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
Supposing a compass diagram, with the principal points laid down, the N.E.
is the wind for which the barometer stands highest; for the S.W. wind it
is lowest. This is found to be so in the great majority of cases; but
there are exceptions to this, as to all rules. The N.E. and S.W. may
therefore be regarded as the poles of the winds, being opposite each
other. When the wind veers from the S.W. through W. and N. to N.E., the
barometer gradually rises; on the contrary, when the wind veers from N.E.
and E. to S.E., S. and S.W., the mercury falls. A similar curious law
exists in relation to the veering of the wind, and the action of the
thermometer. As the wind veers from the S.W. to W. and N., the thermometer
falls; as it veers from N.E. to E. and S., it rises, because the wind gets
from a colder to a warmer quarter. The polar winds are cold, dry, and
heavy. Those from the equatorial regions are warm, moist, and
comparatively light.
These laws have been clearly developed and expressed by Professor Dove in
his work on the "Law of Storms." The warm winds of Europe are those which
bring the greatest quantity of rain, as they blow from the ocean, and come
heavily laden with moisture. The cold winds, besides containing less
moisture, blow more from the land. The weight of the vapour of the warm
winds tends to raise the barometric column; but, at the same time, the
increased dilatation of the air tends to lower it. This latter influence
being the stronger, the barometer always falls for these winds; and in
regions where they traverse a large extent of land, retain their heat, and
become necessarily very dry, the fall in the barometer will be greater.
Admiral FitzRoy's words for the scales of barometers for use in northern
latitudes, then, are as follows:--
_RISE._ _FALL._
FOR FOR
N. ELY. S. WLY.
NW.--N.--E. SE.--S.--W.
DRY WET
OR OR
LESS MORE
WIND. WIND.
------- -------
EXCEPT EXCEPT
WET FROM WET FROM
N. ED. N. ED.
------- -------
Long foretold, long last; First rise after low,
Short notice, soon past. Foretells stronger blow.
It will be perceived that the exception in each case applies to N.E.
winds. The barometer may fall with north-easterly winds, but they will be
violent and accompanied with rain, hail, or snow; again, it will rise with
these winds accompanied with rain, when they are light, and bring only
little rain. It rises, however, highest with the dry and light N.E. winds.
Public-domain text, read in full here on John Shaqi.
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