870 
870 
Hourty METEOROLOGICAL OBSERVATIONS, JANUARY 6—8, 1845. 
THERMOMETERS. 
Dry. | Wet. 
36-2 | 35-8 
36-5 | 36-1 
37-0 | 36-6 
37-3 | 36-9 
39-6 | 39-2 
41-9 | 41-0 
41-7 | 40-7 
43-3 | 42-1 
42-0 | 40-8 
43-3 |41-6 
40-7 | 39-4 
40-6 | 39-1 
40:3 | 38-6 
35:3 | 34-7 
32-7 | 32-3 
32-8 | 32-2 
32-3 | 31-7 
Diff. 
7 Fee G0) aS 
NEON Oe BIN 
0-5 
0-4 
WIND. 
Maximum 
force in [Prom 
0-1 | 0-0 | 20 
S25 Sees 2S 
es 
i) 
i) 
_ 
=r) 
0-1 10-0 | 23 
Se. : C.-s.: Ci., 
Clouds, 
moving 
from 
pt. pt. 
j:—:22 
:— 122 
—:—:22 
:23:— 
:22:— 
722:— 
:20:— 
Species of Clouds and Meteorological Remarks. 
Scud ; woolly cir. and cir.-str., lying WSW. to ENE. 6] — 
Patches of scud; woolly cirri; cirro-strati. 
Woolly cirri; cirro-strati; haze. 
Id. ; id. ; id. 
id: § id. ; id. 
As before. 
Id. 
Id. 
Id.; stars dim. 
Cirri and cirrous haze. 
Id. 
Cirri and cirrous haze. 
Td. 
Id. 
Td. 
Id. ; drops of rain. 
Rain , 
Cirri, &c.; Rain °*; a few stars very dim. 
Id. id, 
Cirro-stratous scud ; cirro-strati. 
Mass of cirro-stratus. 
Thick mass of wavy cirro-stratus. 
Cirro-stratous scud ; cirro-strati; cirri. 
Cirro-cumuli; cirro-strati; cirrous haze. el] 
Wo. cir.-cum; stratus to E. ; cir.-str. scud ; cir. haze. 
Linear cirri; stratus to E. and S. © | 
iGGs id. ; cirro-strati. 3) 
Woolly cirri ; id. ; id, 
Cirro-strati and cirri on horizon. 
Cirrous clouds. 
Id. 
Dark. 
Id. ; fine particles of rain. 
Dense fog. 
Id. 
Fog clearing away. 
Id. 
Cirro-stratous seud ; cirro-strati. 
Id. 
Masses of scud and cirro-strati. 
Scud ; loose cumuli; cirri; cirro-strati. 
Scud ; loose cumuli. 
Tas id. ; woolly cirri ; cirrous haze. 
Idi; id.; cirro-strati ; cirri; cirrous haze. 
Dense cirrous clouds and haze. 
Send; woolly cirrous clouds, very low; much haze. — 
As before. 
Cirro-strati; haze. 
Patches of light clouds to W. 
Haze round horizon. 
Id: patch of scud to E. 
Jan. 648». Jt was found that the balancing weight of the anemometer acted at about two inches from the extremity of the spiral when 
the index was at 0; the indications for some time must consequently have been rather too small: the suspending cord of the inner vesst 
was now shortened, so as to allow the weight to act correctly. 
Jan. 74 22h, 
same point. 
Masses of loose cirro-stratus evaporating very rapidly, whilst scud is forming as quickly ; both currents moving from th 
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