1![OCTOBERDIJKSTRA AND DE RUIJTER OCTOBERDIJKSTRA AND DE RUIJTER](https://www.pdfsearch.io/img/a6a93bfa53262b357fa204ae957985c0.jpg) | Add to Reading ListSource URL: www.staff.science.uu.nlLanguage: English - Date: 2011-05-16 11:51:24
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2![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/958290c38327c900b3d9675c5e79de04.jpg) | Add to Reading ListSource URL: gaea.es.flinders.edu.auLanguage: English - Date: 2006-08-17 03:26:18
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3![egu_logo_without_circle_grey egu_logo_without_circle_grey](https://www.pdfsearch.io/img/21ec660d0b305f44cd748bc9ce58cd3f.jpg) | Add to Reading ListSource URL: www.ocean-sci.netLanguage: English - Date: 2014-12-03 11:26:42
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4![JOURNALOF GEOPHYSICALRESEARCH,VOL. 96, NO. C10,PAGES18,509-18,518, OCTOBER15, 1991 A DiagnosticStudy of the Wind- and Buoyancy-Driven North JOURNALOF GEOPHYSICALRESEARCH,VOL. 96, NO. C10,PAGES18,509-18,518, OCTOBER15, 1991 A DiagnosticStudy of the Wind- and Buoyancy-Driven North](https://www.pdfsearch.io/img/102d6e0fe79685db77618ea4938081e7.jpg) | Add to Reading ListSource URL: www.whoi.eduLanguage: English - Date: 2009-07-22 14:08:01
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5![AUGUSTSPALL AND PICKART 1829 AUGUSTSPALL AND PICKART 1829](https://www.pdfsearch.io/img/582b8e83fd1558d42fbd965080d29b12.jpg) | Add to Reading ListSource URL: www.whoi.eduLanguage: English - Date: 2003-11-06 10:00:28
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6![](https://www.pdfsearch.io/img/7fb81226c72341b21dca669199149117.jpg) | Add to Reading ListSource URL: faculty.washington.eduLanguage: English - Date: 2006-02-13 16:38:42
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7![The Sverdrup Balance The steady, linear vorticity equation was found to be (2) The Sverdrup balance 3V = Curl()), where upper case symbols indicate depth-integrated velocities, is obtained by The Sverdrup Balance The steady, linear vorticity equation was found to be (2) The Sverdrup balance 3V = Curl()), where upper case symbols indicate depth-integrated velocities, is obtained by](https://www.pdfsearch.io/img/6933066cfed9709e06ca9bacbecae230.jpg) | Add to Reading ListSource URL: faculty.washington.edu- Date: 2001-01-30 23:48:09
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8![994 JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 33 994 JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 33](https://www.pdfsearch.io/img/943a953a1e79ab49a54105cea561f938.jpg) | Add to Reading ListSource URL: faculty.washington.eduLanguage: English - Date: 2003-04-28 16:20:15
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9![SEPTEMBERKESSLER 2457 SEPTEMBERKESSLER 2457](https://www.pdfsearch.io/img/999030d3546c3dc0f23ce06f8019d9e1.jpg) | Add to Reading ListSource URL: faculty.washington.eduLanguage: English - Date: 2002-08-29 19:39:41
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10![3408 JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 32 3408 JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 32](https://www.pdfsearch.io/img/ebf9f548a3a40b6e5079263f010a67fd.jpg) | Add to Reading ListSource URL: www.soest.hawaii.eduLanguage: English - Date: 2003-02-28 22:11:22
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