10

THE HONGKONG GOVERNMENT GAZETTE, 7TH JANUARY, 1888.

rule a fraction of a degree and sometimes much more. But the wind does not return to quite its original direction. There is frequently a change. At the time when the centre is pissing nearest to a vessel, a fierce squall is frequently entered in the log-book. The existence of a line of squalls perpen- dicular to the path of a storm-centre is well known in the storms that cross the British Isles.

It is remarked that typhoons often arrive in quick succession followed by intervals without typhoons, but during the height of the typhoon-season there is generally a typhoon to be found some- where at any time. The following table exhibits the number of typhoons that occurred during the past three years within squares of 2° extent in longitude and latitude :-

FREQUENCY OF TYPHOONS IN 1884-1886 INCLUSIVE.

LONGITUDE EAST.

Latitude 104° 106° 108° 110° 112°

North.

116 118° 120° 122° 124° 126° 128° 130° 182° 134o 136° 138o 140o 142o|

106° 108° 110° 112° 114° |[116° 118° | 120° | 122° 124° 126° | 128° 130° 132° 134° 136° 138o 140o 142° 144°

Sums.

42° - 44°

40° - 42°

38° - 40°

36° - 38°

34° - 36°

32° - 34°

30° - 32°

28° - 30°

TAT

:

:

:

÷

:

:

:

:

:

:

:

:

:

1

1

2

2

N

3

2 2

15

CO

co

4

сл

5

4

27

I

1

1

30

cc

:

1 1 1

1 2 4

N

O

~

N

Co

1

1

1

3

1

4

сл

5

ลง

H

3

7

7

10

5

N

CO

6 3

45

3

ลง

2

2

37

3 3

46

H

4

2

10

C

LO

w

AL

26° - 28°

24° - 26°

22° - 24°

20° - 22°

:

:

:.

1

A

10

5

5

Dr.

1

NO

3

5

10

5

00

5

2

5 2

7

N

CO

CO

10

10

10

4

7

5

~

48

40

10

1

39

41

:

1

39

1

1

47

1

1

1

2

5

4

4

i

3

2

1

1

48

18° – 20°

1

3

7

6 8 7 5

5

2 4

3

3

1.

16o - 18°

2

3

CAS

3

5

Co

00

14° - 16°

12° -14°

10° - 12°

8° - 10°

2 1

2

2

1 4

7

:

:

:

ลง

4

3 2

2

ลง

10

4

5

3

คง

2

~

:

:

5

2

2

1

1

1

1 2 2

2 2

2

2

1 1 1

1 1 1 1

:

:

:

:

:

:

A

72

60

8.00

:

46

34

25

10

Sums.

10

5

9

10 20 31 39 46 55 46 82 71 57 60 47 40 30

29 23 14

719

From the figures in the horizontal lines the average longitude for every 2° of latitude was computed in analogy with the theory of the lever. A curve was then drawn among the points laid down on the

The result was as follows:-

*-----

map.

Long.

Long.

Lat.

Lat.

read.

corr.

read.

corr.

43°

135°

136°.9

25°

124°

123°.8

41

137

135 .2

23

125

123 .1

39

134

133 .5

21

124

122 .6

37

133

132 .0

19

122

122 .4

35

132

130 .2

17

121

122 .3

33

129

128 .4

15

124

122 .5

31

127

126 .8

13

123

123 .1

29

125

125 .5

11

124

124 .3

27

125

124 .6

126

126 .1

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