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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 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 Add to Reading List Source URL: gaea.es.flinders.edu.au Language: English - Date: 2006-08-17 03:26:07
63	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
64	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
65	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
66	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 Add to Reading List Source URL: gaea.es.flinders.edu.au Language: English - Date: 2006-08-17 03:26:10
68	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. Add to Reading List Source URL: gaea.es.flinders.edu.au Language: English - Date: 2006-08-17 03:26:11
70	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

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