FN Archimer Export Format
PT J
TI Using altimetry to help explain patchy changes in hydrographic carbon measurements
BT 
AF RODGERS, Keith B.
   KEY, Robert M.
   GNANADESIKAN, Anand
   SARMIENTO, Jorge L.
   AUMONT, Olivier
   BOPP, Laurent
   DONEY, Scott C.
   DUNNE, John P.
   GLOVER, David M.
   ISHIDA, Akio
   ISHII, Masao
   JACOBSON, Andrew R.
   LO MONACO, Claire
   MAIER-REIMER, Ernst
   MERCIER, Herle
   METZL, Nicolas
   PEREZ, Fiz F.
   RIOS, Aida F.
   WANNINKHOF, Rik
   WETZEL, Patrick
   WINN, Christopher D.
   YAMANAKA, Yasuhiro
AS 1:1;2:1;3:2;4:1;5:3,4;6:5;7:6;8:2;9:6;10:7,8;11:9;12:10;13:3;14:11;15:4,16;16:3;17:12;18:12;19:13;20:11;21:14;22:15;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:;16:;17:;18:;19:;20:;21:;22:;
C1 Princeton Univ, AOS Program, Princeton, NJ 08540 USA.
   NOAA, GFDL, Princeton, NJ 08540 USA.
   Univ Paris 06, IPSL, LOCEAN, F-75252 Paris, France.
   CNRS, UBO, IRD, IFREMER,LPO, F-29280 Plouzane, France.
   DSM, LSCE, F-91191 Gif Sur Yvette, France.
   Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.
   JAMSTEC, FRCGC, Yokohama, Kanagawa, Japan.
   JAMSTEC, IORGC, Yokohama, Kanagawa 2360001, Japan.
   Mission Res Inc, Tsukuba, Ibaraki 3050052, Japan.
   Univ Colorado, CIRES, Boulder, CO 80309 USA.
   MPI, D-20146 Hamburg, Germany.
   CSIC, E-28006 Madrid, Spain.
   NOAA, AOML, Miami, FL 33149 USA.
   Hawaii Pacific Univ, Coll Nat & Computat Sci, Kaneohe, HI 96744 USA.
   Hokkaido Univ, Grad Sch Environm Earth Sci, Sapporo, Hokkaido 0600810, Japan.
C2 UNIV PRINCETON, USA
   NOAA, USA
   LOCEAN, FRANCE
   CNRS, FRANCE
   DSM, FRANCE
   WOODS HOLE, USA
   JAMSTEC, JAPAN
   JAMSTEC, JAPAN
   MISSION RES INC, JAPAN
   UNIV COLORADO, USA
   MPI, GERMANY
   CSIC, SPAIN
   NOAA, USA
   UNIV HAWAII PACIFIC, USA
   UNIV HOKKAIDO, JAPAN
   IFREMER, FRANCE
SI BREST
SE PDG-DPCP
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-europe
   copubli-univ-france
   copubli-int-hors-europe
IF 3.082
TC 15
TU Centre national d'études spatiales
   Centre national de la recherche scientifique
   Commissariat à l'énergie atomique et aux énergies alternatives
   ELECTRICITE DE FRANCE
   Institut de recherche pour le développement
   Institut français de recherche pour l'exploitation de la mer
   Muséum national d'histoire naturelle
   Observatoire de Paris
   Université Paris Diderot
   Université Paris-Est Créteil Val-de-Marne
   Université Paris-Sud
   Université Pierre et Marie Curie
   Université de Bretagne Occidentale
   Université de Cergy-Pontoise
   Université de Versailles Saint-Quentin-en-Yvelines
   École nationale des ponts et chaussées
   École normale supérieure de Paris
   École polytechnique
   École pratique des hautes études
UR https://archimer.ifremer.fr/doc/00000/11107/7415.pdf
LA English
DT Article
CR OISO1
   OISO3-NIVMER98
   OVIDE 1
   OVIDE 2
BO Marion Dufresne
   Thalassa
AB Here we use observations and ocean models to identify mechanisms driving large seasonal to interannual variations in dissolved inorganic carbon (DIC) and dissolved oxygen (O-2) in the upper ocean. We begin with observations linking variations in upper ocean DIC and O-2 inventories with changes in the physical state of the ocean. Models are subsequently used to address the extent to which the relationships derived from short-timescale (6 months to 2 years) repeat measurements are representative of variations over larger spatial and temporal scales. The main new result is that convergence and divergence (column stretching) attributed to baroclinic Rossby waves can make a first-order contribution to DIC and O-2 variability in the upper ocean. This results in a close correspondence between natural variations in DIC and O-2 column inventory variations and sea surface height (SSII) variations over much of the ocean. Oceanic Rossby wave activity is an intrinsic part of the natural variability in the climate system and is elevated even in the absence of significant interannual variability in climate mode indices. The close correspondence between SSII and both DIC and O-2 column inventories for many regions suggests that SSII changes (inferred from satellite altimetry) may prove useful in reducing uncertainty in separating natural and anthropogenic DIC signals (using measurements from Climate Variability and Predictability's CO2/Repeat Hydrography program).
PY 2009
PD SEP
SO Journal Of Geophysical Research Oceans
SN 0148-0227
PU Amer Geophysical Union
VL 114
UT 000270057300001
DI 10.1029/2008JC005183
ID 11107
ER

EF