Skip to content

Please be aware that some material may contain words, descriptions or illustrations which will not reflect current scientific understanding and may be considered in today's context inaccurate, unethical, offensive or distressing.

Description

Strachey writes of a paper by Robert Henry Scott (see PP/4/9): 'The obvious correspondence of the forms and times of occurrence of the barometric disturbances, described in Mr Scott’s paper, at once suggested that they were due to a common origin, and the great volcanic eruption at Krakatoa in the Straits of Sunda appeared to supply a probable efficient cause. Any shock of sufficient violence might be expected to produce an atmospheric wave, advancing from the place where it was caused in a circular form round the globe, at first expanding until it had got half round the earth, and then again contracting till it was again concentrated at the antipodes, from which again it would be thrown, back, and so pass backwards and forwards till it was obliterated. It might also have been expected that such a wave would travel with the velocity of sound, being probably of the same nature as that which causes sound, though the vibrations had not the peculiar character that affects our organs of hearing. It has, however, been suggested to me that the wave may rather have had the character of a solitary wave produced in a liquid, the velocity of which in the air would not materially differ from that of sound. A rough examination of the facts at first made known by the observations recorded in Great Britain indicated that there was primâ facie strong evidence in support of this view, and that the phenomena would be approximately explained by the passage round the earth of a series of waves travelling at the rate of about 700 miles an hour in opposite directions from the place where the volcanic eruption occurred. The records since procured from other places, and the more careful examination of the facts, has quite confirmed this conclusion.'

Annotations in pencil and ink.

Subject: Meteorology

Received 12 December 1883. Read 13 December 1883.

A version of this paper was published in volume 36 of the Proceedings of the Royal Society as 'Note on the foregoing paper'.

Reference number
PP/4/10
Earliest possible date
1883
Physical description
Ink and graphite pencil on paper
Page extent
17 pages
Format
Manuscript

Creator name

Richard Strachey

View page for Richard Strachey

Use this record

Citation

Richard Strachey, Paper, 'Note on the foregoing paper' by R [Richard] Strachey, 1883, PP/4/10, The Royal Society Archives, London, https://makingscience.royalsociety.org/items/pp_4_10/paper-note-on-the-foregoing-paper-by-r-richard-strachey, accessed on 05 October 2024

Link to this record

Embed this record

<iframe src="https://makingscience.royalsociety.org/embed/items/pp_4_10/paper-note-on-the-foregoing-paper-by-r-richard-strachey" title="Paper, 'Note on the foregoing paper' by R [Richard] Strachey" allow="fullscreen" frameborder="0" width="100%" height="500px"></iframe>

Related Publications

Hierarchy

This item is part of:

Related Fellows

Explore the collection

  • Proceedings Papers

    Dates: 1882 - 1894

    The archival collection known as 'Proceedings Papers' is comprised of manuscripts and occasional proofs of scientific papers sent to the Royal Society which were read before meetings of Fellows and printed in full in the Proceedings of the Royal Society.

    View collection