Date.Aurora.Ozone.
1870,October14th.Aurora.8The display of the 24th was accompanied by the formation of a corona, and that of the 25th was splendidly seen in Edinburgh.
20th.Aurora.10
21st.None seen.5
22nd.Aurora.10
23rd.None seen.8
24th.Aurora.10
25th.Aurora.8

The foregoing figures somewhat point to the conclusion that ozone quantity rises and falls coincidently with the Aurora displays.

The following seems, however, a case still more strongly in point.

Date.Wind.Aurora.Ozone.
1871,January25th.E.S.E.None seen.0
26th.N.N.W.None seen.2
27th.E.S.E.Aurora at night in N. and S. horizons.10
28th.E.None seen.8
29th.S.E.None seen.2

It is curious, in examining the above Table, to note how the ozone rose, notwithstanding an east wind, from 0 on the 25th, and 2 on the 26th, to 10 on the 27th, when the Aurora appeared, and 8 on the 28th, when it might have lingered; and how it again descended to 2 on the 29th.

The case of the Aurora of 6th of October, 1869, when a broad belt of Aurora was in the north, is also an illustrative one, as will be seen by the following data:—

Date.Wind.Ozone.Aurora.
1869,October5th.S.S.W.1
6th.S.S.E.5Aurora.
7th.S.S.W.10
8th.S.10
9th.S.E.5

The Aurora of the night of the 6th was here represented by the ozone-paper of the morning of the 7th with a maximum of 10, which lasted till the 8th.

[It should be borne in mind, in examining these Tables, that the Aurora is of the night of the given date, while the ozone-papers are taken and recorded in the morning of the date quoted.]