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
=119. Laws of Rain-fall.=--Tropical countries have a dry and a wet season
during the year: _dry_, when the sun is at the opposite side of the
equator; _wet_, when the sun is overhead. With reference to the British
Isles, the statistics collected by Mr. G. J. Symons indicate that: 1st.
The stations of least rain are inland, or on the east or south-east
coasts; the stations of greatest rain are on the western coasts. 2nd. The
rain-fall is very large in the vicinity of mountain chains or groups,
unless the station happens to be some miles to the north-eastward.
It may be well to illustrate these remarks by quoting[12] the average fall
at a few places, grouping them as--
Westerly.
Inches.
Bodmin 43
Bolton (Lancashire) 44
Coniston (Windermere) 71
Seathwaite 127
Torosay (I. of Mull) 75
Killaloe (Limerick) 38
Central.
Inches.
Enfield 23
Epping 23
Derby 24
York 22
Stirling 39
Perth 29
Easterly.
Inches.
Witham (Essex) 21
Patrington (Hull) 21
Sunderland 17
Inveresk (Edinburgh) 25
Pittenweem (Fife) 24
Dublin 22
Mr. Green, the celebrated aeronaut, has asserted from his experience,
"that whenever a fall of rain happens, and the sky is entirely overcast,
there will invariably be found to exist another stratum of cloud at a
certain elevation above the former;" and the recent scientific balloon
ascents by Mr. Glaisher have tended to confirm this theory. Mr. Glaisher
says, "It would seem to be an established fact, that whenever rain is
falling from an overcast sky, there is a second stratum above." "It would
also seem that when the sky is overcast without rain, that there is no
stratum of cloud above, but that the sun is shining on the upper surface.
In every instance in which I have been up under these circumstances, I
have found such to be the case, agreeing in this respect also with Mr.
Green's observations."
The amount of rain collected in a gauge placed near the surface of the
earth is larger than in any gauge placed above it; and the higher the
gauge is placed, the less water is collected. Mr. Glaisher contends that
his balloon experiments corroborate this law.
Public-domain text, read in full here on John Shaqi.
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