31![Chapter 12 Hydrology of the Indian Ocean The distribution of hydrological properties in the Indian Ocean is much less affected by the seasonal monsoon cycle than the near-surface current field. Direct monsoonal influence Chapter 12 Hydrology of the Indian Ocean The distribution of hydrological properties in the Indian Ocean is much less affected by the seasonal monsoon cycle than the near-surface current field. Direct monsoonal influence](https://www.pdfsearch.io/img/f1ef88b2084e051b408f48a1a80788ef.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:30
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32![64 Regional Oceanography: an Introduction 2500 m depth, or 10-30% of the speeds observed at the 500 m level. It is therefore easy to see why the Circumpolar Current has the largest mass transport of all ocean current
64 Regional Oceanography: an Introduction 2500 m depth, or 10-30% of the speeds observed at the 500 m level. It is therefore easy to see why the Circumpolar Current has the largest mass transport of all ocean current](https://www.pdfsearch.io/img/3a810bdbcbc2d5c500a814e9a0cf14e3.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:18
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33![Chapter 9 Hydrology of the Pacific Ocean The preceding chapter presented the currents of the Pacific Ocean essentially as winddriven and treated temperature, salinity and other hydrographic properties as passive tracers, Chapter 9 Hydrology of the Pacific Ocean The preceding chapter presented the currents of the Pacific Ocean essentially as winddriven and treated temperature, salinity and other hydrographic properties as passive tracers,](https://www.pdfsearch.io/img/a2727f383cf1595830b6ff64ff49ef49.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:29
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34![doi:[removed]j.dsr[removed] doi:[removed]j.dsr[removed]](https://www.pdfsearch.io/img/71683edf5c63032ee23203e4945832dd.jpg) | Add to Reading ListSource URL: www.aoml.noaa.govLanguage: English - Date: 2010-03-31 13:42:33
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35![138 Regional Oceanography: an Introduction A characteristic feature of the South Pacific Ocean is the existence of a second region of wind convergence in the tropics known as the South Pacific Convergence Zone or SPCZ.
138 Regional Oceanography: an Introduction A characteristic feature of the South Pacific Ocean is the existence of a second region of wind convergence in the tropics known as the South Pacific Convergence Zone or SPCZ.](https://www.pdfsearch.io/img/461375c93c4634d0821b814b00e258fd.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:20
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36![254 Regional Oceanography: an Introduction Sea surface temperature and salinity As noted earlier, the map of sea surface salinity (SSS; Figure 2.5b) resembles the P-E
254 Regional Oceanography: an Introduction Sea surface temperature and salinity As noted earlier, the map of sea surface salinity (SSS; Figure 2.5b) resembles the P-E](https://www.pdfsearch.io/img/a8834e643e0fcd972cfe3553813c139f.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:16
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37![Chapter 12 Hydrology of the Indian Ocean The distribution of hydrological properties in the Indian Ocean is much less affected by the seasonal monsoon cycle than the near-surface current field. Direct monsoonal influence Chapter 12 Hydrology of the Indian Ocean The distribution of hydrological properties in the Indian Ocean is much less affected by the seasonal monsoon cycle than the near-surface current field. Direct monsoonal influence](https://www.pdfsearch.io/img/cc5f17ca08ac731930155132f0ffb6f3.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:14
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38![Chapter 15 Hydrology of the Atlantic Ocean The hydrology of the Atlantic Ocean basins is deeply affected by the formation and recirculation of North Atlantic Deep Water, which was discussed in Chapter 7. The injection of Chapter 15 Hydrology of the Atlantic Ocean The hydrology of the Atlantic Ocean basins is deeply affected by the formation and recirculation of North Atlantic Deep Water, which was discussed in Chapter 7. The injection of](https://www.pdfsearch.io/img/9c3e471255ce494004dfa4cfb3446ca8.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:06
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39![Journal of Marine Research, 59, 281–312, 2001 New observations of the intermediate depth circulation in the tropical Atlantic by Claudia Schmid1 ,2 , Robert L. Molinari2 and Silvia L. Garzoli2 ABSTRACT Journal of Marine Research, 59, 281–312, 2001 New observations of the intermediate depth circulation in the tropical Atlantic by Claudia Schmid1 ,2 , Robert L. Molinari2 and Silvia L. Garzoli2 ABSTRACT](https://www.pdfsearch.io/img/fc531ed3802aa3d2510c95cc82771638.jpg) | Add to Reading ListSource URL: www.aoml.noaa.govLanguage: English - Date: 2009-10-07 13:47:02
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40![Chapter 15 Hydrology of the Atlantic Ocean The hydrology of the Atlantic Ocean basins is deeply affected by the formation and recirculation of North Atlantic Deep Water, which was discussed in Chapter 7. The injection of Chapter 15 Hydrology of the Atlantic Ocean The hydrology of the Atlantic Ocean basins is deeply affected by the formation and recirculation of North Atlantic Deep Water, which was discussed in Chapter 7. The injection of](https://www.pdfsearch.io/img/d0cd1e10270c782b50465bda0ad5b1bc.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:23
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