Outlines of a mechanical theory of storms : $b containing the true law of lunar influence, with practical instructions to the navigator, to enable him approximately to calculate the coming changes of the wind and weather, for any given day, and for any part of the oceanBassnett, Thomas
Science
Outlines of a mechanical theory of storms : $b containing the true law of lunar influence, with practical instructions to the navigator, to enable him approximately to calculate the coming changes of the wind and weather, for any given day, and for any part of the ocean
Bassnett, Thomas
Weather
We will now make the calculation for the central vortex _descending_,
for longitude 88° 50′ west, August 7, 1853,--putting down the necessary
elements for the time of the meridian passage in order:
Meridian passage in local time at 2h. 25m. P.M.
" " in Greenwich time 7d. 8h. 18m.
Mass of the moon 1/12.3 M. R. V. minor 3,256 miles.
Obliquity of the vortex, same time 26° 5′ 0″
Polar angle of " " 17 41 47
True longitude of moon's node " 78 42 0
" inclination of orbit " 5 5 0
" longitude of the sun " 135 20 0
Moon's longitude " 169 44 0
" distance from node " 91 2 0
" distance from quadrature " 55 36 0
" true semi-diameter " 943
" right ascension " 172 30 0
" declination north " 8 42 20
Constant logarithm 2.889214
Arith. comp. of log. of 943 7.025488
Log. cos. arc. AR 9.914702 = 34° 44′ 48″
1st. correction, + 2 45 0
2d. correction, - 1 14 15
--------------
Corrected arc AQ = 36 15 33
PA = 81° 17′ 40″
PV = 26 5 0
P = 115 11 47
V = 63 34 26
A = 23 28 24
AV = 92 48 39
Q = 31 32 18
Complement of lat. = PQ = 48° 49′ 41″
The latitude is therefore for
the earth, as a sphere 41 10 18
Correction for protuberance + 0 16 0
------------
True latitude of centre 41 26 18 north.
------------
Latitude of Ottowa 41 20 0 "
------------
Vortex passed 6 18 north of Ottowa.
[Illustration: Fig. 16]
As this was nearly a central passage, and as the influence was less
extensive than usual, on account of great atmospheric pressure with a
low dew point, the central disturbance could the more readily be
located, and was certainly to the north, and but a few miles. The
following is from the record of the weather:
_August_ 6th. Very fine and clear all day; wind from S.-W.; a light
breeze; 8 P.M. frequent flashes of lightning in the northern sky;
10 P.M. a _low bank of dense clouds in north_, fringed with cirri,
visible during the flash of the lightning; 12 P.M. same continues.
Public-domain text, read in full here on John Shaqi.
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