A Treatise on Meteorological Instruments: Explanatory of Their Scientific Principles, Method of Construction, and Practical UtilityNegretti, Enrico Angelo Lodovico
Science
A Treatise on Meteorological Instruments: Explanatory of Their Scientific Principles, Method of Construction, and Practical Utility
Negretti, Enrico Angelo Lodovico
Meteorological instruments; Meteorology; Scientific apparatus and instruments
At 31 inches Very dry.
" 30.5 " Settled fair.
" 30 " Fair.
" 29.5 " Changeable.
" 29 " Rain.
" 28.5 " Much rain.
" 28 " Stormy.
The French place upon their barometers a similar formula:--
At 785 millimetres Tres-sec.
" 776 " Beau-fixe.
" 767 " Beau temps.
" 758 " Variable.
" 749 " Pluie ou vent.
" 740 " Grande pluie.
" 731 " Tempete.
Manufacturers of barometers have uniformly adopted these indications for
all countries, without regard to the elevation above the sea, or the
different geographical conditions; and as it can readily be shown that the
height and variations of the barometer are dependent on these, it follows
that barometers have furnished indications which, under many
circumstances, have been completely false. Even in this country, and near
the sea-level, storms are frequent with the barometer not below 29; rain
is not uncommon with the glass at 30; even fine weather sometimes occurs
with a low pressure; while it is evident that at an elevation of a few
thousand feet the mercury would never rise to 30 inches; hence, according
to the scale, there should never be fair weather there. If tempests
happened as seldom in our latitude as the barometer gets down to 28
inches, the maritime portion of the community at least would be happy
indeed. These words have long been ridiculed by persons acquainted with
the causes of the barometric fluctuations; nevertheless opticians continue
to place them on the scales, evidently only because they appear to add to
the importance of the instrument in the eyes of those who have not learned
their general inutility. In different regions of the world, the
indications of the barometer are modified by the conditions peculiar to
the geographical position and elevation above the sea, and it is necessary
to take account of these in any attempt to found rules of general utility
in connection with the barometer as a weather guide. All that can be said
in favour of these words is, that within a few hundred feet of the
sea-level, when the column rises or falls gradually during two or three
days towards "Fair" or "Rain," the indications they afford of the coming
weather are generally extremely probable; but when the variations are
quick, upward or downward, they presage unsettled or stormy weather.
Public-domain text, read in full here on John Shaqi.
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