Gaea

Results: 188



#Item
61 330 Regional Oceanography: an Introduction are only a poor indicator for this; dollar values and variations of gross national product do not convey the amount of human suffering behind them. But they indicate the magni

330 Regional Oceanography: an Introduction are only a poor indicator for this; dollar values and variations of gross national product do not convey the amount of human suffering behind them. But they indicate the magni

Add to Reading List

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

Language: English - Date: 2006-08-17 03:26:09
    62 216 Regional Oceanography: an Introduction during summer), are a period of active convection. Which of the two regions

    216 Regional Oceanography: an Introduction during summer), are a period of active convection. Which of the two regions

    Add to Reading List

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

    Language: English - Date: 2006-08-17 03:26:07
      63INDEX 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

      Add to Reading List

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

      Language: English - Date: 2006-08-17 03:26:13
        64Chapter 16 Adjacent seas of the Atlantic Ocean The hydrography of the Atlantic Ocean is strongly influenced by its adjacent seas, to the degree that a discussion of this ocean would be incomplete without a description of

        Chapter 16 Adjacent seas of the Atlantic Ocean The hydrography of the Atlantic Ocean is strongly influenced by its adjacent seas, to the degree that a discussion of this ocean would be incomplete without a description of

        Add to Reading List

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

        Language: English - Date: 2006-08-17 03:26:13
          65Chapter 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

          Add to Reading List

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

          Language: English - Date: 2006-08-17 03:26:30
            66shown in Figure 9.10, which also includes the area where the salinity is above 36 at 200 m depth. It is seen that the high salinities reach much further west in the thermocline than at the sea surface. The origin of thes

            shown in Figure 9.10, which also includes the area where the salinity is above 36 at 200 m depth. It is seen that the high salinities reach much further west in the thermocline than at the sea surface. The origin of thes

            Add to Reading List

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

            Language: English - Date: 2006-08-17 03:26:06
              67 40 Regional Oceanography: an Introduction our Rule 1 we note here again that our rules are not applicable near the equator, where according to eqnEkman layer transport grows beyond all bounds. In practical

              40 Regional Oceanography: an Introduction our Rule 1 we note here again that our rules are not applicable near the equator, where according to eqnEkman layer transport grows beyond all bounds. In practical

              Add to Reading List

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

              Language: English - Date: 2006-08-17 03:26:10
                68Chapter 3 The Coriolis force, intensification geostrophy,

                Chapter 3 The Coriolis force, intensification geostrophy,

                Add to Reading List

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

                Language: English - Date: 2006-08-17 03:26:21
                  69 272 Regional Oceanography: an Introduction FigGeography and circulation of the Northwest Passage and connected seas.

                  272 Regional Oceanography: an Introduction FigGeography and circulation of the Northwest Passage and connected seas.

                  Add to Reading List

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

                  Language: English - Date: 2006-08-17 03:26:11
                    70Chapter 4 Ekman layer transports, Ekman pumping, and the Sverdrup balance Geostrophic flow, or the flow produced by a balance between the pressure gradient force and the Coriolis force, is frictionless flow. But momentum

                    Chapter 4 Ekman layer transports, Ekman pumping, and the Sverdrup balance Geostrophic flow, or the flow produced by a balance between the pressure gradient force and the Coriolis force, is frictionless flow. But momentum

                    Add to Reading List

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

                    Language: English - Date: 2006-08-17 03:26:18