CO129-273 - Governor Sir Robinson & Others - 1896 [10-12] — Page 518

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

CONCLUSIONS.

The figures enclosed by brackets may, I think, be rejected as unduly reduced by want of sufficient storage and consequent overflow. There is no reason why, with any given rainfall, the available percentage at Pokfulam should not be the same as at Tai Tam, except on account of want of storage.

(7) The general conclusions which may be drawn from the data given in the report before me are as follows.

(a) That the rain-year 1895-1896 is a probable minimum. So dry a year is not likely to occur more than once in 20 years, probably in a longer period. 53.83 inches fell, as against an average of 91.76 or 58 per cent.

(b) That the rain-year 1890-91, 66.96 inches as against 91.76 average, was also an unusually dry one.

(c) It is instructive as giving an example of a prolonged drought. The rainfall during the four wet months was not abnormally low, 57.62 as against an average of 60.34. The rainfall during the eight dry months was only 9.34 (Vide appendix A), as against an average of 31.42.

In as much as no such occurrence has ever taken place during 20 years and more, it is not correct

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CONCLUSIONS. The figures enclosed by brackets may, I think, be rejected as unduly reduced by want of sufficient storage and consequent overflow. There is no reason why, with any given rainfall, the available percentage at Pokfulam should not be the same as at Tai Tam, except on account of want of storage. (7) The general conclusions which may be drawn from the data given in the report before me are as follows. (a) That the rain-year 1895-1896 is a probable minimum. So dry a year is not likely to occur more than once in 20 years, probably in a longer period. 53.83 inches fell, as against an average of 91.76 or 58 per cent. (b) That the rain-year 1890-91, 66.96 inches as against 91.76 average, was also an unusually dry one. (c) It is instructive as giving an example of a prolonged drought. The rainfall during the four wet months was not abnormally low, 57.62 as against an average of 60.34. The rainfall during the eight dry months was only 9.34 (Vide appendix A), as against an average of 31.42. In as much as no such occurrence has ever taken place during 20 years and more, it is not correct
Baseline (Original)
R 7 01 i. * £ 515 kainfall rokefooluni inches Fer gent Taitam Fer gent : th 28 August 1890 to 2nd May 1891 9.74 40 (32) Ke year 1895 (Oslendar} 45.84 (48) 56 . May to August 1895 35.60 (40) 57 Sept. 1995 to April 1896 18.23 57 34 - - རྞ CONCLUSIONS. The figures enclosed by brackets may. I think, be rejected as unduly reduced by want of sufficient storage and consequent overflow. There is no reason why, with any given rainfall, the avaliable percentage at Foke foolum should not be the same as at laitam, except on account of want of storage. (7) The general conglusions whiзn may be drawn from the data given in the report before me are as follows. (a) (b) (0) "1 That the rain-year 1895 1896 is a probable minimum. So dry a year is not likely to occur more than ones in 20 years, probably in a longer period. 53.83 inones fell, as against an average of 91*.76 or 58 per cent. one. That the rain-year 1890-91, 66.96 inches as against 91*.76 average, was also an unusually dry It is instructive as giving an example of a prolonged drought. The rainfall during the four wet months was not abnormally low, 57".62 as The rainfall dur- against an average of 60",34. ing the eight dry months was only 9.34 (Vide app- endix A), as against an average of 31.42. In As much as no suar ooourrence has ever taken plage during 20 years and more, it is not correct 7
2026-05-28 06:00:04 · Baseline
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R

7

01

i.

* £

515

kainfall

rokefooluni

inches

Fer gent

Taitam

Fer gent

:

th

28 August 1890 to 2nd May 1891

9.74

40

(32)

Ke year 1895 (Oslendar}

45.84

(48)

56

.

May to August 1895

35.60

(40)

57

Sept. 1995 to April 1896

18.23

57

34

- - རྞ

CONCLUSIONS.

The figures enclosed by brackets may. I think,

be rejected as unduly reduced by want of sufficient

storage and consequent overflow. There is no reason

why,

with any given rainfall, the avaliable percentage

at Foke foolum should not be the same as at laitam, except

on account of want of storage.

(7)

The general conglusions whiзn may be drawn

from the data given in the report before me are as

follows.

(a)

(b)

(0)

"1

That the rain-year 1895 1896 is a probable

minimum. So dry a year is not likely to occur

more than ones in 20 years, probably in a longer

period. 53.83 inones fell, as against an average

of 91*.76 or 58 per cent.

one.

That the rain-year 1890-91, 66.96 inches as

against 91*.76 average, was also an unusually dry

It is instructive as giving an example of

a prolonged drought. The rainfall during the

four wet months was not abnormally low, 57".62 as

The rainfall dur- against an average of 60",34.

ing the eight dry months was only 9.34 (Vide app-

endix A), as against an average of 31.42.

In As much as no suar ooourrence has ever taken

plage during 20 years and more, it is not correct

7

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