Surface circulation and transport in the mozambique channel
Surface circulation and transport in the Mozambique Channel have been determined using altimetry and the hydrographic section along 25 S covered during the World Ocean Circulation Experiment. Vertical sections of potential temperature and salinity are prepared to understand the water characteristics...
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| Format: | Article |
| Language: | English |
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Faculty of Geoinformation Science and Engineering, Universiti Teknologi Malaysia,
2010-12.
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| Online Access: | Get fulltext Get fulltext |
| LEADER | 01569 am a22001693u 4500 | ||
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| 001 | 27790 | ||
| 042 | |a dc | ||
| 100 | 1 | 0 | |a Peter, Benny N. |e author |
| 700 | 1 | 0 | |a Ses, Sahrum |e author |
| 245 | 0 | 0 | |a Surface circulation and transport in the mozambique channel |
| 260 | |b Faculty of Geoinformation Science and Engineering, Universiti Teknologi Malaysia, |c 2010-12. | ||
| 856 | |z Get fulltext |u http://eprints.utm.my/id/eprint/27790/2/ShahrumSes2010_SurfaceCirculationandTransportintheMozambiqueChannel.pdf | ||
| 856 | |z Get fulltext |u http://eprints.utm.my/id/eprint/27790/3/4-surface%20circulation%20and%20transport%20in%20the.pdf | ||
| 520 | |a Surface circulation and transport in the Mozambique Channel have been determined using altimetry and the hydrographic section along 25 S covered during the World Ocean Circulation Experiment. Vertical sections of potential temperature and salinity are prepared to understand the water characteristics. The meridional component of geostrophic velocity is computed referring to the deepest common depth between stations. The mean circulation field exhibits the strong Mozambique current in the northern part of the Channel. But, it is weakened and embedded with anticyclonic eddies towards south. The geostrophic flow reveals the eddy circulation in the Mozambique Channel. The meridional volume and heat transports have been estimated and presented with respect longitude. Both the net volume transport and the heat transport are towards south and are 22.8 Sv and 0.7 pw respectively. | ||
| 546 | |a en | ||
| 546 | |a en | ||
| 650 | 0 | 4 | |a G Geography (General) |