111![Glossary 379 Glossary anti-cyclonic Glossary 379 Glossary anti-cyclonic](https://www.pdfsearch.io/img/a1ae47be042af81d0e68d1d2e5d97448.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:24
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112![References Aagaard, K. and P. Greisman[removed]Towards new mass and heat budgets for the Arctic ocean. Journal of Geophysical Research 80, [removed]Aagaard, K., L. K. Coachman and E. C. Carmack[removed]On the halocline o References Aagaard, K. and P. Greisman[removed]Towards new mass and heat budgets for the Arctic ocean. Journal of Geophysical Research 80, [removed]Aagaard, K., L. K. Coachman and E. C. Carmack[removed]On the halocline o](https://www.pdfsearch.io/img/fb1bd765faef914f15e47bf6927dd61a.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:07
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113![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 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](https://www.pdfsearch.io/img/38a47131a6a94d8e5ee0b0e15004b779.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:27
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114![176 Regional Oceanography: an Introduction Fig[removed]Topography of the Indian Ocean. The 1000, 3000, and 5000 m isobaths are shown, and regions less than 3000 m deep are shaded. South of Australia the Indian Ocean ext
176 Regional Oceanography: an Introduction Fig[removed]Topography of the Indian Ocean. The 1000, 3000, and 5000 m isobaths are shown, and regions less than 3000 m deep are shaded. South of Australia the Indian Ocean ext](https://www.pdfsearch.io/img/4411d667dcbad38c3f9b62269dc253af.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-12-20 22:45:35
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115![Chapter 11 The Indian Ocean We now turn to the Indian Ocean, which is in several respects very different from the Pacific Ocean. The most striking difference is the seasonal reversal of the monsoon winds and its effects Chapter 11 The Indian Ocean We now turn to the Indian Ocean, which is in several respects very different from the Pacific Ocean. The most striking difference is the seasonal reversal of the monsoon winds and its effects](https://www.pdfsearch.io/img/d9b8b8f8e2366751b8bdeb0effe8a7d6.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-12-20 22:44:55
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116![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 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](https://www.pdfsearch.io/img/44167cd65697b6c835577ec2c24dc249.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:12
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117![300 Regional Oceanography: an Introduction Strait the same process operates in that region as well, and the mixed layer temperature in both regions is the same. When that depth is reached, Bass Strait Water cools faste
300 Regional Oceanography: an Introduction Strait the same process operates in that region as well, and the mixed layer temperature in both regions is the same. When that depth is reached, Bass Strait Water cools faste](https://www.pdfsearch.io/img/86d39cf2fe700016b4b0d48138468d95.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:12
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118![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 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](https://www.pdfsearch.io/img/a52ef632e85b27b3b85a8121706be6b2.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:13
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119![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 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](https://www.pdfsearch.io/img/76c50c93f7bb054400eae00ab0461e35.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:28
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120![Chapter 7 Arctic oceanography; the path of North Atlantic Deep Water The importance of the Southern Ocean for the formation of the water masses of the world ocean poses the question whether similar conditions are found i Chapter 7 Arctic oceanography; the path of North Atlantic Deep Water The importance of the Southern Ocean for the formation of the water masses of the world ocean poses the question whether similar conditions are found i](https://www.pdfsearch.io/img/6dc709ed76f198d1f9b15c5b9fba201c.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:19
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