected 9 14 m and more

Conversions computed taking 1852 m per nautical mile. The Beaufort scale does not bear a simple relation to wind speed, as shown by the conversion graphs below. The conversion does not even have a monotonously increasing step size. A power law (with power 1.75 for knots and 1.4 for m/sec, curved dashed lines) provides a valid approximation for the m/sec scale, but this is hardly practical. Linear approximations (straight dashed lines) do not fit more than 2-3 steps of the scale.

(Figures in PS format.)


Adapted from the EB. Last modified on 19/11/2001.