Ekman transport

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4140  Regional Oceanography: an Introduction our Rule 1 we note here again that our rules are not applicable near the equator, where according to eqn[removed]Ekman layer transport grows beyond all bounds. In practical

40 Regional Oceanography: an Introduction our Rule 1 we note here again that our rules are not applicable near the equator, where according to eqn[removed]Ekman layer transport grows beyond all bounds. In practical

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

Language: English - Date: 2006-08-17 03:26:10
42South Atlantic meridional fluxes

South Atlantic meridional fluxes

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Source URL: www.aoml.noaa.gov

Language: English - Date: 2013-01-11 14:11:40
431200  JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 39

1200 JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 39

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Source URL: www.pmel.noaa.gov

Language: English - Date: 2009-05-27 13:33:21
44Microsoft PowerPoint - Fig_5 [Read-Only]

Microsoft PowerPoint - Fig_5 [Read-Only]

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Source URL: www.aoml.noaa.gov

Language: English - Date: 2014-08-20 13:30:31
45PUBLICATIONS Geophysical Research Letters RESEARCH LETTER[removed]2014GL060428 Key Points: • Seasonal variations in geostrophic

PUBLICATIONS Geophysical Research Letters RESEARCH LETTER[removed]2014GL060428 Key Points: • Seasonal variations in geostrophic

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Source URL: www.aoml.noaa.gov

Language: English - Date: 2014-08-19 15:53:48
46Temporal Variability of the Atlantic Meridional Overturning Circulation at 26.5°N Stuart A. Cunningham, et al. Science 317, [removed]); DOI: [removed]science[removed]The following resources related to this article are av

Temporal Variability of the Atlantic Meridional Overturning Circulation at 26.5°N Stuart A. Cunningham, et al. Science 317, [removed]); DOI: [removed]science[removed]The following resources related to this article are av

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Source URL: www.aoml.noaa.gov

Language: English - Date: 2013-05-15 14:10:41
47Observed Flow Compensation Associated with the MOC at 26.5°N in the Atlantic Torsten Kanzow, et al. Science 317, [removed]); DOI: [removed]science[removed]The following resources related to this article are available onl

Observed Flow Compensation Associated with the MOC at 26.5°N in the Atlantic Torsten Kanzow, et al. Science 317, [removed]); DOI: [removed]science[removed]The following resources related to this article are available onl

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Source URL: www.aoml.noaa.gov

Language: English - Date: 2013-05-15 14:10:42
48North Atlantic sea level, heat content and MOC variability over the last 60 years estimated from hydrographic data Vassil Roussenov1, Ric Williams1, M. Susan Lozier 2 and Doug Smith3 1.  Department of Earth and Ocean S

North Atlantic sea level, heat content and MOC variability over the last 60 years estimated from hydrographic data Vassil Roussenov1, Ric Williams1, M. Susan Lozier 2 and Doug Smith3 1.  Department of Earth and Ocean S

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Source URL: www.psmsl.org

Language: English - Date: 2013-11-11 11:16:10
49outline[removed]Ocean 620 Introduction to Physical Oceanography Fall, 2014

outline[removed]Ocean 620 Introduction to Physical Oceanography Fall, 2014

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Source URL: currents.soest.hawaii.edu

Language: English - Date: 2014-09-30 15:58:15
50Case Study 15 Biological Response Associated With a Coastal Upwelling Event Hervé Demarcq∗1 and Dominique Dagorne2  15.1

Case Study 15 Biological Response Associated With a Coastal Upwelling Event Hervé Demarcq∗1 and Dominique Dagorne2 15.1

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Source URL: www.ioccg.org

Language: English - Date: 2011-06-23 12:32:45