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SQUALL , the name given to any sudden increase of See also: wind to gale force
.
Generally speaking a squall is understood to be of See also: 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-See also: 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 See also: coast station the ribbon is wider for a See also: shore wind than for a See also: sea wind
.
From the records obtained at Scilly and Holyhead, Dr G
.
C
.
See also: Simpson concluded. that a wind of mean hourly velocity v was composed of alternations of gusts and lulls ranging on the See also: 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 See also: hour when the mean velocity is v, and the extreme range within the same See also: 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:
See also: Southport (Marshside) to m
.
Scilly 15 „
See also: Shoeburyness 20 „ (from W.)
.
.
.
10 „ (from E.N.E.)
Holyhead 15 „
Pendennis See also: Castle (See also: Falmouth) 8 „ (from S.)
16 (from \V.)
See also: Aberdeen 30 „ (from N.W.)
See also: Alnwick Castle 25 „
See also: Kew 30 „
Fig
.
2 represents a succession of squalls occurring in an ordinary gusty wind; the squalls succeed one another with See also: 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
.
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