About this page
A light-hearted look at various Beaufort scales - but with a sideways look at the serious and realistic aspects.
Preamble
The Beaufort Scale, used throughout the marine world, has developed over many years. How the scale is defined depends, to some extent, on the user. This page puts Beaufort into historical context and shows how the ideas have different applications.
Related pages
- * How the Beaufort scale came into being and why it is still a useful tool
- Is it better to measure or estimate wind strength?
- Why do we need a Beaufort Scale?
- Visibility measurement at sea
- Single Observer Forecasting.
On this page
- Pre Beaufort
- Beaufort's Original
- Evolution of the scale
- Beaufort's Final
- Beaufort Today
- Dinghy Version
- Coarse Sailors
- Cruising version
- Beaufort Philosophy
- Self calibration
The history pre Beaufort.
In 1704, after he had witnessed the Great Storm of 1703, Daniel Defoe suggested a scale of winds comprising 11 points and using words normally used in the English language. Even before that, certainly during the late 17th century sailors were using a fairly standard set of names to describe winds. In a book written in 1697 after a circum-navigation, it is clear that William Dampier, the Privateer, was using the same general words to describe winds.
Defoe's Scale of winds, 1704 | |
0 |
stark calm |
1 |
calm weather |
2 |
little wind |
3 |
a fine breeze |
4 |
a small gale |
5 |
a fresh gale |
6 |
a top sail gale |
7 |
blows fresh |
8 |
a hard gale of wind |
9 |
a fret of wind |
10 |
a storm |
11 |
a tempest |
In 1759, John Smeaton, a British civil engineer designed an early anemometer as part of his study into windmill design. From readings with this and his experiments he defined an 8 point scale of winds. This had descriptions in terms of movement of leaves, branches and trees as well as the speed of rotation of a windmill. Some 20 years later, Alexander Dalrymple, Hydrographer of the Honourable East India Company, with which Beaufort had served his sea going apprenticeship, produced a scale of winds for use by company captains. A very similar words were used by Archibald Menzies on Vancouver's circumnavigation from. 1791 to 1795.
In 1801, Colonel Capper, also of the Honourable East India Company, calibrated a list of he common terms in terms of miles per hour and feet per second. Apart from Smeaton and Capper, nobody else seems to have tried to define the terms used in ship's logs to describe wind. Even Dalrymple seems to have taken it for granted that his captains would all work to a c common, but unwritten standard. When, on 13th January, 1806, Commander Francis Beaufort of His Majesty’s Sloop Woolwich wrote in his logbook that he would use a 0 - 13 point scale to which he gave descriptive names, he was only following the custom of the sea at that time. Not surprisingly, Beaufort was highly influenced by Dalrymple and, in his 1806 scale he used very similar descriptive names but added an extra, fifth, point which he called a “Moderate Breeze". It is clear that Beaufort was being evolutionary rather than revolutionary.
The evolution of the Beaufort scale
The real and very significant contribution of Beaufort came in 1810 when, now as captain of His Majesty’s Sloop Blossom, he defined, in his logbook, the sea going characteristics of each point on his scale. His definitions are unlikely to be original in that he was, no doubt, reflecting collective marine experience of the time. Beaufort showed great foresight in recognising the need for a standard and uniformly applied wind scale. In this respect, his scale has been and continues to be of great value to both operational meteorology and, importantly in these days of climate change concerns, also to climatology.
Following discussion with Captain Fitzroy of HMS Beagle, and others, Beaufort refined the scale, now the 0 to 12 points version that rightly bears his name. In 1831 he submitted it to his seniors for official approval and in 1838 it was accepted by their Lordships of the Admiralty as the definitive scale to be used by all ships of the Royal Navy (Table 2). In 1854, Fitzroy, another great sailor, navigator and innovator, formed, and became the first Secretary of, the Meteorological Department of the Board of Trade, later the Meteorological Office.
