LEADER 03418nam 2200697 a 450 001 9910454776703321 005 20200520144314.0 010 $a1-282-35580-5 010 $a9786612355806 010 $a0-520-91596-8 024 7 $a10.1525/9780520915961 035 $a(CKB)1000000000767464 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 035 $a(DE-B1597)521119 035 $a(DE-B1597)9780520915961 035 $a(Au-PeEL)EBL470850 035 $a(CaPaEBR)ebr10676167 035 $a(CaONFJC)MIL235580 035 $a(EXLCZ)991000000000767464 100 $a19990503d1999 uy 0 101 0 $aeng 135 $aur|n|---||||| 181 $ctxt 182 $cc 183 $acr 200 10$aSeasonal carbon cycling in the Sargasso Sea near Bermuda$b[electronic resource] /$fNicolas Gruber and Charles D. Keeling 210 $aBerkeley $cUniversity of California Press$d1999 215 $a1 online resource (106 p.) 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 $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) 608 $aElectronic books. 615 0$aSeawater$xAnalysis. 615 0$aCarbon$xAnalysis. 615 0$aCarbon cycle (Biogeochemistry) 676 $a551.46/462 700 $aGruber$b Nicolas$f1968-$01046591 701 $aKeeling$b Charles D.$f1928-$01046592 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a9910454776703321 996 $aSeasonal carbon cycling in the Sargasso Sea near Bermuda$92473604 997 $aUNINA LEADER 01232oam 2200421zu 450 001 996204916303316 005 20210803234304.0 035 $a(CKB)1000000000726898 035 $a(SSID)ssj0000409502 035 $a(PQKBManifestationID)12172153 035 $a(PQKBTitleCode)TC0000409502 035 $a(PQKBWorkID)10348220 035 $a(PQKB)11595089 035 $a(EXLCZ)991000000000726898 100 $a20160829d2000 uy 101 0 $aeng 181 $ctxt 182 $cc 183 $acr 200 10$aSocial Development in Asia 210 31$a[Place of publication not identified]$cSpringer$d2000 300 $aBibliographic Level Mode of Issuance: Monograph 311 $a0-7923-6256-X 606 $aSocial Conditions$2HILCC 606 $aSociology & Social History$2HILCC 606 $aSocial Sciences$2HILCC 607 $aAsia$xSocial conditions 615 7$aSocial Conditions 615 7$aSociology & Social History 615 7$aSocial Sciences 676 $a306/.095 700 $aTang$b Kwong-Ieung$0854857 701 $aTang$b Kwong-Leung$0854858 801 0$bPQKB 906 $aBOOK 912 $a996204916303316 996 $aSocial Development in Asia$91908973 997 $aUNISA LEADER 01787oam 2200517I 450 001 9910706186703321 005 20170821080721.0 035 $a(CKB)5470000002454557 035 $a(OCoLC)703664837 035 $a(EXLCZ)995470000002454557 100 $a20110224j199910 ua 0 101 0 $aeng 135 $aurbn||||||||| 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 10$aInlet flow characteristics during rapid maneuvers for an F/A-18A airplane /$fWilliam G. Steenken and John G. Williams, Kevin R. Walsh 210 1$aEdwards, California :$cNational Aeronautics and Space Administration, Dryden Flight Research Center,$dOctober 1999. 215 $a1 online resource (ix, 208 pages) $cillustrations 225 1 $aNASA/TM ;$v1999-206587 300 $a"October 1999." 300 $a"Performing organization: NASA Dryden Flight Research Center"--Report documentation page. 320 $aIncludes bibliographical references (pages 47-48). 606 $aAir flow$2nasat 606 $aAir intakes$2nasat 606 $aFlow characteristics$2nasat 606 $aResearch aircraft$2nasat 606 $aIntake systems$2nasat 606 $aInlet flow$2nasat 615 7$aAir flow. 615 7$aAir intakes. 615 7$aFlow characteristics. 615 7$aResearch aircraft. 615 7$aIntake systems. 615 7$aInlet flow. 700 $aSteenken$b William G.$01392405 702 $aWilliams$b J. G$g(John G.), 702 $aWalsh$b Kevin R. 712 02$aDryden Flight Research Facility, 801 0$bSSN 801 1$bSSN 801 2$bGPO 906 $aBOOK 912 $a9910706186703321 996 $aInlet flow characteristics during rapid maneuvers for an F$93447090 997 $aUNINA