Antarctic Bottom Water

Results: 110



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1Inclusion of a katabatic wind correction in a coarse-resolution global coupled climate model

Inclusion of a katabatic wind correction in a coarse-resolution global coupled climate model

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Source URL: homepages.vub.ac.be

Language: English - Date: 2012-11-30 17:59:10
2Microsoft Word - frisp_2006_kmak_a.doc

Microsoft Word - frisp_2006_kmak_a.doc

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Source URL: folk.uib.no

Language: English - Date: 2006-10-19 09:15:58
3Clim. Past, 10, 1239–1251, 2014 www.clim-past.netdoi:cp © Author(sCC Attribution 3.0 License.  Seasonal changes in glacial polynya activity inferred

Clim. Past, 10, 1239–1251, 2014 www.clim-past.netdoi:cp © Author(sCC Attribution 3.0 License. Seasonal changes in glacial polynya activity inferred

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Source URL: www.clim-past.net

Language: English - Date: 2014-12-09 13:33:55
4Clim. Past, 11, 803–824, 2015 www.clim-past.netdoi:cp © Author(sCC Attribution 3.0 License.  Bottom water variability in the subtropical northwestern Pacific

Clim. Past, 11, 803–824, 2015 www.clim-past.netdoi:cp © Author(sCC Attribution 3.0 License. Bottom water variability in the subtropical northwestern Pacific

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Source URL: www.clim-past.net

Language: English - Date: 2015-06-03 02:29:30
5138  Regional Oceanography: an Introduction A characteristic feature of the South Pacific Ocean is the existence of a second region of wind convergence in the tropics known as the South Pacific Convergence Zone or SPCZ.

138 Regional Oceanography: an Introduction A characteristic feature of the South Pacific Ocean is the existence of a second region of wind convergence in the tropics known as the South Pacific Convergence Zone or SPCZ.

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

Language: English - Date: 2006-08-17 03:26:20
6Chapter 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,

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

Language: English - Date: 2006-08-17 03:26:29
7Ocean Sci., 4, 89–98, 2008 www.ocean-sci.net/ © Author(sThis work is distributed under the Creative Commons Attribution 3.0 License.  Ocean Science

Ocean Sci., 4, 89–98, 2008 www.ocean-sci.net/ © Author(sThis work is distributed under the Creative Commons Attribution 3.0 License. Ocean Science

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Source URL: www.ocean-sci.net

Language: English - Date: 2014-12-03 10:47:49
8Ocean Sci., 8, 419–432, 2012 www.ocean-sci.netdoi:os © Author(sCC Attribution 3.0 License.  Ocean Science

Ocean Sci., 8, 419–432, 2012 www.ocean-sci.netdoi:os © Author(sCC Attribution 3.0 License. Ocean Science

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Source URL: www.ocean-sci.net

Language: English - Date: 2014-12-03 11:11:12
9This discussion paper is/has been under review for the journal Ocean Science (OS). Please refer to the corresponding final paper in OS if available. Discussion Paper  Ocean Sci. Discuss., 12, 769–822, 2015

This discussion paper is/has been under review for the journal Ocean Science (OS). Please refer to the corresponding final paper in OS if available. Discussion Paper Ocean Sci. Discuss., 12, 769–822, 2015

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Source URL: www.ocean-sci-discuss.net

Language: English - Date: 2015-05-21 06:14:52
10Deep Sea Drilling Project Initial Reports Volume 72

Deep Sea Drilling Project Initial Reports Volume 72

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Source URL: www.deepseadrilling.org

Language: English