0 |
Calm | ||
1 |
Light air |
Or just sufficient to give steerage way | |
2 |
Light breeze |
Or that in which a man-of-war with all sail set and clean full would go in smooth water from -- |
1 to 2 knots |
3 |
Gentle breeze |
3 to 4 knots | |
4 |
Moderate breeze |
4 to 5 knots | |
5 |
Fresh breeze |
Or that in which a well conditioned man-of-war could just carry, in chase, full and by -- |
Royals etc |
6 |
Strong breeze |
Single reefed topsails and top-gallant sails | |
7 |
Moderate gale |
Double-reefed topsails, jib etc | |
8 |
Fresh gale |
Treble reefed topsails etc | |
9 |
Strong gale |
Close reefed topsails and courses | |
10 |
Whole gale |
Or that in which she could scarcely bear close reefed main topsail and reefed fore sail | |
11 |
Storm |
Or that which would reduce her to storm staysails | |
12 |
Hurricane |
Or that which no canvas could withstand |
Each force from 1 - 4 was described by Beaufort in terms of the speed of a man-of-war under full sail on her fastest point of sailing – “clean full.” This would correspond to the broad reach of a modern sailing yacht with the wind some 120 degrees off the bow. For forces 5 to 11 he used descriptions relating to the amount of sail that she could carry when “in chase, full and by”. That meant when the captain was carrying as much sail as possible in order to catch the enemy but without masts or spars being carried away. Clearly, this was a matter of very fine judgement; carry too little sail and the enemy would escape; too much sail and the same result would ensue. Neither would enhance the reputation or career prospects of the captain.
For a modern yacht, the equivalent of “full and by” would, most probably, be a fine reach or a close hauled course with the wind some 40 degrees off the bow. A square rigged vessel of the time might manage up to between 60 and 70 degrees off the bow. Even a sloop, like those commanded by Beaufort could do little better. For a modern sailing yacht, as for a ship of Beaufort’s time, the amount of sail carried has a critical effect on the performance of the boat.
This is most evident when racing when there is, again, a fine balance between carrying so much sail that the yacht is heeling too much for optimum speed, or even suffers gear failure, and so little that opponents sail a faster course to the next mark of the course. Neither wins races.
The strongest wind, a force 12, was defined by the immortal phrase “That which no canvas could withstand.” In survival conditions, Beaufort saw no need to differentiate between higher strengths of wind. Modern versions of the Beaufort scale have higher numbers but, although important meteorologically, these are as irrelevant to the skipper of a sailing vessel now as they would have been 200 years ago. For a small vessel, any hurricane represents survival conditions. Even for a large ship, a force 12 or higher is extremely hazardous. The single word “hurricane” is quite sufficient in any forecast to draw attention to the severity of the expected conditions.
Beaufort defined his scale for a man of war and the definitions would not necessarily suit every ship of the time. However. experienced sailors would recognise the terms used and be able to give a wind force in a reasonably consistent manner.
Beaufort Today
For reasons outlined on the page Why Do We Need The Beaufort Scale? the observing of wind by the Officer of the Watch on board a merchant ship is usually by reference to the state of the sea. The current Beaufort scale, and a land version follows. The land version is to help observers who do not have properly sited anemometers to report the wind force.
