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101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

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

Language: English - Date: 2006-08-17 03:26:09
102Chapter 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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Source URL: gaea.es.flinders.edu.au

Language: English - Date: 2006-08-17 03:26:15
103Chapter 6 Antarctic oceanography The region of the world ocean bordering on Antarctica is unique in many respects. First of all, it is the only region where the flow of water can continue all around the globe nearly unhi

Chapter 6 Antarctic oceanography The region of the world ocean bordering on Antarctica is unique in many respects. First of all, it is the only region where the flow of water can continue all around the globe nearly unhi

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

Language: English - Date: 2006-08-17 03:26:19
10484  Regional Oceanography: an Introduction where the density of the oceanic water matches its own; it then spreads on this density surface, where it can be traced through the ocean basin by its high salinity. (A promine

84 Regional Oceanography: an Introduction where the density of the oceanic water matches its own; it then spreads on this density surface, where it can be traced through the ocean basin by its high salinity. (A promine

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

Language: English - Date: 2006-08-17 03:26:19
105Chapter 6 Antarctic oceanography The region of the world ocean bordering on Antarctica is unique in many respects. First of all, it is the only region where the flow of water can continue all around the globe nearly unhi

Chapter 6 Antarctic oceanography The region of the world ocean bordering on Antarctica is unique in many respects. First of all, it is the only region where the flow of water can continue all around the globe nearly unhi

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

Language: English - Date: 2006-08-17 03:26:21
106Chapter 8 The Pacific Ocean After these two lengthy excursions into polar oceanography we are now ready to test our understanding of ocean dynamics by looking at one of the three major ocean basins. The Pacific Ocean is

Chapter 8 The Pacific Ocean After these two lengthy excursions into polar oceanography we are now ready to test our understanding of ocean dynamics by looking at one of the three major ocean basins. The Pacific Ocean is

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

Language: English - Date: 2006-08-17 03:26:12
107Chapter 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

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Language: English - Date: 2006-08-17 03:26:30
108Glossary  379 Glossary anti-cyclonic

Glossary 379 Glossary anti-cyclonic

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Language: English - Date: 2006-08-17 03:26:17
109pdf version 1.0 (December 2001)  pdf version 1.1 (May 2002) Preface to the first[removed]edition: This book developed from lectures for undergraduate students of marine sciences in

pdf version 1.0 (December 2001) pdf version 1.1 (May 2002) Preface to the first[removed]edition: This book developed from lectures for undergraduate students of marine sciences in

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Language: English - Date: 2006-08-17 03:26:18
110Chapter 5 Water mass formation, subduction, and the oceanic heat budget In the first four chapters we developed the concept of Ekman pumping, Rossby wave propagation, and the Sverdrup circulation as the steady-state bala

Chapter 5 Water mass formation, subduction, and the oceanic heat budget In the first four chapters we developed the concept of Ekman pumping, Rossby wave propagation, and the Sverdrup circulation as the steady-state bala

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

Language: English - Date: 2006-08-17 03:26:14