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Seasonal Carbon Cycling in the Sargasso Sea Near Bermuda.

The authors of this study demonstrate that by simultaneously observing changes in the stable isotopic ratio of dissolved inorganic carbon, it is possible to quantify the contribution of physical and biological processes to the summer-fall drawdown recorded at Station S in the Sargasso Sea.

Detalles Bibliográficos
Clasificación:Libro Electrónico
Autor principal: Gruber, Nicolas, 1968- (Autor)
Formato: Electrónico eBook
Idioma:Inglés
Publicado: Berkeley : University of California Press, 1999.
Colección:Bulletin of the Scripps Institution of Oceanography, 30.
Temas:
Acceso en línea:Texto completo

MARC

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100 1 |a Gruber, Nicolas,  |d 1968-  |e author. 
245 1 0 |a Seasonal Carbon Cycling in the Sargasso Sea Near Bermuda. 
260 |a Berkeley :  |b University of California Press,  |c 1999. 
300 |a 1 online resource (106 pages) 
336 |a text  |b txt  |2 rdacontent 
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490 1 |a Bulletin of the Scripps Institution of Oceanography, 30 
505 0 |a COVER; TITLE; COPYRIGHT; CONTENTS; ABSTRACT; ACKNOWLEDGMENTS; 1. INTRODUCTION; 2. PROCESSES CONTROLLING THE CARBON BALANCE IN THE UPPER OCEAN; 2.1 Introduction; 2.2 Biological Processes; 2.3 Air-Sea Exchange; 2.4 Mixed-Layer Dynamics and Vertical Transport; 2.5 Lateral Transport; 2.6 The Seasonal Cycle Near Bermuda; 3. CONSTRAINING CARBON BUDGETS BY CONCURRENT MEASUREMENTS OF DIC AND 13d; 4. SEASONAL OBSERVATIONS; 5. HARMONIC FITTING; 6. DESCRIPTION OF THE SEASONAL MODEL; 6.1 Outline of the Model; 6.2 Air-Sea Gas Transfer; 6.3 Vertical Turbulent Diffusive Transport; 6.4 Vertical Entrainment. 
505 8 |a 6.5 Biological Exchange: Net Community Production6.6 Calculation of Vertically Integrated Rates of Change; 7. RESULTS OF THE SEASONAL MODEL; 7.1 Seasonal Variations of Dissolved Inorganic Carbon; 7.2 Calculated Seasonal Cycle of Dissolved Inorganic Carbon; 7.3 Seasonal Variations of Vertically Integrated Rates of Change; 7.4 Temporally Integrated Changes in Concentration; 7.5 Temporally and Vertically Integrated Rates of Ch. 
520 |a The authors of this study demonstrate that by simultaneously observing changes in the stable isotopic ratio of dissolved inorganic carbon, it is possible to quantify the contribution of physical and biological processes to the summer-fall drawdown recorded at Station S in the Sargasso Sea. 
588 0 |a Print version record. 
504 |a Includes bibliographical references. 
546 |a English. 
590 |a JSTOR  |b Books at JSTOR All Purchased 
590 |a JSTOR  |b Books at JSTOR Evidence Based Acquisitions 
590 |a JSTOR  |b Books at JSTOR Demand Driven Acquisitions (DDA) 
650 0 |a Seawater  |x Analysis. 
650 0 |a Carbon  |x Analysis. 
650 0 |a Carbon cycle (Biogeochemistry) 
650 6 |a Eau de mer  |x Analyse. 
650 6 |a Carbone  |x Analyse. 
650 6 |a Cycle du carbone (Biogéochimie) 
650 7 |a NATURE  |x Ecosystems & Habitats  |x Oceans & Seas.  |2 bisacsh 
650 7 |a SCIENCE  |x Earth Sciences  |x Oceanography.  |2 bisacsh 
650 7 |a Carbon  |x Analysis  |2 fast 
650 7 |a Carbon cycle (Biogeochemistry)  |2 fast 
650 7 |a Seawater  |x Analysis  |2 fast 
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830 0 |a Bulletin of the Scripps Institution of Oceanography, 30. 
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