Current International Definitions on Sea and on Land for the Beaufort Scale | ||||
Force |
Knots |
Brief name |
For use at sea |
For use on land |
0 |
< 1 |
Calm |
Sea like a mirror |
Smoke rises vertically |
1 |
1-3 |
Light air |
Ripples with the appearance of scales are formed, but without foam crests |
Direction of wind shown by smoke drift but not by wind vanes |
2 |
4-6 |
Light breeze |
Small wavelets, still short but more pronounced. Crests have a glassy appearance and do not break. |
Wind felt on ace, leaves rustle, ordinary wind vanes moved by wind |
3 |
7-10 |
Gentle breeze |
Large wavelets. Crests begin to break. Foam of glassy appearance. Perhaps scattered white horses |
Leaves and small twigs in constant motion, wind extends light flags. |
4 |
11-16 |
Moderate breeze |
Small waves, becoming longer, fairly frequent white horses |
Wind raises dust and loose paper, small branches move. |
5 |
17-21 |
Fresh breeze |
Moderate waves, taking a more pronounced form, many white horses are formed. Chance of some spray. |
Small trees in leaf start to sway, crested wavelets on inland waters. |
6 |
22-27 |
Strong breeze |
Large waves begin to form, the white foam crests are more extensive everywhere. Probably some spray |
Large branches in motion, whistling in telegraph wires, umbrellas used with difficulty. |
7 |
28-33 |
Near gale |
Sea heaps up and white foam from breaking waves begins to be blown in streaks along the direction of the wind. |
Whole trees in motion, inconvenient to walk against the wind. |
8 |
34-40 |
Gale... |
Moderately high waves of greater length; edges of crests begin to break into spindrift. The foam is blown in well marked streaks along the direction of the wind |
Twigs break from trees, difficult to walk. |
9 |
41-47 |
Strong gale |
High waves. Dense streaks of foam along the direction of the wind. Crests of waves begin to topple, tumble and roll over. Spray may affect visibility. |
Slight structural damage occurs, chimney pots and slates removed. |
10 |
48-55 |
Storm |
Very high waves with long over hanging crests. The 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. The "tumbling" of the sea becomes heavy and shock-like.. Visibility affected. |
Trees uprooted, considerable structural damage occurs |
11 |
56-63 |
Violent storm |
Exceptionally high waves (small and medium sized ships might be lost for a time behind the waves). The sea is completely covered with long white patches of foam lying along the direction of the wind. Everywhere, the edges of the waves are blown into froth. Visibility affected. |
Widespread damage |
12 |
64 |
Hurricane |
The air is filled with foam and spray. sea completely white with driving spray, visibility very seriously affected. |
Widespread damage |
A Dinghy Sailor's Scale.
There are, of course, other versions of the Beaufort Scale. In the early 70s, the Heron Dinghy Class had its own set of definitions as follows.
Heron Dinghy Class Wind Scale- circa 1970 | |
1 |
Helmsman and crew sit well in board. Boat has very little way on. |
2 |
Helmsman only sits on weather side. |
3 |
Helmsman and crew both sit on weather side. |
4 |
Helmsman and crew both sit out on weather side. |
.5 |
Dinghies have to ease sheets in heavier gusts when beating. |
6 |
Reefing necessary, even when racing. |
7 |
Mainsail reefed below jib head. Boats should not be taken out. |
8 |
Difficult to sail at all even with jib only. |
In our days of sailing Fireflies, we knew that we could plane at the high end of a Force 3. No doubt, other classes will have their bench marks,
A Coarse Sailor's Scale
In Wind in the Willows, Toad of Toad Hall described sailing as mucking about in boats. On the other hand, Michael Green in his wonderfully, apocryphal book, The Art of Coarse Sailing defined sailing on the Broads as boating about in the muck. In this book and very much in keeping with the general tenor he defined the Coarse Sailor's Beaufort scale as follows -
Force |
Coarse Sailor's Sea Going Version |
Landsman's version |
0 |
Boat moves sideways with tide. |
Cigarette smoke gets in eyes. |
1 |
Coarse yachtsman hoists sail, then wind drops. |
Wet finger feels cold. |
2 |
Tea towels blow off rigging. |
Public houses close one window. |
3 |
Coarse boats careen. Difficult to make tea underway |
Public houses close two windows. |
4 |
Gas keeps going out. |
Beer froth blows off. |
5 |
Coarse sailors get book on sailing from cabin and look up bit about reefing. |
Customers in pub gardens go inside bar. |
6 |
Coarse sailors try to double reef and go aground |
Elderly customers have difficulty in leaving pub. |
7 |
Coarse sailor rescued by launch. |
Pub door cannot be opened against wind. |
8 |
Aaaaaaah!! |
Pub sign blows down. |
9 |
Coarse sailors in pub. |
Coarse sailor hit by falling sign |
Above force 9 - only of interest on TV. |
In Dieppe one of my correspondents saw Météo France cards in the Capitainerie. On the back of these cards was a definition of the Beaufort scale including Force 9 and above - "Les enfants moins de six ans volent" - "If children less than 6 years old fly". Even Michael Green would have been proud of that one!
