121![312 Regional Oceanography: an Introduction Fig[removed]Annual mean equilibrium surface temperature (°C) for the world ocean. This is the temperature the sea surface would have if the heat budget were locally balanced a
312 Regional Oceanography: an Introduction Fig[removed]Annual mean equilibrium surface temperature (°C) for the world ocean. This is the temperature the sea surface would have if the heat budget were locally balanced a](https://www.pdfsearch.io/img/208df23dfd5e9ed2cf9159472c4ec549.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:08
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122![106 Regional Oceanography: an Introduction All adjacent seas of the Pacific Ocean are grouped along its west coast. Some of them (such as the Arafura and East China Seas) are large shelf seas, others (e.g. the Solomon
106 Regional Oceanography: an Introduction All adjacent seas of the Pacific Ocean are grouped along its west coast. Some of them (such as the Arafura and East China Seas) are large shelf seas, others (e.g. the Solomon](https://www.pdfsearch.io/img/16cefff0935686eda4047198c9a6e5a5.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:16
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123![64 Regional Oceanography: an Introduction 2500 m depth, or 10-30% of the speeds observed at the 500 m level. It is therefore easy to see why the Circumpolar Current has the largest mass transport of all ocean current
64 Regional Oceanography: an Introduction 2500 m depth, or 10-30% of the speeds observed at the 500 m level. It is therefore easy to see why the Circumpolar Current has the largest mass transport of all ocean current](https://www.pdfsearch.io/img/3a810bdbcbc2d5c500a814e9a0cf14e3.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:18
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124![52 Regional Oceanography: an Introduction combine water mass analysis with our knowledge of the constraints on possible flows posed by geostrophy and Ekman dynamics. This approach, which infers water movement
52 Regional Oceanography: an Introduction combine water mass analysis with our knowledge of the constraints on possible flows posed by geostrophy and Ekman dynamics. This approach, which infers water movement](https://www.pdfsearch.io/img/48f3edc0cb088d1f9b7f71fed0fd549e.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:10
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125![380 Regional Oceanography: an Introduction isohalines isopycnals
380 Regional Oceanography: an Introduction isohalines isopycnals](https://www.pdfsearch.io/img/2b841c926d730a4d8f7bc5005a101c14.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:17
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126![Chapter 20 The ocean and climate change In this final chapter we turn from the short-term climate variability of ENSO to consider variations with timescales of several decades or more. Small but persistent changes in cli Chapter 20 The ocean and climate change In this final chapter we turn from the short-term climate variability of ENSO to consider variations with timescales of several decades or more. Small but persistent changes in cli](https://www.pdfsearch.io/img/ae6bd8aeb05e9bb7101bc835f68a9b11.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:10
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127![30 Regional Oceanography: an Introduction into account in the balance of forces. The Coriolis force is proportional in magnitude to the flow speed and directed perpendicular to the direction of the flow. It acts to the
30 Regional Oceanography: an Introduction into account in the balance of forces. The Coriolis force is proportional in magnitude to the flow speed and directed perpendicular to the direction of the flow. It acts to the](https://www.pdfsearch.io/img/3f33c1480a055021319acfd1302b588c.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:06
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128![Chapter 9 Hydrology of the Pacific Ocean The preceding chapter presented the currents of the Pacific Ocean essentially as winddriven and treated temperature, salinity and other hydrographic properties as passive tracers, Chapter 9 Hydrology of the Pacific Ocean The preceding chapter presented the currents of the Pacific Ocean essentially as winddriven and treated temperature, salinity and other hydrographic properties as passive tracers,](https://www.pdfsearch.io/img/a2727f383cf1595830b6ff64ff49ef49.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:29
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129![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/a24c3f033e0c9d87404952a836d00c00.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:18
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130![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 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](https://www.pdfsearch.io/img/cfc7488f09b2c2b03b1df5a2aa0f3fec.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:22
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