CO129-273 - Governor Sir Robinson & Others - 1896 [10-12] — Page 517

CO129 Colonial Office Hong Kong Records 理藩院香港檔案 All AI Reviewed

V.

THE DROUGHT OF 1895-1896.

rainfall on the two catchment-grounds, is not necessarily identical each with the other, or with that at the Observatory.

I think however that the more probable explanation is that although the overflow ceased at Pokefulam on 28th August, it continued for some time in September at Taitam.

(5)

The facts observed during this drought are valuable, because the Taitam reservoir, at least, never overflowed, and therefore the available percentage of the rainfall can be calculated with precision, during the wet season. There is no information to show whether the same condition obtained at Pokefulam.

The rain-year of 1895-96 was probably the lowest on record, 45".8 as against 91".75 or about one half the general average. This defect is mainly observed in the wet season, May to August, during which the rainfall was 35".6 as against 60".34 or 59 percent only, of average. The rain in August was somewhat in excess of average but that of the other wet months considerably below it.

The rainfall of the dry season was also low, 18".23 as against an average of 31".39 or 58% of the average. Indeed it is the second lowest record for the dry season, of the whole period of 20 years.

It is unnecessary to repeat the calculations which I have made in the case of 1890-1. I gave these at length, in order to show whether I had fully comprehended the method of calculation, adopted by Mr Cooper.

The results as to the percentage of available rainfall may be thus tabulated.

6

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V. THE DROUGHT OF 1895-1896. rainfall on the two catchment-grounds, is not necessarily identical each with the other, or with that at the Observatory. I think however that the more probable explanation is that although the overflow ceased at Pokefulam on 28th August, it continued for some time in September at Taitam. (5) The facts observed during this drought are valuable, because the Taitam reservoir, at least, never overflowed, and therefore the available percentage of the rainfall can be calculated with precision, during the wet season. There is no information to show whether the same condition obtained at Pokefulam. The rain-year of 1895-96 was probably the lowest on record, 45".8 as against 91".75 or about one half the general average. This defect is mainly observed in the wet season, May to August, during which the rainfall was 35".6 as against 60".34 or 59 percent only, of average. The rain in August was somewhat in excess of average but that of the other wet months considerably below it. The rainfall of the dry season was also low, 18".23 as against an average of 31".39 or 58% of the average. Indeed it is the second lowest record for the dry season, of the whole period of 20 years. It is unnecessary to repeat the calculations which I have made in the case of 1890-1. I gave these at length, in order to show whether I had fully comprehended the method of calculation, adopted by Mr Cooper. The results as to the percentage of available rainfall may be thus tabulated. 6
Baseline (Original)
V. i = 001 -:་།།༼ ? 514 3 THE DROUGHT OF 1895 1896. rainfall on the two thering-grounds, is not nege888- -rily identical each with the other, or with that at the Observatory. I think however that the more probable explana - tion is that although the overflow nessed at Pokefoolum on 28th August, it continued for some time in September at Taitam. (5) The facts observed during this drought are valuable, because the Taitam reservoir, at least, never overflowed, and therefore the avaliable percentage of the rainfall can be calculated with precision, during the wet season. There is no information to snew wheti er the same condition obtained at Pokefoolum. d The rain-year of 1895-96 was probably tre lowest on record, 45o.B as against 91".75 or about one half the general average. Tris defect is mainly observ- -ed in the wat season, May to August, during which the rainfal▲ was 35,6 as against 60".34 or 59 per omnt only, of average. The rain in August was somewhat in exOASS of average but that of the other wet montis considerably below it. The rainfall of the dry season was also low, 18.23 as against an average of 31.39 or 58% of the Indeed it is the segond lowest record for average. the dry season, of the whole period of 20 years. It is unnecessary to repeat the algulations which I have made in the oase of 1890-1. I gave these at length, in order to shew whether I nad fully comprehended the method of simulation, adopted by Mr Cooper, The results as to the percentage of avaliable rainfall may be thus tabulated. 6
2026-05-28 05:59:48 · Baseline
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V.

i

= 001

-:་།།༼

?

514

3

THE DROUGHT OF 1895 1896.

rainfall on the two thering-grounds, is not nege888-

-rily identical each with the other, or with that at

the Observatory.

I think however that the more probable explana -

tion is that although the overflow nessed at Pokefoolum

on 28th August, it continued for some time in September

at Taitam.

(5)

The facts observed during this drought are

valuable, because the Taitam reservoir, at least, never

overflowed, and therefore the avaliable percentage of

the rainfall can be calculated with precision, during the

wet season. There is no information to snew wheti er

the same condition obtained at Pokefoolum.

d

The rain-year of 1895-96 was probably tre

lowest on record, 45o.B as against 91".75 or about one

half the general average. Tris defect is mainly observ-

-ed in the wat season, May to August, during which the

rainfal▲ was 35,6 as against 60".34 or 59 per omnt only,

of average. The rain in August was somewhat in exOASS

of average but that of the other wet montis considerably

below it.

The rainfall of the dry season was also low,

18.23 as against an average of 31.39 or 58% of the

Indeed it is the segond lowest record for

average.

the dry season, of the whole period of 20 years.

It is unnecessary to repeat the algulations

which I have made in the oase of 1890-1. I gave

these at length, in order to shew whether I nad fully

comprehended the method of simulation, adopted by Mr

Cooper,

The results as to the percentage of avaliable

rainfall may be thus tabulated.

6

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