222 SUPPLEMENT TO THE HONGKONG GOV" GAZETTE OF 7TM MAR., 1885.
GOVERNMENT NOTIFICATION.---No. 107.
The following Report on the height of Victoria Peak, furnished by the Government Astronomer, is published for general information.
By Command,
Colonial Secretary's Office, Hongkong, 7th March, 1885.
ON THE HEIGHT OF VICTORIA PEAK.
W. H. MARSH,
Colonial Secretary,
The height of Victoria Peak has been calculated (from the monthly means of observations made
2h'
H
during 1884) by aid of Ferrel's tables derived from the formula:- b'
H=60521.5 (log. Bʻ-log B) (1+.001017 [t′+t-64°]) (1+.189) (1+.189) (1 + —2——) (1 + 7 )
(1+.002606 cos. 2×).
T
-) −
I
H represents the difference of height betweca the upper and lower stations-here, the Peak and the Observatory; B the barometric pressure reduced to 32° Fahrenheit at the upper station as exhibited in the third column of the following table; B' the same at the lower station as exhibited in the second column; t the temperature of the air at the upper station, t' the same at the lower station as exhibited in the fifth and the fourth columns; b the tension of aqueous vapour at the upper station, b' the same at the lower station as exhibited in the seventh and the sixth columns; h' the height of the lower station above mean sea level-bere, 107.1 feet, and a the geographical latitude of the upper station-- here, about 22° 16′.
Month.
B'
B
t
b'
H
1884.
ins.
ins.
ins.
ins.
feet.
January,
30.093
28.302
62.3
55.4
0.443
0.404
1713.4
February,
30.061
28.244
57.0
50.8
0.377
0.337
1723.0
May,
29.752
28.038
74.8
68.4
0.736
0.662
1703.9
June,
29.662
27.965
80.1
72.4
0.850
0.767
1709.0
July,
29.581
27.893
82.2
74.7
0.908
0.816
1712,6
August,
29.625
27.937
81.8
74.6
0.886
0.802
1709.0
September,
29.685
27.993
81.2
73.9
0.811
0.741
1706.0
October,
29.920
28.198
77.2
70.0
0.698
0.634
1707.8
November,
29.396
28.228
67.8
60.9
0.490
0.457
1715.6
December,
30.119
28.323
59.6
53.3
0.318
0.281
1706.1
Mean,
29.849
28.112
72.4
65.4
0.652
0.590
1710.6
It will be remarked that no correction for barometric gradient has been applied, in fact the height of the barometer reduced to sea level does not differ more than a fraction of a thousandth of an inch between the two stations, nor is a correction for diminution of gravity with increasing height called for as both barometers are mercurial.
The mean of the resulting differences of height increased by 107.1 fect, the height of the lower station above mean sea level, gives finally the height of the Peak at the highest level of the rock where the look-out tower is erected. The differences in the results exhibited in the last column of the table are due principally to the fact, that it has been assumed that the mean of the temperatures of the air at the Observatory and at the Peak, represents accurately the average temperature of the air between the two stations. The probable error of the final result has been determined from these differences, to be about 14 inches. The height is therefore determined with such accuracy and a more accurate result can only be obtained from several years observations.
Altitude of Victoria Peak-1818 feet+1} feet above mean sea level.
Hongkong Observatory, 5th February, 1885.
W. DOBERCK, Government Astronomer.
Printed and Published by NORONHA & Co., Printers to the Hongkong Government, Nos. 5, 7, and 9, Zetland Street.
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