Gaea

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51 380 Regional Oceanography: an Introduction isohalines isopycnals

380 Regional Oceanography: an Introduction isohalines isopycnals

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Source URL: gaea.es.flinders.edu.au

- Date: 2006-08-17 03:26:17
    52 366 Regional Oceanography: an Introduction Camden-Smith, F., L.-A. Perrins, R. V. Dingle and G. B. BrunditA preliminary report on long-term bottom-current measurements and sediment transport/erosion in

    366 Regional Oceanography: an Introduction Camden-Smith, F., L.-A. Perrins, R. V. Dingle and G. B. BrunditA preliminary report on long-term bottom-current measurements and sediment transport/erosion in

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    Source URL: gaea.es.flinders.edu.au

    - Date: 2006-08-17 03:26:06
      53Chapter 13 Adjacent seas of the Indian Ocean and the Australasian Mediterranean S e a (the Indonesian throughflow) Being the smallest of all oceans, the Indian Ocean does not have the large number of distinct subregions

      Chapter 13 Adjacent seas of the Indian Ocean and the Australasian Mediterranean S e a (the Indonesian throughflow) Being the smallest of all oceans, the Indian Ocean does not have the large number of distinct subregions

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      - Date: 2006-08-17 03:26:25
        54Chapter 14 The Atlantic Ocean A glance at the distribution of high quality ocean data (Figure 2.3) tells us that the Atlantic Ocean is by far the best researched part of the world ocean. This is particularly true of the

        Chapter 14 The Atlantic Ocean A glance at the distribution of high quality ocean data (Figure 2.3) tells us that the Atlantic Ocean is by far the best researched part of the world ocean. This is particularly true of the

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        - Date: 2006-08-17 03:26:28
          55 16 Regional Oceanography: an Introduction salinometers, which compare water samples from CTD stations with a seawater standard of known salinity (for details see Dietrich et al., A CTD is therefore usually house

          16 Regional Oceanography: an Introduction salinometers, which compare water samples from CTD stations with a seawater standard of known salinity (for details see Dietrich et al., A CTD is therefore usually house

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          - Date: 2006-08-17 03:26:06
            56Chapter 1 Introduction: What drives the ocean currents? Sixty years ago, this textbook would have been titled

            Chapter 1 Introduction: What drives the ocean currents? Sixty years ago, this textbook would have been titled "Introductory Geography of the Oceans". Physical oceanography then was a close relative of physical geography

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            Language: English - Date: 2006-08-17 03:26:26
              57INDEX The following abbreviations are used in this index: WO = World Ocean, AO = Atlantic Ocean, IO = Indian Ocean, PO = Pacific Ocean, Med = Mediterranean, C = Current. Adélie coast 79,80

              INDEX The following abbreviations are used in this index: WO = World Ocean, AO = Atlantic Ocean, IO = Indian Ocean, PO = Pacific Ocean, Med = Mediterranean, C = Current. Adélie coast 79,80

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              Source URL: gaea.es.flinders.edu.au

              Language: English - Date: 2006-08-17 03:26:22
                58INDEX The following abbreviations are used in this index: WO = World Ocean, AO = Atlantic Ocean, IO = Indian Ocean, PO = Pacific Ocean, Med = Mediterranean, C = Current. Adélie coast 79,80

                INDEX The following abbreviations are used in this index: WO = World Ocean, AO = Atlantic Ocean, IO = Indian Ocean, PO = Pacific Ocean, Med = Mediterranean, C = Current. Adélie coast 79,80

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                Language: English - Date: 2006-08-17 03:26:16
                  59 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

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                  Language: English - Date: 2006-08-17 03:26:18
                    60Chapter 19 El Niño and the Southern Oscillation (ENSO) The previous chapter stressed the importance of the tropics for the coupling between ocean and atmosphere and showed how positive feedback between the sea surface t

                    Chapter 19 El Niño and the Southern Oscillation (ENSO) The previous chapter stressed the importance of the tropics for the coupling between ocean and atmosphere and showed how positive feedback between the sea surface t

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                    Source URL: gaea.es.flinders.edu.au

                    Language: English - Date: 2006-08-17 03:26:24