LEADER 04302nam  2201057 a 450 
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010   $a1-282-35580-5
010   $a9786612355806
010   $a0-520-91596-8
024 7 $a10.1525/9780520915961
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035   $a(EBL)470850
035   $a(OCoLC)609849939
035   $a(SSID)ssj0000350348
035   $a(PQKBManifestationID)11249736
035   $a(PQKBTitleCode)TC0000350348
035   $a(PQKBWorkID)10355816
035   $a(PQKB)10598458
035   $a(MiAaPQ)EBC470850
035   $a(OCoLC)777471944
035   $a(MdBmJHUP)muse31092
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035   $a(DE-B1597)9780520915961
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035   $a(EXLCZ)991000000000767464
100   $a19990503d1999      uy             0
101 0 $aeng
135   $aur|n|---|||||
181   $ctxt$2rdacontent
182   $cc$2rdamedia
183   $acr$2rdacarrier
200 10$aSeasonal carbon cycling in the Sargasso Sea near Bermuda /$fNicolas Gruber, Charles D. Keeling
210  1$aBerkeley :$cUniversity of California Press,$d1999.
215   $a1 online resource (106 pages) $cillustrations
225 1 $aBulletin of the Scripps Institution of Oceanography, University of California, San Diego ;$vv. 30
300   $aDescription based upon print version of record.
311 0 $a0-520-09833-1 
320   $aIncludes bibliographical references.
327   $tFrontmatter --$tCONTENTS --$tABSTRACT --$tACKNOWLEDGMENTS --$t1. INTRODUCTION --$t2. PROCESSES CONTROLLING THE CARBON BALANCE IN THE UPPER OCEAN --$t3. CONSTRAINING CARBON BUDGETS BY CONCURRENT MEASUREMENTS OF DIC AND 13? --$t4. SEASONAL OBSERVATIONS --$t5. HARMONIC FITTING --$t6. DESCRIPTION OF THE SEASONAL MODEL --$t7. RESULTS OF THE SEASONAL MODEL --$t8. DISCUSSION --$t9. SUMMARY AND CONCLUSIONS --$tREFERENCES --$tAPPENDIX A: FORMULAS FOR THE SEASONAL MODEL --$tAPPENDIX B: THREE-DIMENSIONAL GLOBAL OCEAN TRACER TRANSPORT MODEL OF BACASTOW AND MAIER-REIMER (1991) --$tAPPENDIX C: SENSITIVITY TESTS --$tTABLES --$tFIGURES
330   $aEach year, the concentration of dissolved inorganic carbon (DIC) in the mixed layer at Station S in the Sargasso Sea decreases from winter to summer by about 30 umol/kg. The authors of this study demonstrate that by simultaneously observing changes in the stable isotopic ration of DIC, it is possible to quantify the contribution of physical and biological processes to this summer-fall drawdown. They find that biology is the dominant contrbutor to the drawdown, but that physical processes also play an important role.
410  0$aBulletin of the Scripps Institution of Oceanography, La Jolla, California ;$vv. 30.
606   $aSeawater$xAnalysis
606   $aCarbon$xAnalysis
606   $aCarbon cycle (Biogeochemistry)
610   $aair sea boundary layer.
610   $aair sea exchange.
610   $abermuda.
610   $abiogeochemistry.
610   $acarbon balance.
610   $acarbon cycle.
610   $acarbon.
610   $aconservation.
610   $adic.
610   $aecosystem.
610   $aenvironment.
610   $aenvironmentalism.
610   $ahealthy oceans.
610   $ainorganic carbon.
610   $aisland.
610   $amarine environments.
610   $anatural science.
610   $anature.
610   $anonfiction.
610   $aocean.
610   $aoceanography.
610   $apollution.
610   $asargasso sea.
610   $ascience.
610   $asea.
610   $aseawater.
610   $asediment traps.
610   $asurface oceans.
610   $atropics.
610   $aupper ocean.
610   $awater health.
615  0$aSeawater$xAnalysis.
615  0$aCarbon$xAnalysis.
615  0$aCarbon cycle (Biogeochemistry)
676   $a551.46/462
700   $aGruber$b Nicolas$f1968-$01506939
701   $aKeeling$b Charles D.$f1928-2005.$01506940
801  0$bMiAaPQ
801  1$bMiAaPQ
801  2$bMiAaPQ
906   $aBOOK
912   $a9910777933803321
996   $aSeasonal carbon cycling in the Sargasso Sea near Bermuda$93737371
997   $aUNINA