The Every-day Book and Table Book. v. 2 (of 3): or Everlasting Calendar of Popular Amusements, Sports, Pastimes, Ceremonies, Manners, Customs and Events, Incident to Each of the Three Hundred and Sixty-five Days, in past and Present Times; Forming a Complete History of the Year, Month, and Seasons, and a Perpetual Key to the Almanac — John Shaqi
The Every-day Book and Table Book. v. 2 (of 3): or Everlasting Calendar of Popular Amusements, Sports, Pastimes, Ceremonies, Manners, Customs and Events, Incident to Each of the Three Hundred and Sixty-five Days, in past and Present Times; Forming a Complete History of the Year, Month, and Seasons, and a Perpetual Key to the AlmanacHone, William
History
The Every-day Book and Table Book. v. 2 (of 3): or Everlasting Calendar of Popular Amusements, Sports, Pastimes, Ceremonies, Manners, Customs and Events, Incident to Each of the Three Hundred and Sixty-five Days, in past and Present Times; Forming a Complete History of the Year, Month, and Seasons, and a Perpetual Key to the Almanac
Hone, William
Days; Great Britain -- Social life and customs
Mr. Luke Howard is the author of a highly useful work, entitled “The
Climate of London, deduced from Meteorological Observations, made at
different places in the neighbourhood of the Metropolis: London, 1818.”
2 vols. 8vo. Out of this magazine of fact it is proposed to extract,
from time to time, certain results which may acquaint general readers
with useful knowledge concerning the weather of our latitude, and induce
the inquisitive to resort to Mr. Howard’s book, as a careful guide of
high authority in conducting their researches. That gentleman, it is
hoped, will not deem this an improper use of his labours: it is meant to
be, as far as regards himself, a humble tribute to his talents and
diligence. With these views, under each month will be given a state of
the weather, in Mr. Howard’s own words: and thus we begin.
JANUARY WEATHER
The _Sun_ in the middle of this month continues about 8 h. 20 m. above
the horizon. The _Temperature_ rises in the day, on an average of
twenty years, to 40·28° and falls in the night, in the open country to
31·36°--the difference, 8·92°, representing the mean effect of the sun’s
rays for the month, may be termed the _solar variation_ of the
temperature.
The _Mean Temperature_ of the month, if the observations in this city be
included, is 36·34°. But this mean has a range, in ten years, of about
10·25°, which may be termed the _lunar variation_ of the temperature. It
holds equally in the decade, beginning with 1797, observed in London,
and in that beginning with 1807, in the country. In the former decade,
the month was coldest in 1802, and warmest in 1812, and coldest in 1814.
I have likewise shown, that there was a tendency in the _daily_
variation of temperature through this month, to proceed, in these
respective periods of years, in opposite directions. The prevalence of
different classes of winds, in the different periods, is the most
obvious cause of these periodical variations of the mean temperature.
The _Barometer_ in this month rises, on an average of ten years, to
30·40 in., and falls to 28·97 in.: the _mean range_ is therefore 1·43
in.; but the extreme range in ten years is 2·38 in. The mean height for
the month is about 29·79 inches.
The prevailing _Winds_ are the class from west to north. The northerly
predominate, by a fourth of their amount, over the southerly winds.
The average _Evaporation_ (on a total of 30·50 inches for the year) is
0·832 in., and the mean of De Luc’s hydrometer 80.
The mean _Rain_, at the surface of the earth, is 1·959 in.; and the
number of days on which snow or rain falls, in this month, averages
14,4.
A majority of the _Nights_ in this month have constantly the temperature
at or below the foregoing point.[4]
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