Madagascar: A pacemaker for the Agulhas Current system?
| dc.contributor.author | Penven, P | |
| dc.contributor.author | Lutjeharms, J R E | |
| dc.contributor.author | Florenchie, P | |
| dc.date.accessioned | 2021-10-08T07:04:07Z | |
| dc.date.available | 2021-10-08T07:04:07Z | |
| dc.date.issued | 2006 | |
| dc.description.abstract | [1] Western boundary currents are driven by zonally integrated wind-stress curl over the width of subtropical basins. This cross-basin integration is interrupted in the South Indian Ocean where Madagascar presents a formidable barrier. Nevertheless, a western boundary current has been thought to exist in the Mozambique Channel, the Mozambique Current. Recent observations have however shown that no such current exists and that the flow in the channel instead consists of a train of eddies. Is this western boundary anomaly due to the presence of Madagascar? We have used a primitive equations model to investigate the flow in the South West Indian Ocean as if there were no Madagascar. We show that a normal, continuous western boundary current is then formed that constitutes a continuum with the Agulhas Current. The presence of Madagascar is shown to affect the frequency of inter-ocean exchange events south of Africa. | |
| dc.identifier.apacitation | Penven, P., Lutjeharms, J. R. E., & Florenchie, P. (2006). Madagascar: A pacemaker for the Agulhas Current system?. <i>Geophysical Research Letters</i>, 33(17), 174 - 177. http://hdl.handle.net/11427/34430 | en_ZA |
| dc.identifier.chicagocitation | Penven, P, J R E Lutjeharms, and P Florenchie "Madagascar: A pacemaker for the Agulhas Current system?." <i>Geophysical Research Letters</i> 33, 17. (2006): 174 - 177. http://hdl.handle.net/11427/34430 | en_ZA |
| dc.identifier.citation | Penven, P., Lutjeharms, J.R.E. & Florenchie, P. 2006. Madagascar: A pacemaker for the Agulhas Current system?. <i>Geophysical Research Letters.</i> 33(17):174 - 177. http://hdl.handle.net/11427/34430 | en_ZA |
| dc.identifier.issn | 0094-8276 | |
| dc.identifier.issn | 1944-8007 | |
| dc.identifier.ris | TY - Journal Article AU - Penven, P AU - Lutjeharms, J R E AU - Florenchie, P AB - [1] Western boundary currents are driven by zonally integrated wind-stress curl over the width of subtropical basins. This cross-basin integration is interrupted in the South Indian Ocean where Madagascar presents a formidable barrier. Nevertheless, a western boundary current has been thought to exist in the Mozambique Channel, the Mozambique Current. Recent observations have however shown that no such current exists and that the flow in the channel instead consists of a train of eddies. Is this western boundary anomaly due to the presence of Madagascar? We have used a primitive equations model to investigate the flow in the South West Indian Ocean as if there were no Madagascar. We show that a normal, continuous western boundary current is then formed that constitutes a continuum with the Agulhas Current. The presence of Madagascar is shown to affect the frequency of inter-ocean exchange events south of Africa. DA - 2006 DB - OpenUCT DP - University of Cape Town IS - 17 J1 - Geophysical Research Letters LK - https://open.uct.ac.za PY - 2006 SM - 0094-8276 SM - 1944-8007 T1 - Madagascar: A pacemaker for the Agulhas Current system? TI - Madagascar: A pacemaker for the Agulhas Current system? UR - http://hdl.handle.net/11427/34430 ER - | en_ZA |
| dc.identifier.uri | http://hdl.handle.net/11427/34430 | |
| dc.identifier.vancouvercitation | Penven P, Lutjeharms JRE, Florenchie P. Madagascar: A pacemaker for the Agulhas Current system?. Geophysical Research Letters. 2006;33(17):174 - 177. http://hdl.handle.net/11427/34430. | en_ZA |
| dc.language.iso | eng | |
| dc.publisher.department | Department of Oceanography | |
| dc.publisher.faculty | Faculty of Science | |
| dc.source | Geophysical Research Letters | |
| dc.source.journalissue | 17 | |
| dc.source.journalvolume | 33 | |
| dc.source.pagination | 174 - 177 | |
| dc.source.uri | https://dx.doi.org/10.1029/2006GL026854 | |
| dc.subject.other | Africa | |
| dc.subject.other | frequency | |
| dc.subject.other | Continuum | |
| dc.subject.other | models | |
| dc.subject.other | Primitive equation | |
| dc.subject.other | anomalies | |
| dc.subject.other | Vortex | |
| dc.subject.other | channels | |
| dc.subject.other | Indian Ocean | |
| dc.subject.other | Wind effect | |
| dc.subject.other | Western boundary current | |
| dc.subject.other | West Indian Ocean | |
| dc.subject.other | Mozambique | |
| dc.subject.other | Mozambique Channel | |
| dc.subject.other | Agulhas current | |
| dc.subject.other | Madagascar | |
| dc.subject.other | East Africa | |
| dc.subject.other | Indian Ocean Islands | |
| dc.subject.other | Afrique | |
| dc.subject.other | Fréquence | |
| dc.subject.other | Modèle | |
| dc.subject.other | Equation primitive | |
| dc.subject.other | Anomalie | |
| dc.subject.other | Tourbillon | |
| dc.subject.other | Chenal | |
| dc.subject.other | Océan Indien | |
| dc.subject.other | Action vent | |
| dc.title | Madagascar: A pacemaker for the Agulhas Current system? | |
| dc.type | Journal Article | |
| uct.type.publication | Research | |
| uct.type.resource | Journal Article |
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