Online Encyclopedia

SQUALL

Online Encyclopedia
Originally appearing in Volume V25, Page 744 of the 1911 Encyclopedia Britannica.
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SQUALL  , the name given to any sudden increase of

wind to gale force . Generally speaking a squall is understood to be of short duration, but the word " gust " would be used to indicate an increase of wind force of more transient character than a squall . Gusts may succeed one another several times within the compass of a minute . A squall may comprise a succession of gusts, with intervening partial lulls, and would last with varying intensity for some minutes at least . The distinci n between gusts and squalls is best illustrated by the traces of a Dines pressure-tube anemograph . The trace reproduced in fig . I for an ordinary steady wind shows that the force of the wind is constantly oscillating . The general appearance of the trace is a ribbon which has a breadth proportional to the mean wind velocity . The breadth of the ribbon is also dependent upon the nature of the reference; the better the exposure the narrower the ribbon; for an anemograph at a coast station the ribbon is wider for a
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shore wind than for a sea wind . From the records obtained at Scilly and Holyhead, Dr G . C . Simpson concluded. that a wind of mean hourly velocity v was composed of alternations of gusts and lulls ranging on the
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average between limits -5+1.2v and — •5+ •76V with occasional recurrences to extreme velocities of 1.5+I.3V and —I'o+•65v .

In other words, the average range of the ribbon is •5+.45v for the twostations during the

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hour when the mean velocity is v, and the extreme range within the same period is 2.0+ .685 . The differences of gust velocity at stations with different exposures may be illustrated by quoting the breadth of the ribbon for a 3o m. wind at the following stations:
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Southport (Marshside) to m . Scilly 15 „
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Shoeburyness 20 „ (from W.) . . . 10 „ (from E.N.E.) Holyhead 15 „ Pendennis Castle (
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Falmouth) 8 „ (from S.) 16 (from \V.) Aberdeen 30 „ (from N.W.)
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Alnwick Castle 25 „
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Kew 30 „ Fig . 2 represents a succession of squalls occurring in an ordinary gusty wind; the squalls succeed one another with
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fair regularity about every twenty minutes and last in full force for a few minutes . A 1~ ;'l ird 9a "k IT r P1 1 , riff I~r ~lu'lO L~~dtiIi, 11~4i Vi Nou 5p.m . 6 5p.m . 6 T 8 9 10 11 Midt . 1a.m . 2 FIG . 2 .

End of Article: SQUALL
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