CARIACO Ocean Time Series Program

Results: 82



#Item
1A review of nitrogen isotopic alteration in marine sediments

A review of nitrogen isotopic alteration in marine sediments

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Source URL: people.oregonstate.edu

Language: English - Date: 2013-06-03 14:51:15
2NASA CRNASb-CR-132E25) C U E C C K T A H I N A T E D A T I ~ O L I H E R E : T H E C A b G E R OF C L I B A T E C E E N G E , PHASES 1 A R C 2 Final Eieport (Crerel Uniop HC 64.75

NASA CRNASb-CR-132E25) C U E C C K T A H I N A T E D A T I ~ O L I H E R E : T H E C A b G E R OF C L I B A T E C E E N G E , PHASES 1 A R C 2 Final Eieport (Crerel Uniop HC 64.75

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Source URL: ntrs.nasa.gov

Language: English - Date: 2013-08-31 15:56:17
3ODP Distinguished Lecture Series: Larry Peterson

ODP Distinguished Lecture Series: Larry Peterson

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Source URL: www.odplegacy.org

Language: English - Date: 2014-09-04 08:45:01
4REPORTS tration for Ta ⫽ 10 when ␦ ⱖ O(10). In the case of the jovian atmosphere, if we take Ta ⫽ 1012 for Jupiter (9), we obtain ␦ ⫽ 100. Teleconvection may have important implications for the dynamics of pl

REPORTS tration for Ta ⫽ 10 when ␦ ⱖ O(10). In the case of the jovian atmosphere, if we take Ta ⫽ 1012 for Jupiter (9), we obtain ␦ ⫽ 100. Teleconvection may have important implications for the dynamics of pl

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Source URL: www.climategeology.ethz.ch

Language: English - Date: 2007-10-05 05:30:54
5Oceanography THE OFFICIAL MAGAZINE OF THE OCEANOGRAPHY SOCIETY CITATION Scranton, M.I., G.T. Taylor, R. Thunell, C.R. Benitez-Nelson, F. Muller-Karger, K. Fanning, L. Lorenzoni, E. Montes, R. Varela, and Y. Astor. 2014

Oceanography THE OFFICIAL MAGAZINE OF THE OCEANOGRAPHY SOCIETY CITATION Scranton, M.I., G.T. Taylor, R. Thunell, C.R. Benitez-Nelson, F. Muller-Karger, K. Fanning, L. Lorenzoni, E. Montes, R. Varela, and Y. Astor. 2014

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Source URL: www.tos.org

Language: English - Date: 2015-07-08 11:16:50
6deposited mineral phases within fissures and cracks. The martian weathering products are the most likely source of the required LREE, incompatible, and volatile elements. Upon impact, preferential, shock-induced melting

deposited mineral phases within fissures and cracks. The martian weathering products are the most likely source of the required LREE, incompatible, and volatile elements. Upon impact, preferential, shock-induced melting

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Source URL: www.climategeology.ethz.ch

Language: English - Date: 2012-11-12 02:18:58
7Links between tropical rainfall and North Atlantic climate during the last glacial period

Links between tropical rainfall and North Atlantic climate during the last glacial period

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Source URL: www.climategeology.ethz.ch

Language: English - Date: 2013-02-26 06:00:40
8EGU General Assembly 2012 EGU General Assembly 2012 Programme Group Programme OS – Ocean Sciences Monday, 23 April........................................................................................................

EGU General Assembly 2012 EGU General Assembly 2012 Programme Group Programme OS – Ocean Sciences Monday, 23 April........................................................................................................

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Source URL: www.egu2012.eu

Language: English - Date: 2013-11-11 23:12:20
9Remote Sensing of Environment – 140 www.elsevier.com/locate/rse An improved in-situ bio-optical data set for ocean color algorithm development and satellite data product validation P. Jeremy Werdell a,*,

Remote Sensing of Environment – 140 www.elsevier.com/locate/rse An improved in-situ bio-optical data set for ocean color algorithm development and satellite data product validation P. Jeremy Werdell a,*,

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Source URL: oceancolor.gsfc.nasa.gov

Language: English - Date: 2014-07-15 12:17:16
10Journal of Oceanography, Vol. 62, pp. 745 to 752, 2006  Short Contribution Lower Cd/P Ratio in Settling Particles than in Surface Seawater in the Okinawa Trough

Journal of Oceanography, Vol. 62, pp. 745 to 752, 2006 Short Contribution Lower Cd/P Ratio in Settling Particles than in Surface Seawater in the Okinawa Trough

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Source URL: www.terrapub.co.jp

Language: English - Date: 2006-08-25 04:35:53