Along the same lines and thanks to another of my contacts, I can offer the following, attributed to Geoffrey Ball, Sutton Coldfield,
Force |
Revised description |
0 |
Children want dad to fly new kite |
1 |
Reading newspaper out of doors becomes a problem |
2 |
Reading newspaper out of doors becomes impossible |
3 |
Twigs by front window begin to tap on glass |
4 |
Side gate bangs in night if someone forgot to put bolt on |
5 |
Old gentlemen's hats blow away |
6 |
Clothes line comes down dragging newly washed clothes on grass |
7 |
Side gate bangs in night even when bolted |
8 |
Car steering seems to have gone wrong |
9 |
Old ladies hats blown away |
10 |
Clothes line with newly washed sheets takes off |
11 |
Old ladies and old gentlemen blown away |
12 |
Children want dad to fly new kite |
A Cruising Yachtsman's Scale
More recently, a firm of riggers produced the following versions -
Helmsman's version |
Crew's version | |
0-1 |
Drifting conditions |
Boredom |
2 |
Set large sail to catch wind. |
Mild pleasure. |
3 |
Large headsail and full mainsail |
Pleasure |
4 |
Reduce headsail and mainsail |
Great pleasure |
5 |
Reduce headsail and reef mainsail |
Delight |
6 |
Ditto |
Delight tinged with anxiety |
7 |
Reefed mainsail and small jib |
Anxiety tinged with fear |
8 |
Deep reefed mainsail |
Fear tinged with terror |
9 |
Set storm jib and trysail |
Great terror |
10 |
Survival conditions |
Panic |
The Philosophy of the Beaufort Scale
Clearly there will be variations on the definitions depending upon the yacht, its crew and their recent lifestyle. A Hallberg Rassy 42 would have different rigs for the various wind forces from, say, a small, light yacht such as a Jeanneau 30. A fit, young, strong crew may keep more sail than a retired couple who simply want a comfortable sail and are not concerned about speed.
All the versions of the Beaufort Scale, from the original 1810 version right through the jokey Michael Green versions to the serious and semi-serious Atlantic Spars versions have a common feature.
They all relate the wind to its effects on boats, the sea, people and the world around us. It is that that makes the Beaufort Scale still the most appropriate way to describe wind in weather forecasts for seafarers. There are other reasons. First, the wind is never constant and it is tedious to have to write and listen to an expected wind speed as a range of knots. Secondly, it helps clarity when hearing a forecast to have one or two words clearly enunciated rather than a phrase. Thirdly, the use of the Beaufort Scale does remind us, should we need reminding, that what matters to us is the effect of the wind rather than some number of knots.
Calibrating yourself
The sailor can, of course, check his estimates of the wind force by reference to his measured apparent wind speed. This is best taken using a mast head instrument but a hand held anemometer will suffice. Strictly speaking the hand-held measurements should be corrected for height in order to replicate the masthead reading but this is probably not necessary bearing in mind the various errors in observation. In order to calculate the true wind speed allowance has to be made for the speed of the yacht. This can be done graphically using the triangle of velocities method or by using the mathematical version, the cosine rule.
If you have a VMG display, then it is a simple matter to subtract the VMG value from the indicated wind when going upwind. Going downwind, add the VMG value to the indicated, relative, wind speed. This can become painfully obvious when running downwind and flying a spinnaker when short-handed. It is all too easy to be enjoying tramping along at 7 or eight knots but then suddenly realise that the relative wind has crept up to 15 knots and that the true wind must be around the bottom of Force 6.
Frightening for a cruising yacht skipper but delight to a racing crew.