|
|
|
|
|
|
|
|
1. |
Record Nr. |
UNINA9911145840803321 |
|
|
Autore |
Gruber Nicolas <1968-> |
|
|
Titolo |
Seasonal carbon cycling in the Sargasso Sea near Bermuda / / Nicolas Gruber, Charles D. Keeling |
|
|
|
|
|
|
|
Pubbl/distr/stampa |
|
|
Berkeley : , : University of California Press, , 1999 |
|
|
|
|
|
|
|
ISBN |
|
9786612355806 |
9781282355804 |
1282355805 |
9780520915961 |
0520915968 |
|
|
|
|
|
|
|
|
Edizione |
[1st ed.] |
|
|
|
|
|
Descrizione fisica |
|
1 online resource (106 pages) : illustrations |
|
|
|
|
|
|
Collana |
|
Bulletin of the Scripps Institution of Oceanography, University of California, San Diego ; ; v. 30 |
|
|
|
|
|
|
|
|
Altri autori (Persone) |
|
KeelingCharles D. <1928-2005.> |
|
|
|
|
|
|
Disciplina |
|
|
|
|
|
|
Soggetti |
|
Seawater - Analysis |
Carbon - Analysis |
Carbon cycle (Biogeochemistry) |
|
|
|
|
|
|
|
|
Lingua di pubblicazione |
|
|
|
|
|
|
Formato |
Materiale a stampa |
|
|
|
|
|
Livello bibliografico |
Monografia |
|
|
|
|
|
Note generali |
|
Description based upon print version of record. |
|
|
|
|
|
|
Nota di bibliografia |
|
Includes bibliographical references. |
|
|
|
|
|
|
Nota di contenuto |
|
Frontmatter -- CONTENTS -- ABSTRACT -- ACKNOWLEDGMENTS -- 1. INTRODUCTION -- 2. PROCESSES CONTROLLING THE CARBON BALANCE IN THE UPPER OCEAN -- 3. CONSTRAINING CARBON BUDGETS BY CONCURRENT MEASUREMENTS OF DIC AND 13δ -- 4. SEASONAL OBSERVATIONS -- 5. HARMONIC FITTING -- 6. DESCRIPTION OF THE SEASONAL MODEL -- 7. RESULTS OF THE SEASONAL MODEL -- 8. DISCUSSION -- 9. SUMMARY AND CONCLUSIONS -- REFERENCES -- APPENDIX A: FORMULAS FOR THE SEASONAL MODEL -- APPENDIX B: THREE-DIMENSIONAL GLOBAL OCEAN TRACER TRANSPORT MODEL OF BACASTOW AND MAIER-REIMER (1991) -- APPENDIX C: SENSITIVITY TESTS -- TABLES -- FIGURES |
|
|
|
|
|
|
|
|
Sommario/riassunto |
|
Each year, the concentration of dissolved inorganic carbon (DIC) in the mixed layer at Station S in the Sargasso Sea decreases from winter to summer by about 30 umol/kg. The authors of this study demonstrate that by simultaneously observing changes in the stable isotopic ration of DIC, it is possible to quantify the contribution of physical and |
|
|
|
|