354 REPORT — 1847 . 
Table II. {continued.) 
Epoch, Not. 
Rami- 
g»tc. 
Storno*. 
way. 
Stonio* 
way ±. 
1 Epoch, Not. 
Riau* 
g»le. 
Stvno. 
wsy. 
SUn^ 
11.9 p.u. 
.3o:« 
30-59 
-1--26 
1 15. 9 .i.u. 
30-27 
30-29 
+■02 
\2. 3a.m . 
36 
•59 
-t--23 
^ 3 v.u. ... . 
-24 
27 
t<6 
9 A.M . 
•36 
•64 
^-•28 
9 P.M . 
•2! 
•ai 
+<ri 
3 P.M. 
-.38 
•64 
+ ■26 
16. .^A.«. . 
■24 
3012 
-12 
9 P.M. 
•39 
•64 
-i-'25 
9 A.M . 
•26 
29-w: 
-•80 
]a. 3 A.M. 
•34 
•62 
+•28 
3 P.M. 
•2.1 
•85 
-•3« 
3 P.M. ...... 
•40 
•55 
+•15 
9 P.M. 
•18 
•73 
9 P.M . 
•;}9 
•54 
+•15 : 
17 3 
•OH 
■62 
-•4fi 
14. 3 A.M. 
•;{6 
•45 
a > -u 
3000 
•56 
-'44 
9 A.M. 
33 
•45 
+ 12 1 
3 P.M. ...... 
29-99 
•50 
-49 
3 P.M . 
•30 
•40 
+•10 1 
9 P.M . 
•96 
•57 
-•39 
9 P.M . 
•26 
•41 
+•15 ; 
Somewhat similar alternations of pressure were exhibited at the stali« 
Stornoway and Helstoue; in the following Table the altitudes have beenitf 
rented and reduced to the level of the sea. It is to be remarked that durji 
the period of the great wave, the curve at Helstone was altogether 
to that at Ramsgate. 
Table III. 
Barometric altitudes and ditFerenccs observed at Stornoway in the I'aW' 
Isles, and Helstone in Cornwall, during the transit of the Great 
trical Wave of November I8 t6. 
Epoch, Nov. 
HeU 
ltnn9. 
^toriio* 
wny. 
Storiio* 
way ±. 
Epoch, Not. 
Hul- 
bCuDC. 
Storoo* 
WIT. 
StOBW; 
Tffi 
S. 9 A.M . 
29-791 
29-589 
-•202 
10. 3 P.M. 
30-3U> 
30-435 
t+i" 
3 p.u. 
•760 
•579 
-181 
9 P.M . 
•287 
■474 \f"i 
9 P.M.. 
•8.56 
•■439 
-•417 
11. 3 P.M. 
•266 
•497 
3. 9 A.M. 
•891 
•763 
-•128 
9 P.M.. 
•295 
•4.4U 
+-IR» 
+'Jf6 
3 p.u. 
•9.12 
•792 
■743 
-•140 
-•200 
14 (1 . .. 
-.142 
•327 
•547 
9 P.M. 
•943 
3 P.M. 
•SW 
4. 9 A.M. 
29-926 
■711 
— •215 
9 P.M . 
•329 
•538 
+-i« 
xihi 
I-15I 
9 P.M. 
30'084 
•805 
-•279 
13. 3 P.M. 
•254 
•4C7 
5. 3 P.M . 
•002 
•970 
-•032 1 
9 P.M....... 
•289 
■440 
9 p.u. 
■018 
•879 
— •1.19 
14. 9 A.M. 
•198 
■361 
;.i5^ 
6. 9 P.M.. . 
■058 
29’866 
-•192 
3 P.M. 
•156 
•314 
7. 9 A.M . 
■169 
30-017 
-•152 j 
9 P.M.. 
•121 
■310 
+-iw 
I-iti 
3 P.M . 
•195 
•194* 
■209 
•314 
-•OOl ' 
—•010 1 
+•012 ' 
+•045 1 
t ft o « »• 
3(K»21 
29-986 
HH)28 
29-981 
■213 
9 P.M . 
8. 9 A.M. 
■2.H9 
•302 
lift A*m«*»**»« 
3 P.M.' 
9 r 11 
•171 
30-110 
29-873 
Itsfi 
3 P.M. 
•294 
•339 
16. 9 A.M . 
- 1'^ 
...1 
9 P.M....... 
•324 
•340 
+ -01C ' 
3 P.M. 
•885 1 
•765 
9. 9 A.M. 
•319 
•358 
+•019 
9 P.M. ...... 
•825 I 
•631 
_-iw 
3 P.M. ...... 
•335 
•389 
+-(»5J 
17. 9 A.M. 
■706 
•487 
9 P.M. 
•179 
•4<HI 
+-<r»i 
3 P.M.1 
•799 
•413 
10, 9 A.M. 
•331 
•140 
+-H)1» 
9 P.M. 
•869 
•4?4 
Iho curves at Stornoway, the Orknevs, Largs and AppJegarth 
north-western stations, nui nearly together during the whole of their 
•nt^J'Pf'cUons are very numerous; the greatest extent of their direiT^ 
,*fj* ^^nrmg the transit of the first posterior subordinate wave, Stonn’ • 
tlw,/ nl Q* y pressure. The curve at the Orkneys 
t otornoway in the maximum being identical with the crest of the 
* Reading at 4 rjt. 
