Deep ocean circulation by acoustic-gravity waves: from snowball to greenhouse earth

Kadri, Usama ORCID: https://orcid.org/0000-0002-5441-1812 2015. Deep ocean circulation by acoustic-gravity waves: from snowball to greenhouse earth. Presented at: European Geosciences Union General Assembly 2015, Vienna, Austria, 12-17 April 2015. Geophysical Research Abstracts. , vol.17 European Geosciences Union, p. 2559.

Full text not available from this repository.

Abstract

Acoustic-gravity waves are compression-type waves propagating with amplitudes governed by the restoring force of gravity. They are generated, among others, by wind-wave interactions, surface waves interactions, submarine earthquakes, and movements of ice-blocks. We show that acoustic-gravity waves contribute to deep ocean water transport through different climate timelines: from snowball to greenhouse earth; they cause chaotic flow trajecto- ries of individual water parcels, which can be transported up to a few centimetres per second.

Item Type:	Conference or Workshop Item (Poster)
Status:	Published
Schools:	Mathematics
Publisher:	European Geosciences Union
ISSN:	1029-7006
Last Modified:	01 Nov 2022 11:39
URI:	https://orca.cardiff.ac.uk/id/eprint/95735

Actions (repository staff only)

Edit Item