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](https://www.pdfsearch.io/img/6daebea13b09c5371292274399ddc030.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:09
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102![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 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](https://www.pdfsearch.io/img/fb2adb32ae3c798fb24ea87e33216c5b.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:15
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103![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 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](https://www.pdfsearch.io/img/6d85b11f2de0e0a3c45de7ac8c6c9c57.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:19
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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](https://www.pdfsearch.io/img/47539e19c5dc731d243ff87803be6fbd.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:19
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105![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 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](https://www.pdfsearch.io/img/0fc6f9aa8eb8ef89a24c38ccc098800c.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:21
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106![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 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](https://www.pdfsearch.io/img/07dc83b4feab196b2d02c4c3cec4599b.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:12
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107![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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108![Glossary 379 Glossary anti-cyclonic Glossary 379 Glossary anti-cyclonic](https://www.pdfsearch.io/img/aa277231be3c4ccc15d9b39adc0c9f74.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:17
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109![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 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](https://www.pdfsearch.io/img/d62b55cf2a18c0e25b970bbc7c7f3ab3.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:18
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110![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 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](https://www.pdfsearch.io/img/ee00a96c87bd2c480866264e4cc7bbd8.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:14
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