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Seasonal Carbon Cycling in the Sargasso Sea Near Bermuda.

Author: Nicolas Gruber
Publisher: Berkeley : University of California Press, 1999.
Series: Bulletin of the Scripps Institution of Oceanography, 30.
Edition/Format:   eBook : Document : EnglishView all editions and formats
Summary:
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.
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Genre/Form: Electronic books
Additional Physical Format: Print version:
Material Type: Document, Internet resource
Document Type: Internet Resource, Computer File
All Authors / Contributors: Nicolas Gruber
ISBN: 9780520915961 0520915968
OCLC Number: 609849939
Description: 1 online resource (106 pages).
Contents: 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. 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.
Series Title: Bulletin of the Scripps Institution of Oceanography, 30.

Abstract:

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  Read more...

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