AECTIC SEAS. — PAET V. EEFUGE COYE. 
835 
Table II. (continued). 
High Water. 
Low Water. 
High Water. 
Low Water. 
1853. 
k 
m 
k m 
h 
m 
1853. 
h m 
k m 
h m 
Sept. 25. 
10 
20 A.M. 
7 
35 
Oct. 3. 
6 45 p.m. 
5 51 
25 . 
5 
30 p.m. 
-0 49 
3. 
Midnight 
— 1 0 
26 . 
12 
30 A.M. 
5 
49 
4. 
7 15 A.M. 
5 45 
26 . 
5 
45 „ 
-1 1 
4. 
Noon 
-1 27 
26 . 
12 
30 p.m. 
6 
16 
4. 
8 0 p.m. 
5 27 
26 . 
6 
30 „ 
-0 40 
5. 
1 0 A.M. 
-0 51 
27 . 
1 
15 A.M. 
5 
55 
5. 
8 30 „ 
5 21 
27 . 
7 
0 „ 
-0 37 
5. 
1 28 p.m. 
-0 53 
27. 
l 
30 p.m. 
6 
7 
5. 
8 20 „ 
6 1 
2.7. 
7 
30 „ 
— 0 31 
6. 
1 40 a.m. 
-1 5 
28. 
3 
0 A.M. 
5 
l 
6. 
8 30 „ 
6 15 
28. 
8 
0 „ 
-0 29 
6. 
1 0 P.M. 
-2 17 
28. 
3 
30 p.m. 
4 
59 
6. 
9 30 „ 
5 47 
28. 
10 
5 „ 
+ 1 12 
7. 
4 0 A.M. 
+ 0 19 
29. 
4 
0 A.M. 
4 
53 
7. 
9 0 „ 
6 41 
29. 
10 
25 „ 
+ 1 6 
7. 
3 0 p.m. 
-1 16 
29. 
4 
0 P.M. 
5 
19 
7- 
9 45 „ 
6 31 1 
29. 
10 
40 „ 
+ 0 57 
8. 
4 0 A.M. 
-0 40 
30. 
5 
0 A.M. 
4 
43 
8. 
10 0 „ 
6 40 
30. 
10 
45 „ 
+ 0 36 
8. 
5 0 p.m. 
-0 17 
30. 
4 
45 p.m. 
5 
24 
8. 
10 50 „ 
6 27 
30. 
11 
45 „ 
+ 1 12 
9. 
4 15 A.M. 
-1 26 
Oct. 1. 
6 
0 A.M. 
4 
33 
9. 
10 50 „ 
6 51 
1. 
11 
o » 
+ 0 2 
9. 
4 50 p.m. 
00 
©I 
7 
1. 
5 
15 P.M. 
6 
17 
10. 
12 10 a.m. 
6 8 
1. 
11 
45 „ 
+ 0 23 
10. 
4 30 „ 
-2 12 
2. 
5 
0 A.M. 
6 
22 
10. 
12 30 p.m. 
6 12 
2. 
12 
30 p.m. 
+ 0 18 
10. 
6 45 „ 
— 0 31 
2. 
6 
15 „ 
5 
57 
11. 
2 0 A.M. 
5 16 
3. 
12 
20 A.M. 
-0 16 
11. 
6 40 „ 
...... 
-1 0 
3. 
6 
o 
6 
36 
3. 
1 
0 P.M. 
+ 0 24 
Mean 
-0 26-7 
6 1-1 
If we compare the mean Lunitidal Intervals here found with the corresponding 
intervals at Northumberland Sound, we find : — 
Mean Lunitidal Interval. 
High Water. Low Water, 
h m h m 
Eefuge Cove —0 26-7 6 IT 
Northumberland Sound . . -{-0 7'05 6 35-35 
Difference .... 33-75 34-25 
These differences represent the time of the Atlantic Tide-wave passing from Eefuge 
Cove to Northumberland Sound (uncorrected for longitude) ; and their agreement is a 
proof of the accuracy of the observations at both places. 
B. Semidiurnal Tide (Heights). 
When Table I. is plotted to scale, it is easy to correct the tide for the Diurnal 
Inequality, or to do so by th.e Diurnal Tide at High Water and Low Water given in 
2 y 2 
